Annual Variation of Coastal Uplift in Greenland as an Indicator of Variable and Accelerating Ice Mass Loss

Seasonal melting of the coastal part of the Greenland ice sheet is investigated using GPS vertical displacement data from coastal stations, combined with data on atmospheric and ocean temperatures. Using a high pass filter and cubic spline models, we estimate five variables describing seasonal uplif...

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Published in:Geochemistry, Geophysics, Geosystems
Main Authors: Yang, Qian, Wdowinski, Shimon, Dixon, Timothy H.
Format: Article in Journal/Newspaper
Language:unknown
Published: Digital Commons @ University of South Florida 2013
Subjects:
Online Access:https://digitalcommons.usf.edu/geo_facpub/1542
https://doi.org/10.1002/ggge.20089
https://digitalcommons.usf.edu/context/geo_facpub/article/2461/viewcontent/Yang_et_al_2013_Geochemistry__Geophysics__Geosystems.pdf
https://digitalcommons.usf.edu/context/geo_facpub/article/2461/filename/0/type/additional/viewcontent/Supplementary_Information.pdf
https://digitalcommons.usf.edu/context/geo_facpub/article/2461/filename/1/type/additional/viewcontent/2012gc004432pa01.pdf
https://digitalcommons.usf.edu/context/geo_facpub/article/2461/filename/2/type/additional/viewcontent/2012gc004432pa02.pdf
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https://digitalcommons.usf.edu/context/geo_facpub/article/2461/filename/9/type/additional/viewcontent/2012gc004432pa07.pdf
https://digitalcommons.usf.edu/context/geo_facpub/article/2461/filename/10/type/additional/viewcontent/2012gc004432readme.txt
id ftusouthflorida:oai:digitalcommons.usf.edu:geo_facpub-2461
record_format openpolar
institution Open Polar
collection University of South Florida St. Petersburg: Digital USFSP
op_collection_id ftusouthflorida
language unknown
topic Greenland's ice sheet
GPS vertical displacement
seasonal melting
climatic forcings
Earth Sciences
spellingShingle Greenland's ice sheet
GPS vertical displacement
seasonal melting
climatic forcings
Earth Sciences
Yang, Qian
Wdowinski, Shimon
Dixon, Timothy H.
Annual Variation of Coastal Uplift in Greenland as an Indicator of Variable and Accelerating Ice Mass Loss
topic_facet Greenland's ice sheet
GPS vertical displacement
seasonal melting
climatic forcings
Earth Sciences
description Seasonal melting of the coastal part of the Greenland ice sheet is investigated using GPS vertical displacement data from coastal stations, combined with data on atmospheric and ocean temperatures. Using a high pass filter and cubic spline models, we estimate five variables describing seasonal uplift, a proxy for proximal mass loss, including duration of the melt season and the amount of summer uplift. Our analysis shows both temporal and spatial variations of uplift. Southern coastal Greenland experienced anomalously large uplift in summer 2010, implying significant melting that year. However, the northwest coast did not experience significant change in uplift at that time. Our data suggest that a combination of warm summer air temperature and warm sub‐surface ocean water temperature drove the large mass losses in 2010. Using the uplift pattern of 2008–2010, and comparing to atmospheric data and ocean water temperature data, we show that warm Irminger Water (IW) exerted significant influence on coastal melting in southeastern, southern and southwestern Greenland, reaching about 69°N in 2010. North of this, IW did not exert significant influence, in effect defining the northward limit of the sub‐polar gyre for that year. Thus, short‐term variability in the coastal GPS uplift signal can be used to infer an oceanographic parameter that has a critical influence on Greenland ice sheet health.
format Article in Journal/Newspaper
author Yang, Qian
Wdowinski, Shimon
Dixon, Timothy H.
author_facet Yang, Qian
Wdowinski, Shimon
Dixon, Timothy H.
author_sort Yang, Qian
title Annual Variation of Coastal Uplift in Greenland as an Indicator of Variable and Accelerating Ice Mass Loss
title_short Annual Variation of Coastal Uplift in Greenland as an Indicator of Variable and Accelerating Ice Mass Loss
title_full Annual Variation of Coastal Uplift in Greenland as an Indicator of Variable and Accelerating Ice Mass Loss
title_fullStr Annual Variation of Coastal Uplift in Greenland as an Indicator of Variable and Accelerating Ice Mass Loss
title_full_unstemmed Annual Variation of Coastal Uplift in Greenland as an Indicator of Variable and Accelerating Ice Mass Loss
title_sort annual variation of coastal uplift in greenland as an indicator of variable and accelerating ice mass loss
publisher Digital Commons @ University of South Florida
publishDate 2013
url https://digitalcommons.usf.edu/geo_facpub/1542
https://doi.org/10.1002/ggge.20089
https://digitalcommons.usf.edu/context/geo_facpub/article/2461/viewcontent/Yang_et_al_2013_Geochemistry__Geophysics__Geosystems.pdf
https://digitalcommons.usf.edu/context/geo_facpub/article/2461/filename/0/type/additional/viewcontent/Supplementary_Information.pdf
https://digitalcommons.usf.edu/context/geo_facpub/article/2461/filename/1/type/additional/viewcontent/2012gc004432pa01.pdf
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https://digitalcommons.usf.edu/context/geo_facpub/article/2461/filename/10/type/additional/viewcontent/2012gc004432readme.txt
geographic Greenland
geographic_facet Greenland
genre Greenland
Ice Sheet
genre_facet Greenland
Ice Sheet
op_source School of Geosciences Faculty and Staff Publications
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spelling ftusouthflorida:oai:digitalcommons.usf.edu:geo_facpub-2461 2023-07-30T04:03:45+02:00 Annual Variation of Coastal Uplift in Greenland as an Indicator of Variable and Accelerating Ice Mass Loss Yang, Qian Wdowinski, Shimon Dixon, Timothy H. 2013-05-01T07:00:00Z application/pdf https://digitalcommons.usf.edu/geo_facpub/1542 https://doi.org/10.1002/ggge.20089 https://digitalcommons.usf.edu/context/geo_facpub/article/2461/viewcontent/Yang_et_al_2013_Geochemistry__Geophysics__Geosystems.pdf https://digitalcommons.usf.edu/context/geo_facpub/article/2461/filename/0/type/additional/viewcontent/Supplementary_Information.pdf https://digitalcommons.usf.edu/context/geo_facpub/article/2461/filename/1/type/additional/viewcontent/2012gc004432pa01.pdf https://digitalcommons.usf.edu/context/geo_facpub/article/2461/filename/2/type/additional/viewcontent/2012gc004432pa02.pdf https://digitalcommons.usf.edu/context/geo_facpub/article/2461/filename/3/type/additional/viewcontent/2012gc004432pa03.pdf https://digitalcommons.usf.edu/context/geo_facpub/article/2461/filename/4/type/additional/viewcontent/2012gc004432pa04.pdf https://digitalcommons.usf.edu/context/geo_facpub/article/2461/filename/5/type/additional/viewcontent/2012gc004432pa05a.pdf https://digitalcommons.usf.edu/context/geo_facpub/article/2461/filename/6/type/additional/viewcontent/2012gc004432pa05b.pdf https://digitalcommons.usf.edu/context/geo_facpub/article/2461/filename/7/type/additional/viewcontent/2012gc004432pa06a.pdf https://digitalcommons.usf.edu/context/geo_facpub/article/2461/filename/8/type/additional/viewcontent/2012gc004432pa06b.pdf https://digitalcommons.usf.edu/context/geo_facpub/article/2461/filename/9/type/additional/viewcontent/2012gc004432pa07.pdf https://digitalcommons.usf.edu/context/geo_facpub/article/2461/filename/10/type/additional/viewcontent/2012gc004432readme.txt unknown Digital Commons @ University of South Florida https://digitalcommons.usf.edu/geo_facpub/1542 doi:10.1002/ggge.20089 https://digitalcommons.usf.edu/context/geo_facpub/article/2461/viewcontent/Yang_et_al_2013_Geochemistry__Geophysics__Geosystems.pdf https://digitalcommons.usf.edu/context/geo_facpub/article/2461/filename/0/type/additional/viewcontent/Supplementary_Information.pdf https://digitalcommons.usf.edu/context/geo_facpub/article/2461/filename/1/type/additional/viewcontent/2012gc004432pa01.pdf https://digitalcommons.usf.edu/context/geo_facpub/article/2461/filename/2/type/additional/viewcontent/2012gc004432pa02.pdf https://digitalcommons.usf.edu/context/geo_facpub/article/2461/filename/3/type/additional/viewcontent/2012gc004432pa03.pdf https://digitalcommons.usf.edu/context/geo_facpub/article/2461/filename/4/type/additional/viewcontent/2012gc004432pa04.pdf https://digitalcommons.usf.edu/context/geo_facpub/article/2461/filename/5/type/additional/viewcontent/2012gc004432pa05a.pdf https://digitalcommons.usf.edu/context/geo_facpub/article/2461/filename/6/type/additional/viewcontent/2012gc004432pa05b.pdf https://digitalcommons.usf.edu/context/geo_facpub/article/2461/filename/7/type/additional/viewcontent/2012gc004432pa06a.pdf https://digitalcommons.usf.edu/context/geo_facpub/article/2461/filename/8/type/additional/viewcontent/2012gc004432pa06b.pdf https://digitalcommons.usf.edu/context/geo_facpub/article/2461/filename/9/type/additional/viewcontent/2012gc004432pa07.pdf https://digitalcommons.usf.edu/context/geo_facpub/article/2461/filename/10/type/additional/viewcontent/2012gc004432readme.txt default School of Geosciences Faculty and Staff Publications Greenland's ice sheet GPS vertical displacement seasonal melting climatic forcings Earth Sciences article 2013 ftusouthflorida https://doi.org/10.1002/ggge.20089 2023-07-13T20:43:52Z Seasonal melting of the coastal part of the Greenland ice sheet is investigated using GPS vertical displacement data from coastal stations, combined with data on atmospheric and ocean temperatures. Using a high pass filter and cubic spline models, we estimate five variables describing seasonal uplift, a proxy for proximal mass loss, including duration of the melt season and the amount of summer uplift. Our analysis shows both temporal and spatial variations of uplift. Southern coastal Greenland experienced anomalously large uplift in summer 2010, implying significant melting that year. However, the northwest coast did not experience significant change in uplift at that time. Our data suggest that a combination of warm summer air temperature and warm sub‐surface ocean water temperature drove the large mass losses in 2010. Using the uplift pattern of 2008–2010, and comparing to atmospheric data and ocean water temperature data, we show that warm Irminger Water (IW) exerted significant influence on coastal melting in southeastern, southern and southwestern Greenland, reaching about 69°N in 2010. North of this, IW did not exert significant influence, in effect defining the northward limit of the sub‐polar gyre for that year. Thus, short‐term variability in the coastal GPS uplift signal can be used to infer an oceanographic parameter that has a critical influence on Greenland ice sheet health. Article in Journal/Newspaper Greenland Ice Sheet University of South Florida St. Petersburg: Digital USFSP Greenland Geochemistry, Geophysics, Geosystems 14 5 1569 1589