Constraining ice mass loss from Jakobshavn Isbræ (Greenland) using InSAR-measured crustal uplift

Publication: Research - peer-reviewJournal article – Annual report year: 2012

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Constraining ice mass loss from Jakobshavn Isbræ (Greenland) using InSAR-measured crustal uplift. / Liu, Lin; Wahr, John; Howat, Ian; Khan, Shfaqat Abbas; Joughin, Ian; Furuya, Masato.

In: Geophysical Journal International, Vol. 188, No. 3, 2012, p. 994-1006.

Publication: Research - peer-reviewJournal article – Annual report year: 2012

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Liu, Lin; Wahr, John; Howat, Ian; Khan, Shfaqat Abbas; Joughin, Ian; Furuya, Masato / Constraining ice mass loss from Jakobshavn Isbræ (Greenland) using InSAR-measured crustal uplift.

In: Geophysical Journal International, Vol. 188, No. 3, 2012, p. 994-1006.

Publication: Research - peer-reviewJournal article – Annual report year: 2012

Bibtex

@article{8bc022a647024180a4a8452240c91d5e,
title = "Constraining ice mass loss from Jakobshavn Isbræ (Greenland) using InSAR-measured crustal uplift",
keywords = "Arctic region, Space geodetic surveys, Kinematics of crustal and mantle deformation, Radar interferometry, Glaciology",
publisher = "Wiley-Blackwell Publishing Ltd.",
author = "Lin Liu and John Wahr and Ian Howat and Khan, {Shfaqat Abbas} and Ian Joughin and Masato Furuya",
year = "2012",
doi = "10.1111/j.1365-246X.2011.05317.x",
volume = "188",
number = "3",
pages = "994--1006",
journal = "Geophysical Journal International",
issn = "0956-540X",

}

RIS

TY - JOUR

T1 - Constraining ice mass loss from Jakobshavn Isbræ (Greenland) using InSAR-measured crustal uplift

A1 - Liu,Lin

A1 - Wahr,John

A1 - Howat,Ian

A1 - Khan,Shfaqat Abbas

A1 - Joughin,Ian

A1 - Furuya,Masato

AU - Liu,Lin

AU - Wahr,John

AU - Howat,Ian

AU - Khan,Shfaqat Abbas

AU - Joughin,Ian

AU - Furuya,Masato

PB - Wiley-Blackwell Publishing Ltd.

PY - 2012

Y1 - 2012

N2 - Jakobshavn Isbræ in west Greenland has been undergoing dramatic thinning since 1997. Applying the interferometric synthetic aperture radar (InSAR) technique to Radarsat-1 SAR data, we measure crustal uplift near Jakobshavn Isbræ caused by recent ice mass loss. The crustal uplift is predominantly at long spatial wavelengths (larger than 10 km), and thus is difficult to separate from InSAR orbit errors. We reduce the effects of orbit errors by removing long-wavelength deformation signals using conventional InSAR baseline fitting methods. We find good agreement between the remaining short-scale InSAR-estimated deformation rates during 2004–2008 and the corresponding short-scale components of a deformation model that is based on changes in ice elevation measured by NASA’s Airborne Topographic Mapper (ATM). We are also able to use the InSAR-measured deformation to invert for the spatial pattern of ice thinning. Overall, our results suggest that despite the inherent difficulties of working with a signal that has significant large-scale components, InSAR-measured crustal deformation can be used to study the ice mass loss of a rapidly thinning glacier and its surrounding catchment, providing both a constraint on any existing model of ice mass loss and a data source that can be used to invert for ice mass loss. These new applications of InSAR can help to better understand a glacier’s rapid response to a warming climate.

AB - Jakobshavn Isbræ in west Greenland has been undergoing dramatic thinning since 1997. Applying the interferometric synthetic aperture radar (InSAR) technique to Radarsat-1 SAR data, we measure crustal uplift near Jakobshavn Isbræ caused by recent ice mass loss. The crustal uplift is predominantly at long spatial wavelengths (larger than 10 km), and thus is difficult to separate from InSAR orbit errors. We reduce the effects of orbit errors by removing long-wavelength deformation signals using conventional InSAR baseline fitting methods. We find good agreement between the remaining short-scale InSAR-estimated deformation rates during 2004–2008 and the corresponding short-scale components of a deformation model that is based on changes in ice elevation measured by NASA’s Airborne Topographic Mapper (ATM). We are also able to use the InSAR-measured deformation to invert for the spatial pattern of ice thinning. Overall, our results suggest that despite the inherent difficulties of working with a signal that has significant large-scale components, InSAR-measured crustal deformation can be used to study the ice mass loss of a rapidly thinning glacier and its surrounding catchment, providing both a constraint on any existing model of ice mass loss and a data source that can be used to invert for ice mass loss. These new applications of InSAR can help to better understand a glacier’s rapid response to a warming climate.

KW - Arctic region

KW - Space geodetic surveys

KW - Kinematics of crustal and mantle deformation

KW - Radar interferometry

KW - Glaciology

U2 - 10.1111/j.1365-246X.2011.05317.x

DO - 10.1111/j.1365-246X.2011.05317.x

JO - Geophysical Journal International

JF - Geophysical Journal International

SN - 0956-540X

IS - 3

VL - 188

SP - 994

EP - 1006

ER -