Dead water (shipping)

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In shipping, dead water is stratified water that can slow down a ship.

causes

If light fresh water is stratified on heavy salt water near the mouth of a river, an entering ship can create a wave on the boundary surface that runs behind the ship and seems to be sucked into its stern without being able to identify the cause on the surface (so-called . Nansen wave). In 1893, Fridtjof Nansen registered such waves off the estuaries of the Siberian coast, which slowed his ship Fram from 7 to 1.5 knots without the wave becoming visible on the surface. Such water areas are called dead water ( internal waves ). Especially in narrow canals, there can be a rhythmic delay in which the ship alternates faster and slower. In 1904 the Swedish physicist and oceanographer Vagn Walfrid Ekman presented part of the solution to the problem for the first time. The effect is based on two different phenomena: the Nansen wave resistance and the Ekman wave resistance .

Web links

Individual evidence

  1. ^ Vagn Walfrid Ekman: On dead-water. In: Fridtjof Nansen (Ed.): The Norwegian North Polar Expedition 1893-1896: Scientific results. Volume V, No. 15, Dybwad, Christiania 1905, pp. 1–152 ( Textarchiv - Internet Archive ).
  2. Jan Dönges: How water becomes dead water on Spektrum.de, July 7, 2020.
  3. ^ Johan Fourdrinoy et al. a .: The dual nature of the dead-water phenomenology: Nansen versus Ekman wave-making drags. In: Proceedings of the National Academy of Sciences.
  4. How dead water brings ships to a standstill . In the online edition of the Standard on July 12, 2020, accessed on July 16, 2020.