Acceleration of the Greenland ice sheet mass loss as observed by GRACE: Confidence and sensitivity

We examine the scale and spatial distribution of the mass change acceleration in Greenland and its statistical significance, using processed gravimetric data from the GRACE mission for the period 2002-2011. Three different data products - the CNES/GRGS, DMT-1b and GGFC GRACE solutions - have been us...

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Published in:Earth and Planetary Science Letters
Main Authors: Svendsen, Peter Limkilde, Andersen, Ole Baltazar, Nielsen, Allan Aasbjerg
Format: Article in Journal/Newspaper
Language:English
Published: 2013
Subjects:
Online Access:https://orbit.dtu.dk/en/publications/4e02c11f-3316-4d0f-9362-5412b1a8f2a0
https://doi.org/10.1016/j.epsl.2012.12.010
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spelling ftdtupubl:oai:pure.atira.dk:publications/4e02c11f-3316-4d0f-9362-5412b1a8f2a0 2024-03-31T07:49:48+00:00 Acceleration of the Greenland ice sheet mass loss as observed by GRACE: Confidence and sensitivity Svendsen, Peter Limkilde Andersen, Ole Baltazar Nielsen, Allan Aasbjerg 2013 https://orbit.dtu.dk/en/publications/4e02c11f-3316-4d0f-9362-5412b1a8f2a0 https://doi.org/10.1016/j.epsl.2012.12.010 eng eng https://orbit.dtu.dk/en/publications/4e02c11f-3316-4d0f-9362-5412b1a8f2a0 info:eu-repo/semantics/closedAccess Svendsen , P L , Andersen , O B & Nielsen , A A 2013 , ' Acceleration of the Greenland ice sheet mass loss as observed by GRACE: Confidence and sensitivity ' , Earth and Planetary Science Letters , vol. 364 , pp. 24-29 . https://doi.org/10.1016/j.epsl.2012.12.010 Geology Mathematical models Acceleration article 2013 ftdtupubl https://doi.org/10.1016/j.epsl.2012.12.010 2024-03-06T00:57:37Z We examine the scale and spatial distribution of the mass change acceleration in Greenland and its statistical significance, using processed gravimetric data from the GRACE mission for the period 2002-2011. Three different data products - the CNES/GRGS, DMT-1b and GGFC GRACE solutions - have been used, all revealing an accelerating mass loss in Greenland, though with significant local differences between the three datasets. Compensating for leakage effects, we obtain acceleration values of -18.6 Gt / yr2 for CNES/GRGS, -8.8 Gt / yr2 for DMT-1b, and -14.8 Gt / yr2 for GGFC.We find considerable mass loss acceleration in the Canadian Arctic Archipelago, some of which will leak into the values for Greenland, depending on the approach used, and for our computations the leakage has been estimated at up to -4.7 Gt / yr2.The length of the time series of the GRACE data makes a huge difference in establishing an acceleration of the data. For both 10-day and monthly GRACE solutions, an observed acceleration on the order of 10 - 20 Gt / yr2 is shown to require more than 5 yrs of data to establish with statistical significance.In order to provide an independent evaluation, ICESat laser altimetry data have been smoothed to match the resolution of the GRACE solutions. This gives us an estimated upper bound for the acceleration of about -29.7 Gt / yr2 for the period 2003-2009, consistent with the acceleration values and corresponding confidence intervals found with GRACE data. © 2012 Elsevier B.V. Article in Journal/Newspaper Arctic Archipelago Arctic Canadian Arctic Archipelago Greenland Ice Sheet Technical University of Denmark: DTU Orbit Arctic Canadian Arctic Archipelago Greenland Earth and Planetary Science Letters 364 24 29
institution Open Polar
collection Technical University of Denmark: DTU Orbit
op_collection_id ftdtupubl
language English
topic Geology
Mathematical models
Acceleration
spellingShingle Geology
Mathematical models
Acceleration
Svendsen, Peter Limkilde
Andersen, Ole Baltazar
Nielsen, Allan Aasbjerg
Acceleration of the Greenland ice sheet mass loss as observed by GRACE: Confidence and sensitivity
topic_facet Geology
Mathematical models
Acceleration
description We examine the scale and spatial distribution of the mass change acceleration in Greenland and its statistical significance, using processed gravimetric data from the GRACE mission for the period 2002-2011. Three different data products - the CNES/GRGS, DMT-1b and GGFC GRACE solutions - have been used, all revealing an accelerating mass loss in Greenland, though with significant local differences between the three datasets. Compensating for leakage effects, we obtain acceleration values of -18.6 Gt / yr2 for CNES/GRGS, -8.8 Gt / yr2 for DMT-1b, and -14.8 Gt / yr2 for GGFC.We find considerable mass loss acceleration in the Canadian Arctic Archipelago, some of which will leak into the values for Greenland, depending on the approach used, and for our computations the leakage has been estimated at up to -4.7 Gt / yr2.The length of the time series of the GRACE data makes a huge difference in establishing an acceleration of the data. For both 10-day and monthly GRACE solutions, an observed acceleration on the order of 10 - 20 Gt / yr2 is shown to require more than 5 yrs of data to establish with statistical significance.In order to provide an independent evaluation, ICESat laser altimetry data have been smoothed to match the resolution of the GRACE solutions. This gives us an estimated upper bound for the acceleration of about -29.7 Gt / yr2 for the period 2003-2009, consistent with the acceleration values and corresponding confidence intervals found with GRACE data. © 2012 Elsevier B.V.
format Article in Journal/Newspaper
author Svendsen, Peter Limkilde
Andersen, Ole Baltazar
Nielsen, Allan Aasbjerg
author_facet Svendsen, Peter Limkilde
Andersen, Ole Baltazar
Nielsen, Allan Aasbjerg
author_sort Svendsen, Peter Limkilde
title Acceleration of the Greenland ice sheet mass loss as observed by GRACE: Confidence and sensitivity
title_short Acceleration of the Greenland ice sheet mass loss as observed by GRACE: Confidence and sensitivity
title_full Acceleration of the Greenland ice sheet mass loss as observed by GRACE: Confidence and sensitivity
title_fullStr Acceleration of the Greenland ice sheet mass loss as observed by GRACE: Confidence and sensitivity
title_full_unstemmed Acceleration of the Greenland ice sheet mass loss as observed by GRACE: Confidence and sensitivity
title_sort acceleration of the greenland ice sheet mass loss as observed by grace: confidence and sensitivity
publishDate 2013
url https://orbit.dtu.dk/en/publications/4e02c11f-3316-4d0f-9362-5412b1a8f2a0
https://doi.org/10.1016/j.epsl.2012.12.010
geographic Arctic
Canadian Arctic Archipelago
Greenland
geographic_facet Arctic
Canadian Arctic Archipelago
Greenland
genre Arctic Archipelago
Arctic
Canadian Arctic Archipelago
Greenland
Ice Sheet
genre_facet Arctic Archipelago
Arctic
Canadian Arctic Archipelago
Greenland
Ice Sheet
op_source Svendsen , P L , Andersen , O B & Nielsen , A A 2013 , ' Acceleration of the Greenland ice sheet mass loss as observed by GRACE: Confidence and sensitivity ' , Earth and Planetary Science Letters , vol. 364 , pp. 24-29 . https://doi.org/10.1016/j.epsl.2012.12.010
op_relation https://orbit.dtu.dk/en/publications/4e02c11f-3316-4d0f-9362-5412b1a8f2a0
op_rights info:eu-repo/semantics/closedAccess
op_doi https://doi.org/10.1016/j.epsl.2012.12.010
container_title Earth and Planetary Science Letters
container_volume 364
container_start_page 24
op_container_end_page 29
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