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Home* News and Stories → Tem­pe­ra­te water in Spitsbergen’s fjords

Tem­pe­ra­te water in Spitsbergen’s fjords

Tem­pe­ra­te Atlan­tic water has ente­red the fjords on the west coast of Spits­ber­gen, resul­ting in a decre­asing chan­ce for a lar­ge-sca­le solid ice-cover in coas­tal waters com­pared to last win­ter. The rela­tively strong ice-for­ma­ti­on of last year may be among­st the reasons: the cold, sal­ty water that sinks down gives way to inflowing Atlan­tic water­mas­ses.

In the end, the wind con­di­ti­ons are decisi­ve for fjord ice for­ma­ti­on.

Fjord­eis­bil­dung braucht ruhi­ges, kal­tes Wet­ter. Hier Eis in Auf­lö­sung im Juni, Lief­defjord.

Temperate water in Spitsbergen’s fjords - data-lazy-src=

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last modification: 2014-07-01 · copyright: Rolf Stange
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