Greenland ice mass balance from GPS, GRACE and ICESat

Shfaqat Abbas Khan; Kurt H. Kjær; Niels Jákup Korsgaard; John Wahr; Jonathan L Bamber; Ruud Hurkmans; Michiel van den Broeke; Lars Hjortborg Timm; Kristian Kjellerup Kjeldsen; Anders Anker Bjørk; Nicolaj Krog Larsen; Lars Tyge Jørgensen; Anders Færch-Jensen; Eske Willerslev; Michael Bevis

Abstract

Global warming is predicted to have a profound impact on the Greenland Ice Sheet (GrIS) and its contribution to future sea-level rise. The GrIS has seen dramatic changes over the last two decades and mass loss has been accelerating, owing to a combination of increased runoff and discharge of ice across the grounding line. The acceleration of glaciers has been reported as pervasive and spreading with time. Prominent is the significant mass change of the southeast and northwest margins associated with glacier speed-up and dynamic thinning. It is unknown, however, whether the extensively documented glacier speed-ups are a response to recent external forcing and the start of a long-term trend in increasing mass loss, or related to internal variability in the ice sheet-climate system that occurs over a range of timescales. Here, we report multi-decadal observations of ice mass change from northwestern Greenland, using stereoscopic coverage by aerial photographs recorded in 1985, and subsequent comparative surface elevation data from ICESat (Ice, Cloud and land Elevation Satellite) and ATM (Airborne Topographic Mapper) supplemented with measurements from GPS and the Gravity Recovery and Climate Experiment (GRACE) satellite gravity mission, launched in March, 2002. The GRACE results provide a direct measure of mass loss, while the GPS data are used to monitor crustal uplift caused by ice mass loss close to the GPS sites.

Original language	English
Publication date	28 Feb 2012
Number of pages	1
Publication status	Published - 28 Feb 2012
Event	2012 UNAVCO Science Workshop - Boulder, CO, United States Duration: 28 Feb 2012 → 1 Mar 2012

Conference

Conference	2012 UNAVCO Science Workshop
Country/Territory	United States
City	Boulder, CO
Period	28/02/2012 → 01/03/2012

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This output contributes to the following UN Sustainable Development Goals (SDGs)

Access to Document

https://register.unavco.org/public/profile/viewab.aspx?xt=523

Cite this

Khan, S. A., Kjær, K. H., Korsgaard, N. J., Wahr, J., Bamber, J. L., Hurkmans, R., Broeke, M. V. D., Timm, L. H., Kjeldsen, K. K., Bjørk, A. A., Larsen, N. K., Jørgensen, L. T., Færch-Jensen, A., Willerslev, E., & Bevis, M. (2012). Greenland ice mass balance from GPS, GRACE and ICESat. Abstract from 2012 UNAVCO Science Workshop, Boulder, CO, United States. https://register.unavco.org/public/profile/viewab.aspx?xt=523

Khan, SA, Kjær, KH, Korsgaard, NJ, Wahr, J, Bamber, JL, Hurkmans, R, Broeke, MVD, Timm, LH, Kjeldsen, KK, Bjørk, AA, Larsen, NK, Jørgensen, LT, Færch-Jensen, A, Willerslev, E & Bevis, M 2012, 'Greenland ice mass balance from GPS, GRACE and ICESat', 2012 UNAVCO Science Workshop, Boulder, CO, United States, 28/02/2012 - 01/03/2012. <https://register.unavco.org/public/profile/viewab.aspx?xt=523>

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title = "Greenland ice mass balance from GPS, GRACE and ICESat",

abstract = "Global warming is predicted to have a profound impact on the Greenland Ice Sheet (GrIS) and its contribution to future sea-level rise. The GrIS has seen dramatic changes over the last two decades and mass loss has been accelerating, owing to a combination of increased runoff and discharge of ice across the grounding line. The acceleration of glaciers has been reported as pervasive and spreading with time. Prominent is the significant mass change of the southeast and northwest margins associated with glacier speed-up and dynamic thinning. It is unknown, however, whether the extensively documented glacier speed-ups are a response to recent external forcing and the start of a long-term trend in increasing mass loss, or related to internal variability in the ice sheet-climate system that occurs over a range of timescales. Here, we report multi-decadal observations of ice mass change from northwestern Greenland, using stereoscopic coverage by aerial photographs recorded in 1985, and subsequent comparative surface elevation data from ICESat (Ice, Cloud and land Elevation Satellite) and ATM (Airborne Topographic Mapper) supplemented with measurements from GPS and the Gravity Recovery and Climate Experiment (GRACE) satellite gravity mission, launched in March, 2002. The GRACE results provide a direct measure of mass loss, while the GPS data are used to monitor crustal uplift caused by ice mass loss close to the GPS sites. ",

author = "Khan, {Shfaqat Abbas} and Kj{\ae}r, {Kurt H.} and Korsgaard, {Niels J{\'a}kup} and John Wahr and Bamber, {Jonathan L} and Ruud Hurkmans and Broeke, {Michiel van den} and Timm, {Lars Hjortborg} and Kjeldsen, {Kristian Kjellerup} and Bj{\o}rk, {Anders Anker} and Larsen, {Nicolaj Krog} and J{\o}rgensen, {Lars Tyge} and Anders F{\ae}rch-Jensen and Eske Willerslev and Michael Bevis",

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T1 - Greenland ice mass balance from GPS, GRACE and ICESat

AU - Khan, Shfaqat Abbas

AU - Kjær, Kurt H.

AU - Korsgaard, Niels Jákup

AU - Wahr, John

AU - Bamber, Jonathan L

AU - Hurkmans, Ruud

AU - Broeke, Michiel van den

AU - Timm, Lars Hjortborg

AU - Kjeldsen, Kristian Kjellerup

AU - Bjørk, Anders Anker

AU - Larsen, Nicolaj Krog

AU - Jørgensen, Lars Tyge

AU - Færch-Jensen, Anders

AU - Willerslev, Eske

AU - Bevis, Michael

PY - 2012/2/28

Y1 - 2012/2/28

N2 - Global warming is predicted to have a profound impact on the Greenland Ice Sheet (GrIS) and its contribution to future sea-level rise. The GrIS has seen dramatic changes over the last two decades and mass loss has been accelerating, owing to a combination of increased runoff and discharge of ice across the grounding line. The acceleration of glaciers has been reported as pervasive and spreading with time. Prominent is the significant mass change of the southeast and northwest margins associated with glacier speed-up and dynamic thinning. It is unknown, however, whether the extensively documented glacier speed-ups are a response to recent external forcing and the start of a long-term trend in increasing mass loss, or related to internal variability in the ice sheet-climate system that occurs over a range of timescales. Here, we report multi-decadal observations of ice mass change from northwestern Greenland, using stereoscopic coverage by aerial photographs recorded in 1985, and subsequent comparative surface elevation data from ICESat (Ice, Cloud and land Elevation Satellite) and ATM (Airborne Topographic Mapper) supplemented with measurements from GPS and the Gravity Recovery and Climate Experiment (GRACE) satellite gravity mission, launched in March, 2002. The GRACE results provide a direct measure of mass loss, while the GPS data are used to monitor crustal uplift caused by ice mass loss close to the GPS sites.

AB - Global warming is predicted to have a profound impact on the Greenland Ice Sheet (GrIS) and its contribution to future sea-level rise. The GrIS has seen dramatic changes over the last two decades and mass loss has been accelerating, owing to a combination of increased runoff and discharge of ice across the grounding line. The acceleration of glaciers has been reported as pervasive and spreading with time. Prominent is the significant mass change of the southeast and northwest margins associated with glacier speed-up and dynamic thinning. It is unknown, however, whether the extensively documented glacier speed-ups are a response to recent external forcing and the start of a long-term trend in increasing mass loss, or related to internal variability in the ice sheet-climate system that occurs over a range of timescales. Here, we report multi-decadal observations of ice mass change from northwestern Greenland, using stereoscopic coverage by aerial photographs recorded in 1985, and subsequent comparative surface elevation data from ICESat (Ice, Cloud and land Elevation Satellite) and ATM (Airborne Topographic Mapper) supplemented with measurements from GPS and the Gravity Recovery and Climate Experiment (GRACE) satellite gravity mission, launched in March, 2002. The GRACE results provide a direct measure of mass loss, while the GPS data are used to monitor crustal uplift caused by ice mass loss close to the GPS sites.

M3 - Conference abstract for conference

T2 - 2012 UNAVCO Science Workshop

Y2 - 28 February 2012 through 1 March 2012

ER -