Constraining mass variations in the Siberian permafrost region based on GRACE and Satellite Altimetry

The permafrost layers in the Siberia (Russia) with different thicknesses cover about 80% of this region. Therefore these frozen sheets play an important role for the hydrological water cycle of the Earth system. The integral mass variations in the Earth system with different spatial-temporal resolut...

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Main Authors: Shabanloui, Akbar, Müller, Jürgen
Format: Conference Object
Language:English
Published: 2014
Subjects:
Online Access:https://www.repo.uni-hannover.de/handle/123456789/4598
https://doi.org/10.15488/4556
id ftunivhannover:oai:www.repo.uni-hannover.de:123456789/4598
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spelling ftunivhannover:oai:www.repo.uni-hannover.de:123456789/4598 2023-07-16T04:00:27+02:00 Constraining mass variations in the Siberian permafrost region based on GRACE and Satellite Altimetry Shabanloui, Akbar Müller, Jürgen 2014-10-07 https://www.repo.uni-hannover.de/handle/123456789/4598 https://doi.org/10.15488/4556 eng eng http://dx.doi.org/10.15488/4556 https://www.repo.uni-hannover.de/handle/123456789/4598 Es gilt deutsches Urheberrecht. Das Dokument darf zum eigenen Gebrauch kostenfrei genutzt, aber nicht im Internet bereitgestellt oder an Außenstehende weitergegeben werden. frei zugänglich Mass variations from GRACE Level 2 Products Satellite Altimetry Siberia Permafrost region Massenvariationen aus GRACE Level2 Produkten Massenverteilung Satellitengravimetrie Satelliten-Altimetrie Siberian Permafrostgebiet ddc:620 ddc:520 status-type:publishedVersion doc-type:ConferenceObject doc-type:Text 2014 ftunivhannover https://doi.org/10.15488/4556 2023-06-28T10:37:10Z The permafrost layers in the Siberia (Russia) with different thicknesses cover about 80% of this region. Therefore these frozen sheets play an important role for the hydrological water cycle of the Earth system. The integral mass variations in the Earth system with different spatial-temporal resolution are determined based on GRACE observations/products. On the one hand, the mass variations in this region are precisely estimated based on the new release of GRACE Level 2 products from GFZ (RL05a). On the other hand, these (hydrological) mass variations can be geometrically determined based on satellite (radar/laser) altimetry tracking data. The mass variations in this region are extracted from lake (see) level variations that observed by satellite altimetry missions (e.g. Jason-2, ICESat). In this investigation, the mass variations in the Siberian region that concluded from satellite altimetry missions are used to constrain hydrological mass variations from GRACE mission. This sort of constraining results should present a realistic mass transport pattern. Conference Object permafrost Siberia Institutional Repository of Leibniz Universität Hannover
institution Open Polar
collection Institutional Repository of Leibniz Universität Hannover
op_collection_id ftunivhannover
language English
topic Mass variations from GRACE Level 2 Products
Satellite Altimetry
Siberia Permafrost region
Massenvariationen aus GRACE Level2 Produkten
Massenverteilung
Satellitengravimetrie
Satelliten-Altimetrie
Siberian Permafrostgebiet
ddc:620
ddc:520
spellingShingle Mass variations from GRACE Level 2 Products
Satellite Altimetry
Siberia Permafrost region
Massenvariationen aus GRACE Level2 Produkten
Massenverteilung
Satellitengravimetrie
Satelliten-Altimetrie
Siberian Permafrostgebiet
ddc:620
ddc:520
Shabanloui, Akbar
Müller, Jürgen
Constraining mass variations in the Siberian permafrost region based on GRACE and Satellite Altimetry
topic_facet Mass variations from GRACE Level 2 Products
Satellite Altimetry
Siberia Permafrost region
Massenvariationen aus GRACE Level2 Produkten
Massenverteilung
Satellitengravimetrie
Satelliten-Altimetrie
Siberian Permafrostgebiet
ddc:620
ddc:520
description The permafrost layers in the Siberia (Russia) with different thicknesses cover about 80% of this region. Therefore these frozen sheets play an important role for the hydrological water cycle of the Earth system. The integral mass variations in the Earth system with different spatial-temporal resolution are determined based on GRACE observations/products. On the one hand, the mass variations in this region are precisely estimated based on the new release of GRACE Level 2 products from GFZ (RL05a). On the other hand, these (hydrological) mass variations can be geometrically determined based on satellite (radar/laser) altimetry tracking data. The mass variations in this region are extracted from lake (see) level variations that observed by satellite altimetry missions (e.g. Jason-2, ICESat). In this investigation, the mass variations in the Siberian region that concluded from satellite altimetry missions are used to constrain hydrological mass variations from GRACE mission. This sort of constraining results should present a realistic mass transport pattern.
format Conference Object
author Shabanloui, Akbar
Müller, Jürgen
author_facet Shabanloui, Akbar
Müller, Jürgen
author_sort Shabanloui, Akbar
title Constraining mass variations in the Siberian permafrost region based on GRACE and Satellite Altimetry
title_short Constraining mass variations in the Siberian permafrost region based on GRACE and Satellite Altimetry
title_full Constraining mass variations in the Siberian permafrost region based on GRACE and Satellite Altimetry
title_fullStr Constraining mass variations in the Siberian permafrost region based on GRACE and Satellite Altimetry
title_full_unstemmed Constraining mass variations in the Siberian permafrost region based on GRACE and Satellite Altimetry
title_sort constraining mass variations in the siberian permafrost region based on grace and satellite altimetry
publishDate 2014
url https://www.repo.uni-hannover.de/handle/123456789/4598
https://doi.org/10.15488/4556
genre permafrost
Siberia
genre_facet permafrost
Siberia
op_relation http://dx.doi.org/10.15488/4556
https://www.repo.uni-hannover.de/handle/123456789/4598
op_rights Es gilt deutsches Urheberrecht. Das Dokument darf zum eigenen Gebrauch kostenfrei genutzt, aber nicht im Internet bereitgestellt oder an Außenstehende weitergegeben werden.
frei zugänglich
op_doi https://doi.org/10.15488/4556
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