Hydraulic transmissivity inferred from ice-sheet relaxation following Greenland supraglacial lake drainages
Hydraulic transmissivity inferred from ice-sheet relaxation following Greenland supraglacial lake drainages
复制标题
根据格陵兰冰上湖排水后冰盖松弛推断的水力透射率
DOI:
10.1038/s41467-021-24186
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发表时间:
2021
影响因子:
16.6
通讯作者:
& Stone, Howard A.
中科院分区:
文献类型:
--
作者:
Lai, Ching-Yao;Stevens, Laura A;Chase, Danielle L.;Creyts, Timothy T;Behn, Mark D;Das, Sarah B;& Stone, Howard A.
Surface meltwater reaching the base of the Greenland Ice Sheet transits through drainage networks, modulating the flow of the ice sheet. Dye and gas-tracing studies conducted in the western margin sector of the ice sheet have directly observed drainage efficiency to evolve seasonally along the drainage pathway. However, the local evolution of drainage systems further inland, where ice thicknesses exceed 1000 m, remains largely unknown. Here, we infer drainage system transmissivity based on surface uplift relaxation following rapid lake drainage events. Combining field observations of five lake drainage events with a mathematical model and laboratory experiments, we show that the surface uplift decreases exponentially with time, as the water in the blister formed beneath the drained lake permeates through the subglacial drainage system. This deflation obeys a universal relaxation law with a timescale that reveals hydraulic transmissivity and indicates a two-order-of-magnitude increase in subglacial transmissivity (from 0.8 ± 0.3to 215 ± 90.2) as the melt season progresses, suggesting significant changes in basal hydrology beneath the lakes driven by seasonal meltwater input.
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影响因子:
64.8
作者:
L. Stevens;M. Behn;J. McGuire;Sarah B. Das;I. Joughin;T. Herring;D. Shean;Matt A. King
通讯作者:
Matt A. King
影响因子:
64.8
作者:
Stevens, Laura A.;Behn, Mark D.;King, Matt A.
通讯作者:
King, Matt A.
影响因子:
3.4
作者:
J. Weertman
通讯作者:
J. Weertman
影响因子:
18.3
作者:
Chandler, D. M.;Wadham, J. L.;Hubbard, A.
通讯作者:
Hubbard, A.
影响因子:
18.3
作者:
Bartholomew, Ian;Nienow, Peter;Sole, Andrew
通讯作者:
Sole, Andrew