Crustal uplift due to ice mass variability on Upernavik Isstrøm, west Greenland

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

Standard

Crustal uplift due to ice mass variability on Upernavik Isstrøm, west Greenland. / Nielsen, Karina; Khan, Shfaqat Abbas; Korsgaard, Niels J.; Kjær, Kurt H.; Wahr, John; Bevis, Michael; Stearns, Leigh A.; Timm, Lars H.

In: Earth and Planetary Science Letters, Vol. 353-354, 2012, p. 182-189.

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

Harvard

Nielsen, K, Khan, SA, Korsgaard, NJ, Kjær, KH, Wahr, J, Bevis, M, Stearns, LA & Timm, LH 2012, 'Crustal uplift due to ice mass variability on Upernavik Isstrøm, west Greenland' Earth and Planetary Science Letters, vol 353-354, pp. 182-189., 10.1016/j.epsl.2012.08.024

APA

Nielsen, K., Khan, S. A., Korsgaard, N. J., Kjær, K. H., Wahr, J., Bevis, M., Stearns, L. A., & Timm, L. H. (2012). Crustal uplift due to ice mass variability on Upernavik Isstrøm, west Greenland. Earth and Planetary Science Letters, 353-354, 182-189. 10.1016/j.epsl.2012.08.024

CBE

Nielsen K, Khan SA, Korsgaard NJ, Kjær KH, Wahr J, Bevis M, Stearns LA, Timm LH. 2012. Crustal uplift due to ice mass variability on Upernavik Isstrøm, west Greenland. Earth and Planetary Science Letters. 353-354:182-189. Available from: 10.1016/j.epsl.2012.08.024

MLA

Vancouver

Author

Nielsen, Karina; Khan, Shfaqat Abbas; Korsgaard, Niels J.; Kjær, Kurt H.; Wahr, John; Bevis, Michael; Stearns, Leigh A.; Timm, Lars H. / Crustal uplift due to ice mass variability on Upernavik Isstrøm, west Greenland.

In: Earth and Planetary Science Letters, Vol. 353-354, 2012, p. 182-189.

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

Bibtex

@article{2d00f09664bd448f9cef64912cad21fa,
title = "Crustal uplift due to ice mass variability on Upernavik Isstrøm, west Greenland",
publisher = "Elsevier BV",
author = "Karina Nielsen and Khan, {Shfaqat Abbas} and Korsgaard, {Niels J.} and Kjær, {Kurt H.} and John Wahr and Michael Bevis and Stearns, {Leigh A.} and Timm, {Lars H.}",
year = "2012",
doi = "10.1016/j.epsl.2012.08.024",
volume = "353-354",
pages = "182--189",
journal = "Earth and Planetary Science Letters",
issn = "0012-821X",

}

RIS

TY - JOUR

T1 - Crustal uplift due to ice mass variability on Upernavik Isstrøm, west Greenland

A1 - Nielsen,Karina

A1 - Khan,Shfaqat Abbas

A1 - Korsgaard,Niels J.

A1 - Kjær,Kurt H.

A1 - Wahr,John

A1 - Bevis,Michael

A1 - Stearns,Leigh A.

A1 - Timm,Lars H.

AU - Nielsen,Karina

AU - Khan,Shfaqat Abbas

AU - Korsgaard,Niels J.

AU - Kjær,Kurt H.

AU - Wahr,John

AU - Bevis,Michael

AU - Stearns,Leigh A.

AU - Timm,Lars H.

PB - Elsevier BV

PY - 2012

Y1 - 2012

N2 - We estimate the mass loss rate of Upernavik Isstrøm (UI) using surface elevation changes between a SPOT 5 Digital Elevation Model (DEM) from 2008 and NASA's Airborne Topographic Mapper (ATM) data from 2010. To assess the validity of our mass loss estimate, we analyze GPS data between 2007 and 2011 from two continuous receivers, UPVK and SRMP which are established on bedrock and located ∼65 and View the MathML source from the front of UI, respectively. We construct along-track elevation changes on UI for several time intervals during 2005–2011, based on ATM, SPOT 5 and Ice, Cloud, and land Elevation Satellite (ICESat) data to assess temporal changes of UI. We estimate a mass loss rate of −6.7±4.2 Gt/yr, over an area of View the MathML source. The ice mass loss occurs primarily over the northern glacier of UI. This pattern is also observed View the MathML source upstream, where we observe glacier thinning at a rate of −1.6±0.3 m/yr across the northern portion of UI and −0.5±0.1 m/yr across the southern portion. GPS measurements suggest bedrock uplift rates of 7.6±0.6 mm/yr (UPVK) and 16.2±0.6 mm/yr (SRMP). The modeled ice mass loss of UI causes bedrock uplift rates of 1.3±0.6 mm/yr (UPVK) and 8.3±4.2 mm/yr (SRMP). Including additional contributions from ice mass changes outside UI and from Glacial Isostatic Adjustment (GIA), we obtain total modeled uplift rates of 4.7±0.6 mm/yr (UPVK) and 13.8±4.2 mm/yr (SRMP). The modeled uplift rates from our UI ice mass loss are substantially lower, indicating that additional mass loss is taking place outside of UI. We obtain a difference of 0.6 mm/yr between the modeled and observed relative uplift rates (SRMP relative to UPVK), suggesting that the mass loss of UI is well captured in the model. We observe elevation changes from −15 to −40 m/yr near the front during the period 2005–2011, indicating that UI undergoes large variations in thinning pattern over short time spans.

AB - We estimate the mass loss rate of Upernavik Isstrøm (UI) using surface elevation changes between a SPOT 5 Digital Elevation Model (DEM) from 2008 and NASA's Airborne Topographic Mapper (ATM) data from 2010. To assess the validity of our mass loss estimate, we analyze GPS data between 2007 and 2011 from two continuous receivers, UPVK and SRMP which are established on bedrock and located ∼65 and View the MathML source from the front of UI, respectively. We construct along-track elevation changes on UI for several time intervals during 2005–2011, based on ATM, SPOT 5 and Ice, Cloud, and land Elevation Satellite (ICESat) data to assess temporal changes of UI. We estimate a mass loss rate of −6.7±4.2 Gt/yr, over an area of View the MathML source. The ice mass loss occurs primarily over the northern glacier of UI. This pattern is also observed View the MathML source upstream, where we observe glacier thinning at a rate of −1.6±0.3 m/yr across the northern portion of UI and −0.5±0.1 m/yr across the southern portion. GPS measurements suggest bedrock uplift rates of 7.6±0.6 mm/yr (UPVK) and 16.2±0.6 mm/yr (SRMP). The modeled ice mass loss of UI causes bedrock uplift rates of 1.3±0.6 mm/yr (UPVK) and 8.3±4.2 mm/yr (SRMP). Including additional contributions from ice mass changes outside UI and from Glacial Isostatic Adjustment (GIA), we obtain total modeled uplift rates of 4.7±0.6 mm/yr (UPVK) and 13.8±4.2 mm/yr (SRMP). The modeled uplift rates from our UI ice mass loss are substantially lower, indicating that additional mass loss is taking place outside of UI. We obtain a difference of 0.6 mm/yr between the modeled and observed relative uplift rates (SRMP relative to UPVK), suggesting that the mass loss of UI is well captured in the model. We observe elevation changes from −15 to −40 m/yr near the front during the period 2005–2011, indicating that UI undergoes large variations in thinning pattern over short time spans.

KW - Elastic uplift

KW - GPS

KW - Ice loss

KW - West Greenland

U2 - 10.1016/j.epsl.2012.08.024

DO - 10.1016/j.epsl.2012.08.024

JO - Earth and Planetary Science Letters

JF - Earth and Planetary Science Letters

SN - 0012-821X

VL - 353-354

SP - 182

EP - 189

ER -