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Revisiting the Last Ice Area projections from a high-resolution Global Earth System Model
被引:0
|作者:
Fol, Madeleine
[1
]
Tremblay, Bruno
[1
,2
]
Pfirman, Stephanie
[3
]
Newton, Robert
[2
]
Howell, Stephen
[4
]
Lemieux, Jean-Francois
[5
]
机构:
[1] McGill Univ, Dept Atmospher & Ocean Sci, Montreal, PQ, Canada
[2] Columbia Univ, Lamont Doherty Earth Observ, Palisades, NY USA
[3] Arizona State Univ, Coll Global Futures, Tempe, AZ USA
[4] Climate Res Div Environm & Climate Change Canada, Toronto, ON, Canada
[5] Environm & Changement Climat Canada, Rech Previs Numer Environm, Dorval, PQ, Canada
来源:
COMMUNICATIONS EARTH & ENVIRONMENT
|
2025年
/
6卷
/
01期
基金:
加拿大自然科学与工程研究理事会;
美国国家科学基金会;
关键词:
ARCTIC SEA-ICE;
THICKNESS DISTRIBUTION;
ARCHIPELAGO;
VARIABILITY;
DYNAMICS;
D O I:
10.1038/s43247-025-02034-5
中图分类号:
X [环境科学、安全科学];
学科分类号:
08 ;
0830 ;
摘要:
The Last Ice Area-located to the north of Greenland and the northern Canadian Arctic Archipelago-is expected to persist as the central Arctic Ocean becomes seasonally ice-free within a few decades. Projections of the Last Ice Area, however, have come from relatively low resolution Global Climate Models that do not resolve sea ice export through the waterways of the Canadian Arctic Archipelago and Nares Strait. Here we revisit Last Ice Area projections using high-resolution numerical simulations from the Community Earth System Model, which resolves these narrow waterways. Under a high-end forcing scenario, the sea ice of the Last Ice Area thins and becomes more mobile, resulting in a large export southward. Under this potentially worst-case scenario, sea ice of the Last Ice Area could disappear a little more than one decade after the central Arctic Ocean has reached seasonally ice-free conditions. This loss would have profound impacts on ice-obligate species.
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页数:12
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