What is the global glacier ice volume outside the ice sheets?

被引:12
作者
Hock, Regine [1 ,2 ]
Maussion, Fabien [3 ]
Marzeion, Ben [4 ,5 ]
Nowicki, Sophie [6 ]
机构
[1] Univ Oslo, Dept Geosci, Oslo, Norway
[2] Univ Alaska, Geophys Inst, Fairbanks, AK 99775 USA
[3] Univ Innsbruck, Dept Atmospher & Cryospher Sci ACINN, Innsbruck, Austria
[4] Univ Bremen, Inst Geog, Bremen, Germany
[5] Univ Bremen, MARUM Ctr Marine Environm Sci, Bremen, Germany
[6] Univ Buffalo, Dept Geol, Buffalo, NY USA
基金
奥地利科学基金会;
关键词
Glacier mapping; glacier mass balance; glacier volume; ice-sheet mass balance; SURFACE MASS-BALANCE; SPATIAL SENSITIVITIES; ENVIRONMENTAL-CHANGE; BRIEF-COMMUNICATION; COMPLETE INVENTORY; MODEL; CAPS; GREENLAND; MOUNTAIN; INSIGHTS;
D O I
10.1017/jog.2023.1
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
A recent study (Millan and others, 2022a, Nature Geoscience 15(2), 124-129) claims that ice volume contained in all glaciers outside the ice sheets and its potential contribution to sea level is 20% less than previously estimated. However, the apparent decrease is largely due to differences in choice of domain, as the study excludes 80% of the glacier area in the Antarctic periphery that was included in previous global glacier volume estimates. The issue highlights the difficulty in separating glaciers from the ice-sheet proper, especially in Antarctica, and the need for both the glacier and ice-sheet communities to develop standards and protocols to avoid double-counting in global ice volume and mass-change assessments and projections. Process-based inversion models have replaced earlier scaling methods, but large uncertainties in global glacier volume estimation remain due to the ill-posed nature of the inversion problem and poorly constrained parameters emphasizing the need for more direct ice thickness observations.
引用
收藏
页码:204 / 210
页数:7
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