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DOI10.5194/tc-15-2251-2021
Comment on "exceptionally high heat flux needed to sustain the Northeast Greenland Ice Stream" by Smith-Johnsen et al. (2020)
Bons P.D.; De Riese T.; Franke S.; Llorens M.-G.; Sachau T.; Stoll N.; Weikusat I.; Westhoff J.; Zhang Y.
发表日期2021
ISSN19940416
起始页码2251
结束页码2254
卷号15期号:5
英文摘要Smith-Johnsen et al. (The Cryosphere, 14, 841-854, 2020) model the effect of a potential hotspot on the Northeast Greenland Ice Stream (NEGIS). They argue that a heat flux of at least 970 mW m-2 is required to have initiated or to control NEGIS. Such an exceptionally high heat flux would be unique in the world and is incompatible with known geological processes that can raise the heat flux. Fast flow at NEGIS must thus be possible without the extraordinary melt rates invoked in Smith-Johnsen et al. (2020). © 2021 Paul D. Bons et al.
英文关键词cryosphere; geothermal system; GRIP; heat flux; ice sheet; numerical model; Arctic; Greenland; Greenland Ice Sheet
语种英语
来源期刊Cryosphere
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/202284
作者单位School of Earth Science and Resources, China University of Geosciences, Beijing, China; Department of Geosciences, Eberhard Karls University Tübingen, Tübingen, Germany; Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany; Geosciences Barcelona, Csic, Barcelona, Spain; Physics of Ice Climate and Earth, University of Copenhagen, Copenhagen, Denmark
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Bons P.D.,De Riese T.,Franke S.,et al. Comment on "exceptionally high heat flux needed to sustain the Northeast Greenland Ice Stream" by Smith-Johnsen et al. (2020)[J],2021,15(5).
APA Bons P.D..,De Riese T..,Franke S..,Llorens M.-G..,Sachau T..,...&Zhang Y..(2021).Comment on "exceptionally high heat flux needed to sustain the Northeast Greenland Ice Stream" by Smith-Johnsen et al. (2020).Cryosphere,15(5).
MLA Bons P.D.,et al."Comment on "exceptionally high heat flux needed to sustain the Northeast Greenland Ice Stream" by Smith-Johnsen et al. (2020)".Cryosphere 15.5(2021).
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