Ryder Glacier (Greenland)

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Ryder glacier
The Ryder Glacier with its meltwater lakes (right) on a satellite photo

The Ryder Glacier with its meltwater lakes (right) on a satellite photo

location Knud-Rasmussen-Land , Greenland
Type Outlet glacier
length 80 km (1990)
Altitude range 1000  m  -  m
width Max. 20 km
Coordinates 81 ° 38 ′  N , 49 ° 10 ′  W Coordinates: 81 ° 38 ′  N , 49 ° 10 ′  W
Ryder Glacier (Greenland) (Greenland)
Ryder Glacier (Greenland)
drainage Sherard Osborn FjordLincolnsee
Operational Navigation Chart A-5, 3rd edition.jpg
Template: Infobox Glacier / Maintenance / Image description missing

The Ryder Glacier is an outlet glacier in Knud-Rasmussen-Land in northern Greenland . It is named after the Danish naval officer Carl Ryder , who explored the fjord system of the Scoresbysund in 1891/92 .

The Ryder Glacier starts at the edge of the Greenland Ice Sheet at an altitude of 1000  m and has its 9 km wide glacier front more than 80 km north in the Sherard Osborn Fjord , on the west side of the Wulff Land . A second, 4 km wide western stream ends in the fjord between Permin Land and Warming Land . The last 30 km of the main stream swim as a tongue of ice on the water of the Sherard Osborn Fjord. A prominent ice ridge at the beginning of the fjord probably stems from a subglacial ridge in the bedrock. Above the ridge, the glacier forms a plateau with a very slight gradient that has numerous meltwater lakes.

The Ryder Glacier has a catchment area of ​​28,300 km, which is 1.7% of the area of ​​the Greenland Ice Sheet. Its average flow rate is around 500 meters per year. In the past, the glacier has calved numerous icebergs , many of which are over 5 km long and whose drift can be followed over decades.

Between 1917, when the Danish polar explorer Lauge Koch measured the glacier for the first time during the Second Thule Expedition , and in 1956 the glacier lost 75% of its ice tongue. It has been expanding again since 1990. This process was accelerated by a “mini surge” in the fall of 1995 when the Ryder Glacier more than tripled its speed for seven weeks. In the period from 2000 to 2010, the area of ​​the glacier increased by 4.6 km².

literature

Web links

Individual evidence

  1. a b c Ian Joughin, Slawek Tulaczyk, Mark Fahnestock, Ron Kwok: A Mini-Surge on the Ryder Glacier, Greenland, Observed by Satellite Radar Interferometry . In: Science . Volume 274, October 11, 1996, pp. 228-230.
  2. a b Mauri Pelto: Ryder Glacier, Northern Greenland Transient snowline rise , accessed on February 20, 2017 (English).
  3. E. Rignot, S. Gogineni, I. Joughin, WB Krabill: Contribution to the glaciology of northern Greenland from satellite radar interferometry (PDF; 6.41 MB). In: Journal of Geophysical Research . 106 (D24), 2001, pp. 34007-34019 (English). doi : 10.1029 / 2001JD900071 .