Global warming


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Land-ocean temperature index from 1880 to today, with reference period 1951–1980. The solid black line is the global annual mean and the solid red line is the five-year locally weighted scatter plot smoothing . The blue uncertainty bars represent the total annual uncertainty with a 95% confidence interval .
Causes of Global Warming (1750-2011) (As of 2018)
Local surface temperatures since 1880, a sliding average over five years and with a spatial resolution of around 1200 km
Possible future scenarios for global greenhouse gas emissions. If all countries deliver on their current Paris Agreement pledges, average warming by 2100 will well exceed the Paris Agreement target of keeping warming “well below 2 ° C”.

The current global warming or global warming (colloquially also "the" climate change ) is the increase in the average temperature of the near-earth atmosphere and the oceans since the beginning of industrialization . It is an anthropogenic (= man-made) climate change .

In contrast to the weather , which describes short-term current conditions of the atmosphere, mean values ​​for the climate are recorded over longer periods of time. Normally, normal periods of 30 years are considered. According to the Intergovernmental Panel on Climate Change (IPCC), the rise in temperature from the pre-industrial period up to 2017 was around 1 ° C. 2016 was the warmest year since systematic measurements began in 1880. It was around 1.1 ° C warmer than in pre-industrial times. According to current research, it was last this warm at the end of the Eem warm period 115,000 years ago. The 20 warmest measured years are in the last 22 years (as of 2018) and the five warmest years were in descending order 2016, 2019, 2015, 2017 and 2018.

The warming has accelerated: The rate of increase calculated over the years 1956 to 2005, at 0.13 ± 0.03 ° C per decade, is almost twice as large as that over the years 1906 to 2005. In 2019, global warming reached an increase of 0, 18 ° C per decade. It also runs considerably faster than all known warming phases of the modern earth period , i.e. for 66 million years. During the transition from an ice age to an interglacial period, the earth warms up by around 4 to 5 ° C within approx. 10,000 years. In the case of man-made global warming, without tightened climate protection measures, it is expected that the temperature will rise by 4 to 5 ° C from the end of the 20th to the end of the 21st century; the warming would be about 100 times faster than with historical natural climate changes.

The cause of the warming is the ongoing anthropogenic enrichment of the earth's atmosphere with greenhouse gases , in particular carbon dioxide (CO 2 ), methane and nitrous oxide , which are mainly released through the burning of fossil energy , through deforestation and agriculture and especially animal husbandry. This increases the retention capacity for infrared heat radiation in the troposphere , which increases the greenhouse effect. The most important greenhouse gas in the current global warming is CO 2 . In 2015, the mean CO 2 concentration in the earth's atmosphere measured by the Mauna Loa measuring station rose to over 400 ppm for the first time  ; before industrialization it was around 280 ppm. The IPCC wrote in his 2015 published the fifth progress report that it is extremely likely that the people have caused more than 50% of 1951-2010 observed warming. The best estimate is that the human contribution to warming during this period is around 100%. These values ​​are supported by other progress reports. Without the current human influence on the climate system, the slight cooling trend that has prevailed for several millennia would very likely continue.

The atmospheric greenhouse effect was first described by Joseph Fourier in 1824 ; From the 1850s there was further research . In 1896, the chemist and physicist Svante Arrhenius predicted global warming due to the amount of CO 2 emitted by humans . In 1938 Guy Stewart Callendar succeeded for the first time in demonstrating global warming on the basis of temperature measurements. After the Second World War, the topic moved increasingly into the focus of science. The researchers Roger Revelle and Hans E. Suess spoke in 1957 of a gigantic ( large-scale ) "geophysical experiment". From around the 1960s, discussions on the topic of anthropogenic climate change took place at international level. Nathaniel Rich has detailed in his 2019 book Losing Earth how much was known about global warming and its consequences as early as the 1980s. Since around the beginning of the 1990s there has been a scientific consensus that global warming, measured since around 1850 , is caused by humans.

According to climate research, the expected and in some cases already observed consequences of global warming include, depending on the region of the earth , sea ice and glacier melt , a rise in sea level , the thawing of permafrost soils with the release of methane hydrate , growing drought zones and increasing weather extremes with corresponding repercussions on life and health Survival situation of humans and animals ( extinction of species ). The extent of the consequences depends on the level and duration of the warming. Some consequences can also be irreversible or act as tipping elements in the earth system , which in turn accelerate global warming with positive feedback , such as the release of the greenhouse gas methane from the thawed permafrost.

In order to mitigate the consequences of global warming for humans and the environment, national and international climate policy aim both to stop climate change through climate protection and to adapt to the warming that has already occurred. In order to be able to stop man-made global warming, on the one hand further energy-related greenhouse gas emissions must be completely avoided and, on the other hand, the emissions introduced into the atmosphere since the beginning of industrialization as well as emissions that cannot be avoided from now on through negative greenhouse gas emissions using suitable technologies such as B. BECCS , DACCS or carbon sequestration in the soil can be completely reversed. As of 2016 already was about 2 / 3 of the CO 2 Budgeting the maximum possible emissions for the Paris Convention agreed two-degree target used up, so that global emissions be reduced quickly would have if the target is to be reached. However, it cannot be ruled out that the two-degree target is not ambitious enough to prevent a state of the climate system known as the greenhouse earth , which would lead to hostile conditions on earth.

Physical basics

70 to 75% of the red, short-wavelength radiation component pass through the atmosphere to the earth's surface, which heats up and thereby turn the blue marked here infrared radiation emits radiation which is impeded to All of greenhouse gases. - Three wavelength ranges of infrared radiation are shown, as emitted by objects with temperatures occurring on the earth's surface: violet (+37 ° C) - blue - black (−63 ° C). The graphics below show which greenhouse gases filter which parts of the spectrum.

Since the industrial revolution , humans have increased the natural greenhouse effect through the emission of greenhouse gases , as has been proven by measurements. Since 1990, radiative forcing - i.e. H. the warming effect on the climate - increased by 43% from persistent greenhouse gases. In climatology there is now consensus that the increased concentration of greenhouse gases released by humans into the earth's atmosphere is very likely to be the most important cause of global warming, since without it the measured temperatures cannot be explained.

Greenhouse gases allow the short-wave radiation from the sun to pass through to the earth largely unhindered, but absorb a large part of the infrared radiation emitted by the earth . As a result, they heat up and even emit radiation in the long-wave range (see Kirchhoff's law of radiation ). The portion of radiation directed towards the earth's surface is known as atmospheric counter-radiation . In the isotropic case, half of the absorbed energy is radiated towards the earth and half towards space. This causes the earth's surface to heat up more than if the sun's short-wave radiation alone would heat it. The IPCC rates the degree of scientific understanding of the effects of greenhouse gases as "high".

The greenhouse gas water vapor (H 2 O) contributes 36 to 66%, carbon dioxide (CO 2 ) 9 to 26% and methane 4 to 9% to the natural greenhouse effect. The wide range can be explained as follows: On the one hand, there are large fluctuations in the concentration of these gases, both locally and temporally. On the other hand, their absorption spectra overlap. Example: Radiation that has already been absorbed by water vapor can no longer be absorbed by CO 2 . This means that in an environment such as ice-covered areas or arid desert, where water vapor contributes little to the greenhouse effect, the remaining greenhouse gases contribute more to the overall greenhouse effect than in the humid tropics.

Since the greenhouse gases mentioned are natural components of the atmosphere, the increase in temperature they cause is known as the natural greenhouse effect . The natural greenhouse effect means that the average temperature of the earth is around +14 ° C. Without the natural greenhouse effect, it would be around −18 ° C. These are calculated values ​​(see also idealized greenhouse model ). In the literature, these values ​​may vary slightly, depending on the calculation approach and the underlying assumptions, for example the reflection behavior ( albedo ) of the earth. These values ​​serve as evidence that there is a natural greenhouse effect, since without it the temperature would have to be significantly lower and the higher temperature can be explained by the greenhouse effect. Deviations of a few degrees Celsius initially do not play a major role in this verification.

Causes of Man Made Global Warming

Development of the earth's surface temperature (above) and the individual climate-affecting factors since 1870: solar activity, volcanism, natural variability (e.g. El Niño / La Niña years) and human activities (greenhouse gas emissions and cooling aerosol emissions).

The global warming currently observed is almost entirely due to human activity. The probable human contribution to the warming of the period 1951 to 2010 is at least 93% and could be up to 123%, i.e. over 100%, which is possible by compensating for various cooling factors. The main cause is the increasing greenhouse gas concentration in the earth's atmosphere due to human activities. In the fifth assessment report of the IPCC , the resulting additional radiative forcing in 2011 compared to the reference year 1750 net (i.e. after deducting cooling effects such as aerosols) at 2.3 W / m². All long-lived greenhouse gases caused a gross radiative forcing of 2.83 W / m². The most important greenhouse gas was CO 2 with 1.82 W / m², followed by methane with 0.48 W / m². Halogenated hydrocarbons caused a radiative forcing of 0.36 W / m², nitrous oxide 0.17 W / m². Of the short-lived greenhouse gases, ozone , the formation of which is stimulated by nitrogen oxides, carbon monoxide or hydrocarbons, has the highest radiative forcing at 0.4 W / m². Aerosols cause negative (i.e. cooling) radiative forcing of −0.9 W / m².

In contrast, changes in natural solar activity are an insignificant factor in the currently observed global warming. During the same period, solar activity accounted for a radiative forcing of only 0.1 W / m²; solar activity has even declined since the middle of the 20th century.

Increase in the concentration of the most important greenhouse gases

Carbon dioxide, nitrous oxide, methane and CFCs / PFCs (only the latter are decreasing due to global efforts to protect the ozone layer)
Increase in atmospheric carbon dioxide concentration in the Holocene
Effect of CO 2 on the climate ( Terra X )

The proportion of all four components of the natural greenhouse effect in the atmosphere has increased since the beginning of the industrial revolution. The rate of increase in concentration is the fastest in 22,000 years.

The concentration of CO 2 in the earth's atmosphere is mainly due to the use of fossil energy, the cement industry and extensive deforestation since the beginning of industrialization from approx. 280 ppmV by 40% to approx. 400 ppmV (parts per million, parts per million by volume ) increased in 2015. During the last 14 million years (since the Middle Miocene ) there were no significantly higher CO 2 values ​​than at present. According to measurements from ice cores , the CO 2 concentration has never exceeded 300 ppmV in the last 800,000 years. Around 100 million tons of carbon dioxide are released into the atmosphere every day through human activities (as of 2020).

The volume fraction of methane rose from 730 ppbV in 1750 to 1,800 ppbV (parts per billion) in 2011. This is an increase of 150% and, like CO 2, the highest level in at least 800,000 years. The main cause of this is currently cattle farming , followed by other agricultural activities such as growing rice. The global warming potential of 1 kg of methane over a period of 100 years is 25 times higher than that of 1 kg of CO 2 . According to a more recent study, this factor is even 33 if interactions with atmospheric aerosols are taken into account. In an oxygen-containing atmosphere, however, methane is oxidized, usually by hydroxyl radicals . A methane molecule once it has entered the atmosphere has an average residence time of twelve years.

In contrast, the residence time of CO 2 is sometimes in the range of centuries. The oceans absorb atmospheric CO 2 very quickly: a CO 2 molecule is dissolved in the oceans after an average of five years. These are released back into the atmosphere, so that part of the CO 2 emitted by humans ultimately lasts for several centuries (approx. 30%) and another part (approx. 20%) even for millennia in the carbon cycle of the hydrosphere and atmosphere remains.

The volume share of nitrous oxide rose from pre-industrial 270 ppbV to 323 ppbV. With its absorption spectrum, it helps to close a radiation window that is otherwise open to space. Despite its very low concentration in the atmosphere, it contributes around 6% to the anthropogenic greenhouse effect , since its effect as a greenhouse gas is 298 times stronger than that of CO 2 ; in addition, it also has a fairly long atmospheric dwell time of 114 years.

The water vapor concentration in the atmosphere is not significantly changed by anthropogenic water vapor emissions, as additional water introduced into the atmosphere condenses out within a few days. Rising global average temperatures, however, lead to higher vapor pressure, i.e. greater evaporation. The global increase in the water vapor content of the atmosphere is an additional driver of global warming. Water vapor thus essentially acts as a feedback element. This water vapor feedback is, next to the ice-albedo feedback, the strongest, positive feedback in global climate events.

Aerosols

In addition to greenhouse gases, solar activity and aerosols also influence the earth's climate. Of all the identified contributions to radiative forcing, aerosols provide the greatest uncertainty, and the understanding of them is described as "low" by the IPCC. The effect of an aerosol on the air temperature depends on its altitude in the atmosphere. In the lowest layer of the atmosphere, the troposphere , soot particles cause the temperature to rise because they absorb sunlight and then give off thermal radiation . The reduced reflectivity ( albedo ) of snow and ice surfaces and the soot particles that have fallen on them also have a warming effect. In the higher layers of the air, on the other hand, mineral particles ensure that the earth's surface is cooler thanks to their shielding effect.

A major factor of uncertainty when measuring the climate impact of aerosols is their influence on the cloud formation , which is also not fully understood . Despite the uncertainties, aerosols are considered to have a significantly cooling effect overall. Decreasing air pollution could therefore contribute to global warming.

The decline in global mean temperatures observed between the 1940s and mid-1970s, as well as the temporary stagnation of global mean temperatures after 2000, is largely attributed to the cooling effect of sulfate aerosols, which in the first case occurred in Europe and the USA and in the last case in the People's Republic of China and India were to be located.

Subordinate and incorrectly suspected causes

Course of the global temperature anomaly (red, right scale) and the activity of galactic cosmic rays (blue, left scale, activity increasing downwards) since the second half of the 20th century. The hypothesis that the temperature increases with increasing solar activity and thus lower galactic cosmic radiation is not supported by the data.

A number of factors influence the global climate system . In the discussion about the causes of global warming, factors are often mentioned that are subordinate or even have a cooling effect on the climate system. Altered cosmic rays are not responsible for the warming currently observed. The earth has been in a phase of rewarming from the Little Ice Age since around 1850, i.e. since the beginning of the industrial revolution . Regardless of this, without human intervention in the natural climate, the cooling trend of 0.10 to 0.15 ° C per millennium that has existed for 6000 years would continue and - depending on the literature source - lead to a new cold period in 20,000 to 50,000 years.

Ozone hole

The assumption that the ozone hole is a major cause of global warming is wrong. The depletion of ozone in the stratosphere has a slightly cooling effect. The ozone depletion works in two ways: The reduced ozone concentration cools the stratosphere, since the UV radiation is no longer absorbed there, but warms the troposphere, since the UV radiation is absorbed on the earth's surface and warms it. The colder stratosphere sends less warming infrared radiation downwards and thus cools the troposphere. Overall, the cooling effect dominates, so that the IPCC concludes that the observed ozone depletion over the last two decades has led to a negative radiative forcing on the climate system, which is around −0.15 ± 0.10 watts per square meter (W / m² ) can be quantified.

Solar activity

Global temperature development (red), atmospheric CO 2 concentration (blue) and solar activity (yellow) since 1850
Effect of the sun on the earth's climate

Changes in the sun are said to have a minor impact on measured global warming. The change in radiation intensity measured directly from orbit since 1978 is far too small to be the main cause of the temperature development observed since then. Since the 1960s, the course of the global average temperature has been decoupled from the radiation intensity of the sun, since 1978 the reduced radiation intensity has very probably counteracted global warming somewhat.

In 2013, the IPCC estimated the additional radiative forcing by the sun since the beginning of industrialization to be around 0.05 (± 0.05) watts per square meter. In comparison, the anthropogenic greenhouse gases contribute 2.83 (± 0.29) W / m² to the warming. The IPCC writes that the degree of scientific understanding regarding the influence of solar variability has increased from “very low” to “low” from the third to the fourth assessment report. In the fifth assessment report, the IPCC attributes its estimate of the solar radiative forcing since 1750 to "medium informative value"; the informative value has been higher for the last three decades.

Cosmic rays

The argument that cosmic rays increase the effects of solar activity is based on a study by Henrik Svensmark and Egil Friis-Christensen . They assume that cosmic radiation influences the formation of clouds and thus has an indirect influence on the earth's surface temperature. This is to explain how fluctuations in solar activity - despite the only slight change in solar radiation - can trigger the observed global temperature increase. However, more recent scientific studies, mainly from the CLOUD experiment , show that the influence of cosmic rays on cloud formation is minimal. In its 5th assessment report, published in 2013, the IPCC stated that although there were indications of such a mechanism of action, it was too weak to have a significant impact on the climate. Cosmic rays as a reinforcing factor are also dependent on solar activity and, given its negative trend since the 1960s, could at most have increased a cooling effect.

Volcanic activity

Large volcanic eruptions of category VEI-5 or VEI-6 on the volcanic explosion index can cause hemispherical or global cooling (around -0.3 to -0.5 ° C) over several years due to the emission of volcanic ash and aerosols into the stratosphere . It is assumed that high volcanic activity, for example, exerted a considerable influence on the temperature development during the Little Ice Age . The effect of volcanic activity has shown a slightly cooling trend over the past 60 years, so it cannot explain the warming either.

It is sometimes argued that the CO 2 emitted by the volcanoes is responsible for the additional greenhouse effect. However, volcanoes only release around 210 to 360 megatons of CO 2 per year . That is about a hundredth of the annual man-made CO 2 emissions.

Steam

With an atmospheric share of around 0.4%, water vapor is the most powerful greenhouse gas in its overall effect and is responsible for around two thirds of the natural greenhouse effect. CO 2 is the second most important factor and accounts for most of the remaining greenhouse effect. However, the concentration of water vapor in the atmosphere is mainly dependent on the air temperature (according to the Clausius-Clapeyron equation , air can absorb around 7% more water vapor per degree Celsius). If the temperature increases due to another influencing factor, the water vapor concentration increases and with it its greenhouse gas effect - which leads to a further increase in temperature. Water vapor thus intensifies the temperature changes triggered by other factors. This effect is called water vapor feedback . Water vapor therefore doubles or triples the warming caused by the increase in CO 2 concentration alone .

Waste heat

Almost all processes generate heat , such as the production of electricity, the use of internal combustion engines (see efficiency ) or the operation of computers. In the USA and Western Europe, building heating, industrial processes and combustion engines contributed 0.39 W / m² and 0.68 W / m² to the warming in 2008 and thus have a certain influence on regional climate change. Seen worldwide, this value was 0.028 W / m² (i.e. only about 1% of global warming). Considerable contributions to warming can be expected from the end of our century in the event of a further unchecked increase in energy production (as in previous decades). If one considers the total length of time carbon dioxide remains in the atmosphere, then the radiation forcing caused by the greenhouse effect as a result of the combustion of carbon exceeds the heat released during the combustion process more than 100,000 times.

Urban heat islands

The temperature in cities is often higher than in the surrounding area, as heat is produced by heating and industrial processes. This is more strongly absorbed in houses and sealed surfaces. The temperature difference in large cities can be up to 10 ° C. Since many temperature measurements are made in cities, this could lead to a virtual increase in global temperature. However, temperature changes and not absolute values ​​are taken into account in measurements of global temperature. In addition, temperature measurements in cities are often carried out on green areas that are cooler due to the greenery. Control calculations of the global temperature with exclusively rural stations result in practically the same temperature trends as the calculation from all stations.

Measured and projected warming

Global average temperature anomaly 1850–2016

The main indicators of the current global warming are the worldwide temperature measurements that have been available since around 1850 and the analyzes of various climate archives . Compared with the fluctuations of the seasons and with the change from day to night, the numbers given below appear small; as a global change in climate, however, they mean a lot when you consider the average temperature on earth during the last ice age , which was only around 6 K lower .

In 2005 u. a. Based on the measured temperature increase of the oceans over a decade, it is calculated that the earth consumes 0.85 watts per square meter more power than it radiates into space.

Previous temperature increase

Development of the temperature increase according to " World Scientists' Warning to Humanity: A Second Notice ", 2017
Global monthly temperatures since 1850, animation based on HadCRUT4 data from the Met Office

According to a publication published in 2016, the global average temperature began to rise as early as 1830 due to human activity. This was found in a broad study in which a large number of palaeoclimatological indicators of bygone times (so-called climate proxies ) were evaluated worldwide . At that time there was no dense network of temperature measuring stations. A clear warming phase could be observed between 1910 and 1945, in which natural fluctuations also had a clear influence due to the still comparatively low concentration of greenhouse gases. The warming is most pronounced from 1975 until today. 

2016 was the warmest year since measurements began in 1880. It was around 1.1 ° C warmer than in pre-industrial times. 2017 was the warmest non-El Niño year to date and also the second warmest year since measurements began. Every decade since the 1980s has been warmer than the previous one; the five warmest years in descending order were 2016, 2019, 2015, 2017 and 2018. According to figures from the Copernicus program , the warming was even 1.3 ° C above the level of the pre-industrial period, bringing the politically targeted limit of 1.5 ° C was almost reached at times. Compared to 2015, the additional warming was 0.2 ° C.

Between 1880 and 2012, the globally averaged, ground-level air temperatures increased by 0.85 ° C. Particularly in the case of short time series, it must be taken into account that the beginning and end of the year can have a strong influence on the trend and therefore do not necessarily have to reflect long-term trends. An example of such a deviation is the period between 1998 and 2012, which began with a strong El Niño and thus an exceptionally hot year, which is why the warming trend of 0.05 ° C per decade in this period is well below the long-term trend of 0.12 ° C per decade between 1951 and 2012. Nevertheless, the 30 years from 1983 to 2012 in the northern hemisphere were the warmest normal period in 1400 years. In this context, a study published in 2020 based on a detailed analysis of paleo-climatic data comes to the conclusion that the warming that has occurred in the 21st century to date has a high probability of exceeding the temperature values ​​of the Holocene optimum climate (about 8,000 to 6,000 years ago).

In a study published in 2007, the natural share of the warming in the 20th century was limited to below 0.2 K.

Ocean warming

The graphic shows where the additional energy remains that is accumulating in the earth system due to the anthropogenic disturbance of the climate

In addition to the air, the oceans have also warmed up, absorbing over 90% of the additional thermal energy. While the world's oceans only heated up by a total of 0.04 K from 1955 to the mid-2000s due to their enormous volume and great temperature inertia, their surface temperature increased by 0.6 K in the same period in the area from the sea surface to one At a depth of 75 meters, the temperature rose by an average of 0.11 K per decade from 1971 to 2010.

The energy content of the world's oceans increased by approx. 14.5 × 10 22 joules between the mid-1950s and 1998 , which corresponds to a heating output of 0.2 watts per m² of the entire earth's surface. The energy increase in the world's oceans of 14.5 × 10 22 joules corresponds to the energy of 100 million Hiroshima atomic bombs ; this amount of energy would heat the bottom 10 kilometers of the atmosphere by 22 K. Over the period 1971 and 2016, the averaged heat absorption of the oceans was around 200 terawatts and thus more than 10 times as high as the entire world energy consumption of mankind.

The heat content of the oceans has been measured with the help of the Argo program since 2000, which means that significantly more precise data on the condition and changes in climatologically relevant measured values ​​(e.g. heat content, salinity , depth profile) have been available since then . The past ten years have been the warmest years for the oceans since measurements began; 2019 the warmest so far.

Spatial and temporal distribution of the observed warming

The northern hemisphere (red) warmed up a little more than the southern hemisphere (blue); The reason for this is the larger proportion of land area in the northern hemisphere, which heats up faster than oceans.

Air over land surfaces generally heats up more strongly than over water surfaces, which can be seen in the animation at the beginning of this article (third position at the top right). The warming of the land areas between 1970 and 2014 averaged 0.26 K and thus more than twice as high as over the sea, which warmed by 0.12 K in the same period. Accordingly, the temperatures in the northern hemisphere, on which the majority of the land area is located, rose more sharply in the past 100 years than in the southern hemisphere, as the graphic opposite shows.

The night and winter temperatures rose slightly more than the day and summer temperatures. Broken down according to the seasons, the greatest warming was measured during the winter months, and particularly strong over western North America, Scandinavia and Siberia. In spring, temperatures rose most in Europe and in North and East Asia. Europe and North Africa were hardest hit in summer, and northern North America, Greenland and East Asia saw the largest increase in autumn. The warming was particularly striking in the Arctic , where it is about twice as high as the global average. With the exception of a few regions, global warming has been detectable since 1979.

In theory, different levels of warming are expected for the various layers of air in the earth's atmosphere, and in fact it is also measured. While the earth's surface and the low to medium troposphere should warm up, models for the higher stratosphere suggest a cooling. In fact, exactly this pattern was found in measurements. The satellite data shows a decrease in the lower stratosphere temperature of 0.314 K per decade over the past 30 years. This cooling is caused on the one hand by the increased greenhouse effect and on the other hand by ozone depletion by CFCs in the stratosphere, see also the Montreal Protocol on the Protection of the Ozone Layer . If the sun were the main cause, the layers close to the surface, the lower to middle troposphere and the stratosphere would have had to warm up. According to current understanding, this means that the majority of the observed warming must be caused by human activities.

The ten warmest years

Observed shift in frequency distribution: The distribution of measured temperature data from the period 2005–2015 compared to the normal period 1951–1980, according to Hansen and Sato 2016, is shown

The ten warmest years in the period from 1880 to 2019 - deviation from the long-term average temperature (1901-2000) in ° C

A. Global surface temperature
land and sea
rank year deviation
1 2016 +0.99
2 2019 +0.95
3 2015 +0.93
4th 2017 +0.91
5 2018 +0.83
6th 2014 +0.74
7th 2010 +0.72
8th 2013 +0.67
9 2005 +0.67
10 2009 +0.64
B. Global surface temperature
on land
rank year deviation
1 2016 +1.54
2 2015 +1.42
3 2019 +1.42
4th 2017 +1.41
5 2018 +1.21
6th 2010 +1.17
7th 2007 +1.16
8th 2005 +1.10
9 2013 +1.04
10 2014 +1.03

Temporary cooling or pause in global warming

Even assuming a warming of 4 K by the end of the 21st century, there will always be phases of stagnation or even cooling. These phases can last up to approx. 15 years. Causes are the eleven-year sunspot cycle , cooling strong volcanic eruptions and the natural property of the global climate to show a fluctuating temperature profile ( AMO , PDO , ENSO ). For example, the occurrence of El Niño or La Niña events can raise or lower the global average temperature by 0.2 K from one year to the next and cover the annual warming trend of approx. 0.02 K for a few years , but also reinforce.

Feedback

The global climate system is characterized by feedbacks that increase or decrease temperature changes. Feedback that reinforces the cause is called positive feedback . According to the current state of knowledge, the positive feedbacks are significantly stronger than the negative feedbacks in certain states of global climate events, so that the climate system can tip over into another state.

The two strongest, positive feedback processes are the ice-albedo feedback and the water vapor feedback. A melting of the polar ice caps causes an additional energy input via the ice-albedo feedback due to reduced reflection. The water vapor feedback occurs because the atmosphere of a warmer world also contains more water vapor. Since water vapor is by far the most powerful greenhouse gas, a warming process that has been initiated is further intensified - regardless of what ultimately triggered this warming. The same applies to cooling, which is further intensified by the same processes. The term climate sensitivity was established for the quantitative description of the reaction of the climate to changes in the radiation balance . It can be used to compare different influencing variables with one another.

Another positive feedback is provided by the CO 2 itself. With increasing global warming, the water in the oceans also becomes warmer and can therefore absorb less CO 2 . As a result, more CO 2 can get into the atmosphere, which can further intensify the greenhouse effect. At the moment, however, the oceans still absorb around 2 Gt of carbon (this corresponds to around 7.3 Gt of CO 2 ) more than they release into the atmosphere in the same period of time, see acidification of the seas .

In addition to these three physically well-understood feedback factors, there are other feedback factors, the effects of which are much more difficult to assess, especially with regard to clouds, vegetation and the ground.

The role of the clouds

Low clouds cool the earth through their sun reflection, high clouds warm the earth

Clouds have a significant impact on the earth's climate by reflecting part of the incident radiation. Radiation from the sun is reflected back into space, and radiation from the layers of the atmosphere below is reflected towards the ground. The brightness of the clouds comes from short-wave radiation in the visible wavelength range.

A greater optical thickness of low clouds means that more energy is reflected back into space; the temperature of the earth is falling. Conversely, less dense clouds allow more solar radiation to pass, which warms the layers of the atmosphere below. Low clouds are often dense and reflect a lot of sunlight back into space. They are also lower in the atmosphere, where temperatures are higher, and therefore give off more heat. The tendency of low clouds is therefore to cool the earth.

High clouds are usually thin and not very reflective. Although they allow a large part of the solar heat to pass through, they reduce the amount of sunlight irradiated somewhat, so that the photosynthetic performance of green plants is also impaired by high cirrus veils or many contrails , but at night the heat radiation from the earth's surface and thus the nightly cooling is somewhat reduced. Because they are very high where the air temperature is very low, these clouds do not give off much heat. The tendency of high clouds is to warm the earth a little at night.

The vegetation and the nature of the soil and in particular its sealing , deforestation or agricultural use have a significant influence on evaporation and thus on cloud formation and the climate. A reduction in cloud formation by plants has also been proven: these emit up to 15 percent less water vapor with an increase in CO 2 ; this in turn reduces cloud formation.

Overall, cloud feedback is likely to exacerbate global warming. A simulation published in 2019 suggests that at a CO 2 concentration above 1,200 ppm stratocumulus clouds could break up into scattered clouds, which would further fuel global warming.

Influence of vegetation and soil

Percent of the reflected sunlight depending on the different surface conditions of the earth

Vegetation and soil reflect the incident sunlight differently depending on their nature. Reflected sunlight is thrown back into space as short-wave solar radiation (otherwise the surface of the earth would be black from the perspective of space without an infrared camera). The albedo is a measure of the retroreflective power of diffusely reflective (re-emitting), i.e. non-reflective and non-luminous surfaces.

surfaces Albedo in%
Settlements 15 to 20
Tropical rain forest 10 to 12
Deciduous forest 12 to 15
Cultural areas 15 to 30
Grassland 12 to 30
Arable land 15 to 30
Sandy soil 15 to 40
Dune sand 30 to 60
Glacial ice 30 to 75
asphalt 15th
Clouds 60 to 90
water 5 to 22

Not only the consumption of fossil fuels leads to the release of greenhouse gases. Intensive cultivation of arable land and deforestation are also significant sources of greenhouse gas. For the process of photosynthesis, the vegetation needs CO 2 to grow. Soil is an important sink because it contains organic, carbonaceous matter. This stored carbon is more easily released in the form of CO 2 through agricultural activities such as plowing , because more oxygen can enter the soil and the organic material is broken down more quickly. Methane releases from wetlands are likely to increase with rising temperature ; There is still uncertainty about the level of the release (as of 2013).

In the permafrost of western Siberia store 70 billion tons of methane in oceans have on the continental slopes much larger quantities in the form of methane hydrate deposited. Due to local climate changes (currently: +3 K within 40 years in Western Siberia), regionally critical temperatures could be reached even with low global warming; there is a risk of the methane stored there being released into the atmosphere.

A calculation assuming such feedback was made by scientists at the University of California, Berkeley , who assumed that the CO 2 content of the atmosphere will increase from the current approximately 390 ppmV to approximately 550 ppmV by 2100. This is solely the anthropogenic increase brought about by mankind. The increased temperature leads to additional release of greenhouse gases, especially CO 2 and methane. As the temperature rises, there is an increased release of CO 2 from the world's oceans and the accelerated rotting of biomass, which releases additional methane and CO 2 . Through this feedback , global warming could be 2 K more than was assumed in 2006. For this and other reasons, Barrie Pittock estimates in Eos, the American Geophysical Union publication , that future warming could exceed the ranges stated by the IPCC. He gives eight reasons for his assumption, including the decline in global darkening and feedback effects from biomass.

Projected warming

Projections of temperature development up to 2100
The NASA video (English, German subtitles) shows temperature and precipitation simulations for the 21st century. It is based on the four representative concentration paths (RCPs) of the 5th IPCC assessment report with the increase in CO₂ levels in the air to 421  ppm (RCP 2.6), 538 ppm (RCP 4.5), 670 ppm (RCP 6.0) and 936 ppm (RCP 8.5) in the year 2100. The colors show the development of the temperatures compared to the average values ​​in the period 1971 to 2000.

If the CO 2 concentration in the atmosphere doubles , climatologists assume that the increase in the mean temperature of the earth will be within 1.5 to 4.5 K. This value is also known as climate sensitivity and is related to the pre-industrial level (from 1750), as is the radiative forcing which is decisive for it ; With this size all known factors influencing the radiation balance of the earth are quantitatively described by the IPCC and made comparable. According to the 5th Assessment Report, the IPCC expects the global average temperature to increase by 1.0 to 3.7 K by the year 2100 (based on 1986-2005 and depending on the GHG emission path and the climate model used). For comparison: the fastest warming in the course of the last ice age to the present warm period was a warming of about one degree per 1000 years.

According to a study at the Carnegie Institution for Science , in which the results of a carbon cycle model were evaluated with data from comparative studies between climate models of the fifth IPCC assessment report, the global climate system reacts to a CO 2 input with a time delay of about 10 years with a step function; this means that the warming reaches its maximum after about 10 years and then remains there for very long periods of time.

The Climate Action Tracker indicates the most likely global warming to be expected by the end of this century. Accordingly, the world is currently (2016) on the way to a warming of 3.6 ° C compared to the pre-industrial global average temperature. To calculate this value, the voluntary commitments of the most important emitters to reduce greenhouse gas emissions are fed into a climate model.

Long-term consideration and the resulting consequences

According to a study published in 2009, the warming that has already started will be irreversible for at least 1000 years, even if all greenhouse gas emissions were to be completely stopped today. In other scenarios, the emissions continued gradually until the end of our century and then also ended abruptly. In doing so, essential assumptions and statements made in the 4th IPCC report over the next 1000 years were confirmed and refined. Long-term climate simulations indicate that the earth, heated by an increased carbon dioxide concentration, will only cool down by about one degree per 12,000 years.

A complete burning of the fossil energy resources , which are conservatively estimated at 5 trillion tons of carbon , would, however, lead to a global temperature increase of about 6.4 to 9.5 ° C, which has very strong negative effects on ecosystems , human health , agriculture, the economy etc. would have. If both conventional and unconventional resources were burned, the carbon dioxide concentration in the earth's atmosphere could rise to around 5000 ppm by the year 2400. In addition to an enormous increase in temperature, the Antarctic ice sheet would almost completely melt, which would cause the sea level to rise by approx. 58 m even without taking the Greenland ice sheet into account .

Projections 2050

In 2019, the Crowther Lab at ETH Zurich forecast the temperatures in 520 metropolises worldwide for the year 2050. For 22% of the cities, climatic conditions are forecast that are currently not found in any city in the world. The others are forecasted with conditions that currently correspond to another city. Vienna, for example, should have a climate similar to Skopje , Hamburg like San Marino , Berlin and Paris like Canberra in Australia, London like Melbourne , Athens and Madrid like Fez in Morocco, Nairobi should have a climate similar to Maputo . New York should have a climate like Virginia Beach , Virginia Beach like Podgorica , Seattle like San Francisco, Toronto like Washington DC, Washington DC like Nashville .

State of research

History of science

Svante Arrhenius , one of the pioneers in the history of the science of global warming

In 1824, Jean Baptiste Joseph Fourier discovered the greenhouse effect. Eunice Newton Foote was the first to experimentally investigate the effect of solar radiation on hermetically sealed glass tubes filled with various gases. She demonstrated the absorption of thermal radiation by carbon dioxide and water vapor , recognized this as a possible cause of climate change events and published her results in 1856. This became known only in 2010 ; In 1859, John Tyndall succeeded in specifically demonstrating the absorption of long-wave infrared radiation emanating from the earth's surface by greenhouse gases; he determined the relative importance of water vapor compared to carbon dioxide and methane for the natural greenhouse effect. Following up on Tyndall, Svante Arrhenius published the hypothesis in 1896 that anthropogenic CO 2 accumulation in the atmosphere could increase the temperature of the earth. It was then that the “science of global warming” in the narrower sense began.

In 1908, the British meteorologist and later President of the Royal Meteorological Society Ernest Gold (1881-1976) published an essay on the stratosphere . In it he wrote that the temperature of the tropopause rises with increasing CO 2 concentration. This is a hallmark of global warming that could also be measured almost a century later.

It was first demonstrated in the late 1950s that the carbon dioxide content of the atmosphere was rising: on the initiative of Roger Revelle , Charles David Keeling started regular measurements of the CO 2 content of the atmosphere ( Keeling curve ) on Mount Mauna Loa ( Hawaii , Big Island) in 1958 ). Gilbert Plass first used computers in 1956 and much more accurate absorption spectra of CO 2 to calculate the expected warming. He received 3.6 K (3.6 ° C) as a value for the climate sensitivity .

The first computer programs for modeling the world's climate were written in the late 1960s.

In 1979 the National Academy of Sciences wrote in the " Charney Report" that an increase in carbon dioxide concentration was undoubtedly linked to significant global warming; However, due to the inertia of the climate system, significant effects are only to be expected in a few decades.

US climate scientist James Hansen said on June 23, 1988 before the Energy and Natural Resources Committee of the US Senate , he was 99 percent sure that the respective annual record temperature was not the result of natural fluctuations. This is considered to be the first such statement by a scientist before a political body. As early as this meeting, calls were made for political measures to slow global warming. The Intergovernmental Panel on Climate Change ( IPCC ) was founded in November 1988 to assist political decision-makers and governments: Here, the scientific state of knowledge on global warming and the anthropogenic part of it is discussed, agreed and summarized in reports.

The anthropogenic global warming in the context of the earth's history

Research into the causes and consequences of global warming has been closely linked to the analysis of climatic conditions of the past since its inception. Svante Arrhenius, who was the first to point out that humans warm the earth through the emission of CO 2 , recognized the climatic influence of changing concentrations of carbon dioxide in the earth's atmosphere while searching for the causes of the ice ages.

Like earthquakes and volcanic eruptions, climate change is also natural. Earth's climate has changed constantly since the earth was formed, and it will continue to change in the future. Primarily responsible for this were a changing concentration and composition of greenhouse gases in the atmosphere due to the different intensity of volcanism and erosion. Other climate-affecting factors are the variable solar radiation, among other things due to the Milanković cycles , as well as a permanent reshaping and shifting of the continents caused by the plate tectonics with a resulting shift of large ocean currents. Land masses at the poles encouraged the formation of ice caps, and altered oceanic currents directed heat either away from or towards the poles, thus affecting the strength of the very powerful ice-albedo feedback .

Although the luminosity and radiant power of the sun at the beginning of the earth's history were about 30 percent below today's values, conditions prevailed throughout that time under which liquid water could exist. This phenomenon, known as the weak young sun paradox , led to the hypothesis of a “CO 2 thermostat” in the 1980s : It kept the temperatures of the earth constant for billions of years in areas that made life on our planet possible. When volcanoes emitted more CO 2 , so that the temperatures rose, the degree of weathering increased, whereby more CO 2 was bound. If the earth was cold and the concentration of greenhouse gas was low, weathering was greatly reduced by the icing of large areas of land. The greenhouse gas that continued to flow into the atmosphere as a result of volcanism accumulated there up to a certain tipping point, eventually triggering a global thaw. The disadvantage of this mechanism is that it takes several millennia to correct for greenhouse gas levels and temperatures, and there are several known cases where it failed.

Phanerozoikum Eiszeitalter#Ordovizisches Eiszeitalter Eiszeitalter#Permokarbones Eiszeitalter Perm-Trias-Ereignis Paläozän/Eozän-Temperaturmaximum Kreide-Paläogen-Grenze Känozoisches Eiszeitalter Kreide-Paläogen-Grenze Paläozän/Eozän-Temperaturmaximum Eocene Thermal Maximum 2 Eem-Warmzeit Letzteiszeitliches Maximum Atlantikum Jüngere Dryaszeit Globale Erwärmung Warmklima Eiszeitalter Kambrium Ordovizium Silur Devon (Geologie) Karbon Perm (Geologie) Trias (Geologie) Jura (Geologie) Kreide (Geologie) Paläogen Neogen Quartär (Geologie) Paläogen Neogen Quartär (Geologie) Paläozän Eozän Oligozän Miozän Pliozän Pleistozän Holozän Christopher Scotese Christopher Scotese James E. Hansen James E. Hansen James E. Hansen EPICA EPICA Greenland Ice Core Project Delta-O-18 Repräsentativer Konzentrationspfad
Clickable reconstructed temperature curve of the Phanerozoic. The values ​​for 2050 and 2100 are based on the 5th assessment report by the IPCC, assuming a continuously increasing CO 2 concentration. - The graph shows how strongly the global temperature fluctuated in the course of the earth's history, while it was almost consistently lower in the last 2.6 million years than today.

It is believed that the great oxygen catastrophe 2.3 billion years ago caused a collapse in methane concentrations in the atmosphere. This reduced the greenhouse effect so much that it resulted in extensive and long-lasting glaciation of the earth during the Huronian Ice Age . In the course of - probably several - Snowball Earth events during the Neoproterozoic around 750 to 635 million years ago, the earth's surface froze again almost completely.

The last such event occurred just before the Cambrian explosion 640 million years ago and is called the Marino Ice Age . The bright surface of the almost completely frozen earth reflected almost all of the incident solar energy back into space and thus kept the earth trapped in the ice age state; This only changed when the concentration of carbon dioxide in the earth's atmosphere rose to extremely high levels due to the volcanism that continued beneath the ice. Since the CO 2 thermostat only reacts slowly to changes, the earth not only thawed, but also plunged into the other extreme of a super greenhouse for several decades. The extent of the icing is, however, controversial in science because climate data from this time are imprecise and incomplete. According to recent studies, a similar constellation occurred at the Carbon-Permian transition about 300 million years ago when the atmospheric carbon dioxide concentration decreased to a minimum of probably 100 ppm. As a result, the earth's climate system moved into the immediate vicinity of the tipping point that would have brought the planet into the climatic state of global icing.

In contrast, at the time of what was probably the greatest mass extinction 252 million years ago , the earth was a super greenhouse with much higher temperatures than today. This drastic increase in temperature, which wiped out almost all life on earth at the Permian Triassic border , was very likely caused by a long-lasting intense volcanic activity that led to the formation of the Siberian Trapps . Current isotope studies indicate that the seas of that time warmed by up to 8 K within a relatively short period of time and, at the same time, became strongly acidic. During these and other periods of extremely high temperatures, the oceans were largely devoid of oxygen. Such oceanic anoxic events were repeated several times in the history of the earth. We now know that phases of strong cooling, such as during the Grande Coupure , as well as rapid warming were accompanied by mass extinctions . The paleontologist Peter Ward even claims that all known mass extinctions in Earth's history, with the exception of the KT impact , were triggered by climate crises.

Global increase in average temperatures of the last 10,000 years since the Neolithic Revolution and the temperature increase expected at the end of the 21st century for three different assumptions about climate sensitivity with unchecked emissions ("business as usual" scenario)

The climate of the past 10,000 years has been unusually stable compared to the frequent and strong fluctuations of the previous millennia. This stability is a basic requirement for the development and continued existence of human civilization . Most recently, rapid and strong global warming occurred during the Paleocene / Eocene temperature maximum and at Eocene Thermal Maximum 2 , which was caused by a massive input of carbon (CO 2 and / or methane) into the atmosphere. These epochs are therefore the subject of intensive research in order to gain knowledge about the possible effects of ongoing man-made warming.

The current climate change, which is expected for the coming years, may have the magnitude of the major climate change in the history of the earth, but the predicted coming temperature change is at least 20 times faster than in all global climate changes of the last 65 million years. Looking at the rate of heating phases of ice ages to interglacial periods , such as five times occurred in the last 500,000 years, so it was there in each case to periods of rapid warming. These phases each lasted about 10,000 years and were characterized by a temperature rise of about 4 to 5 ° C. The temperature rose by around 4 to 5 hundredths of a degree per century. These historical temperature rises were thus around a factor of 100 slower than the currently observed man-made warming, in which temperature rises of 4 to 5 ° C are expected within a century, provided that no significant climate protection measures are taken.

Based on the almost two hundred years of extensive data and research, it can be assumed that the Pliocene epoch can be an analogous example for the near future of our planet. The carbon dioxide content of the atmosphere in the Middle Pliocene was determined with the help of the isotope investigation of Δ13C and was then in the range of 400 ppm, which corresponds to the concentration in 2015. With the help of climate proxies , the temperature and sea level of the time 5 million years ago can be reconstructed. At the beginning of the Pliocene, the global mean temperature was 2 K higher than in the Holocene ; Due to the enormous heat capacity of the world's oceans, the global annual average temperature reacts very slowly to changes in radiative forcing and has only increased by about 1 K since the beginning of the industrial revolution.

The warming leads, among other things, to a rise in sea level . In the middle of the Pliocene, the sea level was around 20 meters higher than it is today.

Every few years, the Intergovernmental Panel on Climate Change (IPCC) summarizes the scientific knowledge about global warming

The IPCC

The Intergovernmental Panel on Climate Change (IPCC) was set up in 1988 by the United Nations Environment Program (UNEP) together with the World Meteorological Organization (WMO) and is associated with the Framework Convention on Climate Change , which was concluded in 1992 . For its reports, which appear every six years, the IPCC summarizes the worldwide research results in the field of climate change and thus reflects the current state of knowledge in climatology.

The organization was awarded the Nobel Peace Prize in 2007, together with former US Vice President Al Gore . The fifth assessment report was published in September 2013.

How sure are the findings on global warming?

Selection of different decidedly human fingerprints of the current global warming

Since the discovery of the greenhouse effect in the atmosphere by Jean Baptiste Joseph Fourier in 1824 and the description of the greenhouse effect of water vapor and carbon dioxide by John Tyndall in 1862, scientific research into the Earth's climate system has become more and more precise. There is now "overwhelming evidence" that global warming is real, man-made and a major threat.

The warming effect of greenhouse gases has been known for 150 years and the increase in concentration in the earth's atmosphere could then be reliably demonstrated in the mid-1950s. The pronounced and uninterrupted global warming that has been observed since the mid-1970s cannot be attributed primarily to solar influences or other natural factors with the help of the measurement technology that has been significantly improved since then, as these have only changed minimally since then. Fundamental research on the effects of greenhouse gases was carried out by oceanographer Veerabhadran Ramanathan in the mid-1970s.

Hundreds of thousands of climatological studies have since been published, the vast majority (around 97%) of which support the scientific consensus on climate change. Projections and calculations that were made decades ago were still quite wide, but overall they hit the trend surprisingly well. If the models are fed with more up-to-date measurements, especially the radiation balance between the upper atmosphere and space, then the scatter between the models decreases and the mean value for warming at the end of the century increases somewhat.

Trends and exact times

In climate research, one differentiates between trend and point in time and calculates the probability of occurrence. In the context of global warming, for example, the following is not exactly known: Several event times, including the time when the Arctic will be ice-free in summer in the 21st century; The exact sea level rise by the end of the 21st century is also unknown. Uncertainties exist in the exact type, shape, location and distribution of global tipping points in the climate system and, associated with this, in the knowledge of the precise regional effects of global warming. The majority of the relevant scientific principles, however, are considered to be very well understood.

The scientific consensus on climate change

97% of all climatologists support the scientific consensus regarding man-made climate change

The topic of global warming was initially the subject of controversial discussions with changing focuses. At the beginning of the 20th century, the uncertainty prevailed as to whether the theoretically predicted warming would be measurable at all. When a significant rise in temperature was first registered in some regions of the USA during the 1930s, this was regarded as a strong indicator of increasing global warming, but at the same time it was doubted whether this process was actually based on human influences. These doubts are expressed by some allegedly climate-skeptical groups to this day, and occasionally the media even predict a global cooling for the coming decades, which is rejected by climate researchers.

Today there is a consensus among experts on man-made global warming that has existed since the early 1990s at the latest. Other sources date the establishment of the scientific consensus as early as the 1980s. So held z. For example, the interim report published in 1988 by the Enquete Commission on Precautions to Protect the Earth's Atmosphere found that a consensus on the existence and human causes of climate change had already been reached at the 1985 Villach climate conference :

“In Villach (Austria, 1985), scientists from all over the world agreed for the first time that the global average temperature near the ground would increase. There was also consensus that the human-induced increase in the concentrations of climate-relevant greenhouse gases in the atmosphere, especially that of carbon dioxide (CO 2 ), methane (CH 4 ), tropospheric ozone, nitrous oxide (N 2 O) and chlorofluorocarbons (CFC), leads to an increase in temperature. "

- Enquete Commission on Precautions to Protect the Earth's Atmosphere of the German Bundestag , November 1988.

The scientific consensus expressed in the IPCC reports is expressly shared by the national and international science academies and all G8 countries.

The scientific consensus on climate change is that the Earth's climate system is warming and will continue to warm. This is determined on the basis of observations of the increasing average temperature of the air and oceans, large-scale melting of snow and ice surfaces and the rise in sea level . With at least 95 percent certainty, this is mainly caused by greenhouse gases (burning of fossil fuels, methane emissions from livestock farming, release of CO 2 during cement production) and the clearing of forest areas. The American Association for the Advancement of Science - the world's largest scientific society - shows that 97% of climatologists agree that human-made climate change is happening, and emphasizes the consensus that exists on many aspects of climatology. Since the turn of the millennium at the latest, the level of knowledge about the consequences of climate change has been viewed as sufficiently reliable to justify extensive climate protection measures.

According to a study published in 2014, assuming no anthropogenic greenhouse effect, there was only a probability of 0.001% for the event actually occurring for at least 304 months in a row (from March 1985 to the status of the analysis in June 2010) with a monthly mean of the global temperature above the mean for the 20th century.

Denial of man-made global warming

Jim Inhofe at a 2015 Senate speech in which he used a snowball to argue against the existence of global warming.

Although there has been a strong scientific consensus on man-made global warming for decades, parts of the public and a large number of political and economic actors continue to reject the existence of climate change, its human cause, the associated negative consequences or the scientific consensus about it . The denial of man-made climate change is a form of pseudoscience that has similarities with other forms of scientific denial, such as denying the theory of evolution or the health-damaging effects of smoking to believing in conspiracy theories . In part, there are personal, organizational and economic connections between these forms of denial of scientific knowledge. A central connection pattern is, among other things, the constant fabrication of artificial controversies such as the alleged controversy about global warming , which, contrary to popular belief, is not a scientific discussion, but rather the conscious dissemination of false claims by climate deniers. The denial of climate research is considered to be “by far the most coordinated and financed form of science denial” and at the same time represents the backbone of the anti- environmental movement and its opposition to environmental research .

The rejection of the scientific consensus is particularly pronounced in countries in which an influential counter-movement has been created with great financial commitment by companies, especially from the fossil energy sector , whose aim is to confirm the existence of the scientific consensus by consciously sowing doubts to undermine. These actions were particularly successful among conservative sections of the population in the USA. Conservative think tanks play an important role in obscuring the state of the art .

The most important forces of the organized climate denial movement , which deny the existence of man-made global warming through targeted attacks on climate research, include the Cato Institute , the Competitive Enterprise Institute , the George C. Marshall Institute and the Heartland Institute , all of which are conservative think tanks. Its aim was and is to use the Fear, Uncertainty and Doubt strategy to create uncertainty and doubts about the existence of global warming in the population, and then to argue that there is not enough evidence to support concrete climate protection measures. In total, the US climate contrarian movement has around $ 900 million a year for campaign purposes. The overwhelming majority of funding comes from politically conservative organizations, with funding increasingly being disguised through donors trust organizations . The majority of the literature that contradicts man-made climate change has been published without peer review , is usually of a pseudoscientific nature (i.e. looks outwardly scientific, but does not meet scientific quality standards), was largely funded by organizations and companies that benefit from the use of fossil fuels benefit, and is associated with conservative think tanks.

Consequences of global warming

Global warming is fraught with risks because of its effects on human safety , health , the economy and the environment . These risks become greater with increasing warming and are higher at 2 degrees warming than if global warming is limited to 1.5 degrees. The negative effects of global warming are already occurring today and may have a. already affected many ecosystems on land and in water. Some changes that are already noticeable today, such as reduced snow cover, rising sea levels or glacier melt, are considered to be evidence of climate change in addition to temperature measurements. Consequences of global warming have a direct impact on both humans and ecosystems . In addition, climate change exacerbates many other serious problems such as B. species loss or soil degradation , so that combating climate change is also a key measure for solving other urgent problems on the way to a sustainable way of life.

Scientists project various direct and indirect effects on the hydrosphere, atmosphere, and biosphere. In the report of the Intergovernmental Panel on Climate Change ( IPCC ) these projections are assigned probabilities. The consequences include heat waves, especially in the tropics, a rise in sea level that affects hundreds of millions of people, and crop failures that threaten global food security . According to a World Bank report, a world that is warming up strongly is associated with considerable adverse effects for people.

Unexpected changes and "tipping points"

Different tilting elements in the earth system

A distinction is made between at least two types of unexpected effects: combined effects, in which several extreme events act together and mutually reinforce their effects (e.g. droughts and large fires), and tipping elements . Due to the multiple feedbacks in the earth system, this often reacts to influences non-linearly, which means that changes in these cases do not take place continuously, but erratically. There are a number of tipping elements which, as the temperature progresses, will likely adopt a new state abruptly, which at a certain point ( tipping point ) will be difficult or impossible to reverse. Examples of tipping elements are the melting of the arctic ice sheet or a slowdown in thermohaline circulation .

Other examples of abrupt events are the sudden extinction of a species that - possibly pre-stressed by other environmental factors - is eliminated by an extreme climatic event, or the effect of rising sea levels. These do not lead directly to flooding, but only if in the context of z. B. storm surges a previously sufficient dam is flooded. The rise in sea level itself can also accelerate rapidly in a very short time due to non-linear effects, as was the case in climatic history, for example, with meltwater pulse 1A .

Studies of climatic changes in the history of the earth show that climate change in the past was not only gradual and slow, but sometimes very quickly. At the end of the Younger Dryas and during the Dansgaard-Oeschger events in the last glacial period, a regional warming of 8 ° C was observed in about 10 years. Based on what we know today, it seems likely that these rapid jumps in the climate system will also take place in the future when certain tipping points are exceeded. Since the possibility of depicting the climate in climate models will never fully correspond to reality, the climate system cannot be predicted in detail due to its chaotic nature and the world is increasingly moving outside the range for which reliable past climate data are available, neither can The type, extent and timing of such events can be predicted.

However, Will Steffen and others calculated the probable temperature ranges of global warming in 2018, in which critical thresholds for tipping elements can be reached, so that "they are put into fundamentally different states." Feedback could trigger further tipping elements, whose change only for higher temperature ranges is to be expected. The thermohaline circulation is influenced by a strong melting of the Greenland ice , which is possible even with a global warming between 1 and 3 degrees . Their collapse is in turn linked to the El Niño-Southern Oscillation , the partial withering of the Amazon rainforest and the melting of the Antarctic sea , later mainland ice . Even if the climate target of 2 degrees global warming is met , there is a risk of a domino effect , a cascade that would lead the climate uncontrollably and irreversibly into a warm climate , with temperatures around 4 to 5 degrees higher in the long term and a rise in sea level of 10 to 60 meters.

Effects on the biosphere

The risks to ecosystems on a warming earth grow with each degree of temperature rise. The risks below a warming of 1 K compared to the pre-industrial value are comparatively low. Between 1 and 2 K warming, there are sometimes substantial risks at the regional level. A warming above 2 K carries increased risks for the extinction of numerous animal and plant species whose habitats no longer meet their requirements. For example, the IPCC assumes that global coral reefs will decline by 70-90% with a warming of 1.5 degrees. If the temperature rises by 2 degrees, the IPCC anticipates a decline of more than 99% and thus an almost complete disappearance of the coral reefs. If the temperature rises by more than 2 K, there is a risk of collapse of ecosystems and significant effects on water and food supplies due to crop failure.

  • Plant growth has increased in recent decades due to increased amounts of precipitation, temperature and CO 2 content in the atmosphere. Between 1982 and 1999 it rose by six percent on a global average, particularly in the tropics and the temperate zone of the northern hemisphere .
  • Risks to human health are in part a direct consequence of rising air temperatures . Heat waves will become more common, while extreme cold events will likely become less frequent. While the number of heat deaths is likely to increase, the number of cold deaths will decrease.
  • Despite global warming, cold events can occur locally and temporarily. Climate simulations predict, for example, that the melting of the Arctic ice can lead to severe disruptions in air currents. This could triple the likelihood of extremely cold winters in Europe and North Asia.
  • Agricultural productivity will be affected by both a rise in temperature and a change in rainfall. Roughly speaking, a deterioration in production potential can be expected globally . The extent of this negative trend is, however, fraught with uncertainty, as it is unclear whether a fertilization effect occurs due to increased carbon concentrations (−3%) or not (−16%). According to model calculations, however, tropical regions will be more severely affected than temperate regions, in which, with carbon fertilization, even significant increases in productivity are expected in some cases. For example, India is expected to drop by around 30–40% by 2080, while estimates for the United States and China are between −7% and +6%, depending on the carbon fertilization scenario. Added to this are likely changes in the distribution areas and populations of pests. According to model calculations, if climate change continues unchecked, around 529,000 deaths are expected annually as a result of poor nutrition, in particular the decline in fruit and vegetable consumption . With a strict climate protection program (implementation of the RCP 2.6 scenario), however, the number of additional deaths could be limited to around 154,000.
  • There will be changes in human and animal health risks as a result of changes in the range, population, and infection potential of disease vectors .

Effects on the hydrosphere and atmosphere

In the period from 1993 to 2017 , the sea level rose by 3.4 mm per year. This is 50% more than the average increase in the 20th century.
  • Rising air temperatures are changing the distribution and extent of precipitation worldwide. According to the Clausius-Clapeyron equation , the atmosphere can absorb approx. 7% more water vapor with every degree of temperature increase , which in turn acts as a greenhouse gas . As a result, the average amount of precipitation will increase globally, but the drought will also increase in individual regions, on the one hand due to the decrease in the amount of precipitation there , but also due to the accelerated evaporation at higher temperatures .
  • The increasing evaporation leads to a higher risk of heavy rain , floods and floods .
  • Glacier melt is increasing worldwide .
  • In the course of global warming, sea ​​levels rise . This increased by 1–2 cm per decade in the 20th century and is accelerating; at the beginning of the 21st century the rate was 3–4 cm. By the year 2100 the IPCC expects a further sea level rise of probably 0.29–0.59 m with strict climate protection and 0.61–1.10 m with further increasing greenhouse gas emissions; a sea level rise of up to 2 m cannot be ruled out. In the long term, it is assumed that the sea level will rise by around 2.3 m per additional degree Celsius of warming.
  • According to the World Meteorological Organization, there are so far indications for and against the presence of an anthropogenic signal in the previous records of tropical cyclones , but so far no firm conclusions can be drawn. The frequency of tropical storms is likely to decrease, but their intensity will increase.
  • There are indications that global warming via a change in Rossby waves (large-scale oscillations of air currents) leads to an increased occurrence of weather extremes (e.g. heat waves , floods).

Peace and world order, politics

In its Global Risks 2013 report, the World Economic Forum Davos classifies climate change as one of the most important global risks: The interplay between the stress on economic and ecological systems will present unpredictable challenges for global and national resilience.

Various military strategists and security experts fear geopolitical upheavals as a result of climate change, which harbors security policy risks for the stability of the world order and " world peace ". The UN Security Council also issued a corresponding declaration in 2011 on Germany's initiative. The former German Foreign Minister Frank-Walter Steinmeier also rated climate change as “a growing challenge for peace and stability” in April 2015 after the publication of a European study for the “ G7 ” Foreign Ministers' Meeting in Lübeck . The study recommends u. a. the establishment of a G7 task force .

Social science aspects

economy

According to current estimates, the economic consequences of global warming are considerable: In 2004/5, the German Institute for Economic Research estimated that if climate protection is not implemented quickly, climate change could result in economic costs of up to 200,000 billion US dollars by 2050 (although this estimate involves large Is fraught with uncertainties). The Stern Report (commissioned by the then British government in mid-2005) estimated the damage to be expected from climate change by the year 2100 at 5 to 20 percent of global economic output.

According to a Lancet report published in the run-up to the 23rd UN Climate Change Conference (" COP 23 ") in Bonn in November 2017 , the number of weather-related natural disasters has increased by 46% since 2000; In 2016 alone, this caused economic damage of $ 126 billion.

See also “ Climate Finance ”, Climate Insurance , Loss and Damage , Corporate Climate Risks

Limit global warming

In order to stabilize the earth's temperature and limit the consequences of global warming, global greenhouse gas emissions must be limited to net zero, as only a certain global CO 2 budget is available for each temperature target . Conversely, this means that global warming continues as long as greenhouse gases are emitted and the total amount of greenhouse gases in the atmosphere increases. Simply reducing emissions does not stop global warming, it only slows it down.

Climate policy

Greenhouse gases accumulate evenly in the atmosphere, their effect does not depend on where they are emitted. A reduction in greenhouse gas emissions thus benefits everyone; but it is often associated with efforts and costs for those who reduce their greenhouse gas emissions. The reduction of global emissions to net zero thus faces the so-called free rider problem : Actors who are predominantly self-interested want a stabilization of the climate and corresponding climate protection efforts by others, but do not see sufficient incentives for their own climate protection efforts. International climate policy is faced with the task of creating a global regulatory framework that brings about collective action towards climate neutrality .

history

The two-degree target was agreed by the heads of state and government of major economies at the G8 summit in L'Aquila in 2009 .

As the heart of international climate policy that applies Framework Convention on Climate Change (UNFCCC) of the United Nations as the international law binding regulation to climate protection. It was adopted in New York City in 1992 and signed by most states in the same year at the UN Conference on Environment and Development ( UNCED ) in Rio de Janeiro . Its main goal is to avoid dangerous disruption of the climate system as a result of human activity. The framework convention is a newly emerged principle of the community of states that a reaction to such a massive threat to the global environment should be made without precise knowledge of the ultimate actual extent. Agenda 21 was also adopted at the Rio conference and has since been the basis for many local protective measures.

The 197 contracting parties of the Framework Convention (as of March 2020) meet annually for UN climate conferences . The most famous of these conferences were in 1997 in Kyoto , Japan , which resulted in the Kyoto Protocol , in Copenhagen in 2009 and in Paris in 2015 . All contracting states agreed there to limit global warming to well below 2 ° C compared to pre-industrial times. The aim is to limit the temperature to 1.5 ° C.

The two-degree goal

Necessary emission paths to meet the two-degree target agreed in the Paris Agreement without negative emissions, depending on the emission peak

As a limit from a tolerable to a “dangerous” disruption of the climate system, an average warming of 2 ° C compared to the pre-industrial level is commonly assumed in climate policy. The fear that beyond 2 ° C the risk of irreversible, abrupt climate changes increases significantly. In Germany, the German Advisory Council on Global Change (WBGU) recommended in 1994 that mean warming be limited to a maximum of 2 ° C. The Council of the European Union adopted the target in 1996. The G8 recognized it at the G8 summit in July 2009. In the same year it found its way into the UN framework as part of the Copenhagen Accord and was adopted in a legally binding form in 2015; the Paris Agreement came into force in November 2016.

However, the requirement is noticeably moving into the distance: Since a warming of 1.1 ° C has already occurred (as of 2019), only 0.9 ° C remains. In scenarios that are still considered feasible, greenhouse gas emissions would have to reach their maximum as early as 2020 and then decrease rapidly to achieve the target. According to a report by the United Nations Environment Program released in November 2019, there are no signs that emissions will peak in the next few years. Should the signatory states to the Paris Agreement reduce their emissions as promised by 2016 (→  National Climate Protection Contribution ), global warming of 2.6 to 3.1 ° C will result by 2100 and a further rise in temperature after 2100. Compliance with the two Degree limit, a subsequent tightening of the commitments or an overachievement of the goals are therefore imperative.

The rise in sea level would not have stopped with the two-degree limit. The sometimes significantly stronger warming over the land areas brings further problems. Temperatures are expected to rise particularly sharply over the Arctic . For example, indigenous peoples declared the two-degree target to be too weak because it would still destroy their culture and way of life, be it in arctic regions, in small island states as well as in forest or dry areas.

Economic debate

In the social science literature, various political instruments for reducing greenhouse gas emissions are recommended and Sometimes discussed controversially. In economic analyzes, there is broad consensus that pricing CO 2 emissions that internalizes the damage caused by climate change as much as possible is a central instrument for effective and cost-efficient climate protection. Such CO 2 prize , by controlling, emissions trading of both instruments can be realized, or combinations. Some scientists such as B. Joachim Weimann recommend global emissions trading as the most efficient instrument on its own. Other economists such as For example, the British energy scientist Dieter Helm, on the other hand, consider a CO 2 tax more suitable because it is more stable than the fluctuating CO 2 prices in emissions trading, which are too difficult for companies to calculate. Others (eg. As the American political Economist Scott Barrett) argue that state prescribed technical standards (certain CO 2 low-carbon or CO 2 as in -free production technologies and consumer goods such as, for. Example, passenger car) Montreal Protocol for Protection of the ozone layer could be politically enforced far better in international politics than a global emissions trading scheme or a CO 2 tax. The social scientist Anthony Patt also sees emissions trading as insufficiently effective in real politics, since political resistance to sufficient (i.e. sufficient for decarbonization ) strongly rising or high CO 2 prices, especially from energy-intensive industries, is too great. As with EU emissions trading , CO 2 prices would therefore only fluctuate at a low level, so that (in the case of emissions trading alone), capital-intensive, long-term future investments in CO 2 -free technologies would not be worthwhile for potential eco-investors . To do this, they would need the certain expectation that CO 2 prices will rise and remain high in the future, so that they can foreseeably assert themselves on the competitive market against competitors who use CO 2 -intensive technologies. However, the political system cannot reliably commit itself to a future reliably rising, high CO 2 price, since such political decisions are or would always be reversible in a democracy (for example, a CO 2 tax was first introduced in Australia and abolished after two years by a new, conservative government). This is also known as the “commitment problem” of climate policy.

Therefore, Anthony Patt advocates laws to subsidize CO 2 -free technologies such as For example, the Renewable Energy Sources Act (EEG) in Germany, which creates precisely this security of expectations for potential investors in CO 2 -free technologies: The EEG guarantees (at least until the 2016 EEG amendment) a producer of electricity Renewable energies for a long period of time (20 years) a certain sales price that is above the market level This guarantee is subject to the constitutional protection of legitimate expectations. Secured in this way, investors in renewable energies have succeeded in the last two decades by expanding the costs of generating electricity from renewable energies by learning by doing ( experience curve ) and gradually reducing electricity from fossil energy sources and Nuclear power to become competitive. Similar arguments, which emphasize the need to flank emissions trading through laws such as the EEG, can be found in the 2011 special report of the Council of Economic Experts for Environmental Issues or the energy economist Erik Gawel . Proponents of emissions trading counter this by saying that the state would intervene too strongly in the market and, in contrast to it, would select excessively expensive technologies for subsidization, since, unlike the market players, it did not have the knowledge about the most efficient technologies. As a result, economic resources would be wasted, so that society could afford less climate protection than actually possible (i.e. with ideal emissions trading).

Climate protection

German electricity generation costs (LCoE) for renewable energies and conventional power plants in 2018.

Political requirements for climate protection must be implemented through appropriate measures. On the technical side, there are a number of options for reducing greenhouse gas emissions that can be used to implement the energy transition. A study published in 2004 came to the conclusion that effective climate protection could already be achieved with the resources available at the time. The German Academy of Natural Scientists Leopoldina stated in a statement published in 2019 that, from a technical point of view, all requirements for the construction of a climate-neutral energy system are in place. In addition to the technologies, the concepts required for the energy transition are also known.

While in the past the costs for climate protection technology such. If, for example, renewable energies were significantly higher than for conventional technology, climate protection costs have now fallen significantly due to the rapid drop in prices. The IPCC put the cost of achieving the two-degree target in 2014 at 0.06% of the annual consumption growth rate. The earlier the greenhouse gas emissions are reduced, the lower the costs of climate protection.

The majority of recent studies assume that a renewable energy system can deliver energy at comparable costs to a conventional energy system. At the same time, climate protection would have strong positive economic side effects by avoiding consequential damage to the climate and avoiding air pollution from fossil fuels. The phase-out of coal is regarded as an important individual measure for achieving the two-degree target , as this allows the tight remaining budget of carbon dioxide emissions to be used as efficiently as possible. With more than 10 billion tonnes of CO 2 emissions in 2018, coal-fired power plants cause around 30% of the total energy-related carbon dioxide emissions of around 33 billion tonnes.

In its special report 1.5 ° C global warming , the IPCC lists the following criteria in order to still be able to achieve the 1.5 degree target:

  • Net zero carbon dioxide emissions by 2050 at the latest
  • strong reductions in other greenhouse gases, especially methane
  • Realization of energy savings
  • Decarbonisation of the electricity sector and other fuels
  • Electrification of final energy consumption (a form of sector coupling )
  • strong reduction in greenhouse gas emissions from agriculture
  • Use of some form of Carbon Dioxide Removal

Technical and individual options

Renewable energy
Wind turbines and photovoltaic systems are considered an essential part of climate protection using renewable energies .

The conversion of the energy system from fossil to renewable energy sources, the so-called energy turnaround , is seen as another indispensable part of an effective climate protection policy. The global potential is presented in the IPCC report. In contrast to fossil fuels, when using renewable energies, with the exception of bioenergy, no carbon dioxide is emitted, and this too is largely CO 2 -neutral . The use of renewable energies offers great potential, both ecologically and economically, above all by largely avoiding the consequential damage associated with other forms of energy, which as so-called external costs cause high economic welfare losses.

Basically, it can be said that renewable energies have a better environmental balance compared to conventional forms of energy use. Although the material requirements for these technologies are higher than for the construction of thermal power plants, the environmental impact due to the higher material requirements is low compared to the fuel-related direct emissions from fossil-fired power plants . By converting the energy supply to a regenerative energy system, the environmental pollution caused by the energy sector can be reduced. The vast majority of studies carried out on the topic come to the conclusion that the complete conversion of the energy supply to renewable energies is both technically possible and economically feasible.

Improve energy efficiency
By converting to energy-efficient lighting such as B. LED lamps can reduce the power consumption for lighting purposes by up to 80%.

Improving energy efficiency is a key element in achieving ambitious climate protection goals and at the same time keeping energy costs low. If energy efficiency increases, a service or a product can be offered or produced with less energy consumption than before. This means, for example, that an apartment needs less heating, a refrigerator requires less electricity or a car consumes less fuel. In all of these cases, the increasing efficiency leads to a decrease in energy consumption and thus to reduced greenhouse gas emissions. McKinsey also calculated that numerous energy efficiency measures simultaneously generate economic benefits.

In a global balance, however, the rebound effect must also be taken into account, which leads to increased energy or resource efficiency being partially offset by increased production of products or services. It is assumed that the energy savings through energy efficiency measures due to the rebound effect are reduced by an average of 10%, with values ​​from individual studies fluctuating between 0 and 30%.

Carbon Dioxide Removal

Carbon Dioxide Removal is understood to mean the removal of carbon dioxide from the atmosphere in order to artificially reduce the increased radiative forcing. Carbon dioxide removal can be achieved through the use of technologies for CO2 removal ("negative emissions"). These include:

The majority of the models come to the conclusion that negative emissions are necessary to limit global warming to 1.5 or 2 degrees. At the same time, according to a review published in 2016, it is considered very risky to strive for the use of negative emission technologies from the outset, as there are currently no such technologies with which the two-degree target without significant negative effects on the consumption of space , energy , water or Nutrients or on the albedo can be achieved. Because of these limitations, they are no substitute for the immediate and rapid reduction of today's greenhouse gas emissions through the decarbonization of the economy.

Geoengineering

Geoengineering encompasses previously unused technical interventions in the environment in order to mitigate the warming, including iron fertilization in the sea to stimulate algae growth and in this way bind CO 2 , and the introduction of sulfate aerosol into the stratosphere to reflect the sun's rays. Both measures are now considered unusable.

Increase in resource productivity

Energy can also be saved by increasing resource productivity (see also factor 4 ), extending product lifetimes and reducing obsolescence , for example with consumer goods or packaging.

Climate protection through behavioral changes

Personal contributions
Urban rail car of the local public transport

Individual possibilities for contributions to climate protection exist in behavioral changes and changed consumption with energy savings . Among the many measures for CO 2 reduction include:

A particularly high reduction in greenhouse gases can be achieved by avoiding meat consumption, modern heating and insulation and flying less once a year. The general population is often mistaken about what helps a lot and what does little to combat climate change. For example, 22% of Germans see doing without plastic bags as the change in behavior that can do the most to combat climate change. In fact, the potential contribution is negligible and by not consuming meat you can achieve 260 times more, by halving 130 times more.

Sustainable nutrition
Greenhouse effect of various food groups: Animal foods, especially beef and lamb, as well as vegetables and fruit from heated greenhouses are particularly harmful to the climate

According to estimates by the IPCC (2007), 10 to 12 percent of global greenhouse gas emissions are due to agriculture . However, the consequences of the deforestation of large areas (including rainforest) for agricultural purposes were not taken into account here. A study commissioned by Greenpeace therefore assumes an agricultural share of 17 to 32 percent of man-made greenhouse gases. In the UK, around 19 percent of greenhouse gas emissions are related to food (agriculture, processing, transportation, retail, consumption, waste). According to these estimates, around 50 percent of this is due to meat and dairy products . The Food Climate Research Network therefore recommends, among other things, market-oriented and regulatory measures for more sustainable production and more sustainable consumption of food (e.g. CO 2 emission-dependent prices / taxes).

If global meat consumption were to be reduced to less than a third within 40 years from 2015, according to a model simulation, nitrous oxide and methane emissions from agriculture would fall below the 1995 level.

The consumption of regional foods is often recommended to reduce food-related emissions . In 2019, the Potsdam Institute for Climate Impact Research showed in a study that optimized local production could reduce emissions from food transport worldwide by a factor of ten. According to a US life cycle assessment by Weber and Matthews (2008), the contribution of transport to the emissions of the food supply in the US is only 11 percent. The main part (83 percent) arises during production, which is why the type of food consumed has the greatest influence. The consumption of red meat is viewed particularly critically with regard to the production of greenhouse gases; Instead, poultry, fish, eggs or vegetables should be used.

Economic strategies

In addition to setting the course for an energy turnaround and phasing out coal , the repertoire of climate protection measures also includes B. the withdrawal of investors such as insurance companies , credit institutions and banks from investments in fossil-fueled industrial sectors and companies ("disinvestment"). Instead, investments can be diverted to sustainable economic sectors such as renewable energies . So has z. For example, at the One Planet Summit in Paris in early December 2017 , the World Bank announced that it would no longer finance projects for the development of crude oil and natural gas from 2019 . The insurance company Axa announced there that it would no longer insure new coal-fired power plants in the future and that it would invest twelve billion euros in “green” projects by 2020 . Environmental protection organizations like Urgewald focus their activities here.

Adaptation strategies

In parallel to preventive climate protection in the form of avoidance strategies, adjustments to the effects of man-made climate change that have already occurred or are expected in the future are necessary: ​​The negative consequences associated with global warming should be reduced as far as possible and made as compatible as possible; at the same time, the use of regionally possibly positive consequences is examined. The adaptability varies depending on various parameters, including existing knowledge of local climate changes or e.g. B. the level of development and the economic performance of a country or society. Overall, especially in socio-economic terms, the ability to adapt is strongly influenced by vulnerability . The Intergovernmental Panel on Climate Change (IPCC) counts the least advanced “ developing countries ” among the countries and regions with particularly high vulnerability.

Adaptation to the consequences of global warming has mainly short to medium-term effects. However, since the adaptability of societies is limited and strong global warming can undo any adaptation measures that have already been taken, adaptation cannot be an alternative to preventive climate protection, but only an addition to it.

The range of potential adaptation measures extends from purely technological measures (e.g. coastal protection ) to changes in behavior (e.g. eating habits, choice of holiday destinations) and business decisions (e.g. changed land management) to political decisions (e.g. planning regulations , Emission reduction targets). Given that climate change affects many sectors of an economy , integrating adaptation e.g. B. in national development plans, poverty reduction strategies or sectoral planning processes a central challenge; many states have therefore developed adaptation strategies.

In the Framework Convention on Climate Change ( UNFCCC ) passed in 1992 , which has meanwhile been ratified by 192 countries, the subject of adaptation hardly played a role in the prevention of dangerous climate change (Article 2 of the UNFCCC). The same applies to the Kyoto Protocol , which was agreed in 1997 and came into force in 2005, but the decision was made to set up a special UN Adaptation Fund in order to provide financing for the developing countries particularly affected to support adaptation measures. The United Nations Green Climate Fund , which was set up during the 2010 climate conference in Cancún, is also intended to contribute to this . Industrialized nations provide money for the fund so that developing countries can better adapt to climate change.

At the latest with the 3rd assessment report of the IPCC, which was published in 2001, the understanding of the need for adaptation strategies has increased. In terms of scientific support for governments, the 2006 Nairobi work program on adaptation and vulnerability was an important step.

Global warming in education, film, literature and the arts

Global warming is increasingly an issue in art , literature, and film ; The topic is presented, for example, in the disaster films Waterworld or The Day After Tomorrow .

There are also a number of documentaries : An inconvenient truth is one of the core messages of Nobel Prize winner Al Gore on anthropogenic climate change. The Swedish documentary Our Planet also deals with climate change and includes interviews with various climate researchers. The US documentary Chasing Ice has the glacier shrinkage as a result of global warming on the content and portrays the Extreme Ice Survey project of the nature photographer James Balog .

In literary terms the topic is u. a. processed in the novels by the British writer Ian McEwan ( Solar ) or the team of authors Ann-Monika Pleitgen and Ilja Bohnet (No Getting Through) published in 2010 . In analogy to “ science fiction ”, the development of a new literary genre is now being spoken of, climate fiction (CliFi) .

In 2013, under the aegis of the German Advisory Council on Global Change, the comic The Great Transformation was published. Climate - can we get the curve? (→ World in Transition - Social Contract for a Great Transformation ) .

Cape Farewell is an international charitable project by British artist David Buckland. The aim is the collaboration of artists, scientists and "communicators" (including media representatives) on the subject of climate change. As part of the project, various expeditions to the Arctic and the Andes were carried out. a. were processed cinematically, photographically, literarily and musically (e.g. in the films Art from the Arctic and Burning Ice ).

Italy's Minister of Education, Lorenzo Fioramonti , announced in November 2019 that the topic of global warming would be integrated into various subjects in public schools in Italy as a compulsory subject from September 2020. While the 6- to 11-year-olds are to be made familiar with the subject of the environment through stories from other cultures , this will be done in the intermediate level through technical information. In the upper level, the students should be introduced to the UN program " Transformation of our world: the 2030 Agenda for Sustainable Development ". The aim is one school lesson (45 minutes each) per week.

literature

See also

Portal: Climate Change  - Overview of Wikipedia content on the topic of global warming

Web links

Commons : Global warming  - collection of images, videos and audio files
Wiktionary: Global warming  - explanations of meanings, word origins, synonyms, translations

Remarks

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This article was added to the list of excellent articles on November 27, 2006 in this version .