Elastic uplift in southeast Greenland due to rapid ice mass loss

Shfaqat Abbas Khan; Tonie Van dam; Gordon S. Hamilton; Leigh A. Stearns; John Wahr; Kristine M. Larson; Olivier Francis

doi:10.1029/2007/GL031468

Elastic uplift in southeast Greenland due to rapid ice mass loss

Shfaqat Abbas Khan, Tonie Van dam, Gordon S. Hamilton, Leigh A. Stearns, John Wahr, Kristine M. Larson, Olivier Francis

National Space Institute

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Abstract

The rapid unloading of ice from the southeastern sector of the Greenland ice sheet between 2001 and 2006 caused an elastic uplift of 35 mm at a GPS site in Kulusuk. Most of the uplift results from ice dynamic-induced volume losses on two nearby outlet glaciers. Volume loss from Helheim Glacier, calculated from sequential digital elevation models, contributes about 16 mm of the observed uplift, with an additional 5 mm from volume loss of Kangerdlugssuaq Glacier. The remaining uplift signal is attributed to significant melt-induced ice volume loss from the ice sheet margin along the southeast coast between 62N and 66N. Citation: Khan, S. A., J. Wahr, L. A. Stearns, G. S. Hamilton, T. van Dam, K. M. Larson, and O. Francis (2007), Elastic uplift in southeast Greenland due to rapid ice mass loss.

Original language	English
Journal	Geophysical Research Letters
Volume	34
ISSN	0094-8276
DOIs	https://doi.org/10.1029/2007/GL031468
Publication status	Published - 2007

Keywords

Global warming
GPS
Ice mass loss

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10.1029/2007/GL031468

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@article{b89f84f1e1844d5caeff4a1d7652d7a4,

title = "Elastic uplift in southeast Greenland due to rapid ice mass loss",

abstract = "The rapid unloading of ice from the southeastern sector of the Greenland ice sheet between 2001 and 2006 caused an elastic uplift of 35 mm at a GPS site in Kulusuk. Most of the uplift results from ice dynamic-induced volume losses on two nearby outlet glaciers. Volume loss from Helheim Glacier, calculated from sequential digital elevation models, contributes about 16 mm of the observed uplift, with an additional 5 mm from volume loss of Kangerdlugssuaq Glacier. The remaining uplift signal is attributed to significant melt-induced ice volume loss from the ice sheet margin along the southeast coast between 62N and 66N. Citation: Khan, S. A., J. Wahr, L. A. Stearns, G. S. Hamilton, T. van Dam, K. M. Larson, and O. Francis (2007), Elastic uplift in southeast Greenland due to rapid ice mass loss.",

keywords = "Global warming, GPS, Ice mass loss",

author = "Khan, {Shfaqat Abbas} and {Van dam}, Tonie and Hamilton, {Gordon S.} and Stearns, {Leigh A.} and John Wahr and Larson, {Kristine M.} and Olivier Francis",

year = "2007",

doi = "10.1029/2007/GL031468",

language = "English",

volume = "34",

journal = "Geophysical Research Letters",

issn = "0094-8276",

publisher = "Wiley-Blackwell",

}

TY - JOUR

T1 - Elastic uplift in southeast Greenland due to rapid ice mass loss

AU - Khan, Shfaqat Abbas

AU - Van dam, Tonie

AU - Hamilton, Gordon S.

AU - Stearns, Leigh A.

AU - Wahr, John

AU - Larson, Kristine M.

AU - Francis, Olivier

PY - 2007

Y1 - 2007

N2 - The rapid unloading of ice from the southeastern sector of the Greenland ice sheet between 2001 and 2006 caused an elastic uplift of 35 mm at a GPS site in Kulusuk. Most of the uplift results from ice dynamic-induced volume losses on two nearby outlet glaciers. Volume loss from Helheim Glacier, calculated from sequential digital elevation models, contributes about 16 mm of the observed uplift, with an additional 5 mm from volume loss of Kangerdlugssuaq Glacier. The remaining uplift signal is attributed to significant melt-induced ice volume loss from the ice sheet margin along the southeast coast between 62N and 66N. Citation: Khan, S. A., J. Wahr, L. A. Stearns, G. S. Hamilton, T. van Dam, K. M. Larson, and O. Francis (2007), Elastic uplift in southeast Greenland due to rapid ice mass loss.

AB - The rapid unloading of ice from the southeastern sector of the Greenland ice sheet between 2001 and 2006 caused an elastic uplift of 35 mm at a GPS site in Kulusuk. Most of the uplift results from ice dynamic-induced volume losses on two nearby outlet glaciers. Volume loss from Helheim Glacier, calculated from sequential digital elevation models, contributes about 16 mm of the observed uplift, with an additional 5 mm from volume loss of Kangerdlugssuaq Glacier. The remaining uplift signal is attributed to significant melt-induced ice volume loss from the ice sheet margin along the southeast coast between 62N and 66N. Citation: Khan, S. A., J. Wahr, L. A. Stearns, G. S. Hamilton, T. van Dam, K. M. Larson, and O. Francis (2007), Elastic uplift in southeast Greenland due to rapid ice mass loss.

KW - Global warming

KW - GPS

KW - Ice mass loss

U2 - 10.1029/2007/GL031468

DO - 10.1029/2007/GL031468

M3 - Journal article

VL - 34

JO - Geophysical Research Letters

JF - Geophysical Research Letters

SN - 0094-8276

ER -