Submarine Meltwater From Nioghalvfjerdsbræ (79 North Glacier), Northeast Greenland
Submarine Meltwater From Nioghalvfjerdsbræ (79 North Glacier), Northeast Greenland
复制标题
来自格陵兰岛东北部 Nioghalvfjerdsbræ(北冰川 79 号)的潜艇融水
DOI:
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发表时间:
2021
期刊:
影响因子:
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通讯作者:
J. Sültenfuss
中科院分区:
文献类型:
--
作者:
O. Huhn;M. Rhein;T. Kanzow;J. Schaffer;J. Sültenfuss
revealed the Abstract The Greenland Ice Sheet (GrIS) faces accelerated melting under a warming climate. This also affects the largest marine-terminating outlet glacier of the Northeast Greenland Ice Stream (NEGIS), the Nioghalvfjerdsbræ (79 North Glacier, 79NG). In the cavity below its floating ice tongue, the heat of inflowing warm and saline Atlantic Water melts the ice at the base, and colder and fresher outflow is exported toward the shelf break and presumably south with the East Greenland Current (EGC). However, freshwater from submarine melting is hardly distinguishable from other freshwater sources by salinity alone. To identify and to quantify the distribution of submarine meltwater on the Northeast Greenland Shelf, we use helium (He) and neon (Ne) observations obtained directly at the calving front of the 79NG, on the Northeast Greenland Shelf, and in Fram Strait during an expedition aboard R/V POLARSTERN in summer 2016. These tracers uniquely identify submarine meltwater (SMW) and allow quantifying its fraction. SMW is present on the shelf but dilutes from 1.8% at the 79NG calving front to nonsignificant in Fram Strait. The SMW
影响因子:
18.3
作者:
Boening, Claus W.;Behrens, Erik;Bamber, Jonathan L.
通讯作者:
Bamber, Jonathan L.
影响因子:
16.6
作者:
Mayer C;Schaffer J;Hattermann T;Floricioiu D;Krieger L;Dodd PA;Kanzow T;Licciulli C;Schannwell C
通讯作者:
Schannwell C
影响因子:
5.2
作者:
Huhn, Oliver;Hattermann, Tore;Sueltenfuss, Juergen
通讯作者:
Sueltenfuss, Juergen