Evaluation of Water Storage Change of Inland Cryosphere in Northwestern China

The Gravity Recovery and Climate Experiment (GRACE) satellite mission provides measurements of Earth’s static and time-variable gravity fields with monthly resolution. In this study, changes of water storage in northwestern China were determined by GRACE monthly gravity field data obtained from 2003...

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Published in:Advances in Meteorology
Main Authors: Min Xu, Shichang Kang, Jiazhen Li
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2015
Subjects:
Online Access:https://doi.org/10.1155/2015/681634
https://doaj.org/article/3885eadc7254434bb04888f092b635ab
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spelling ftdoajarticles:oai:doaj.org/article:3885eadc7254434bb04888f092b635ab 2024-09-15T18:30:04+00:00 Evaluation of Water Storage Change of Inland Cryosphere in Northwestern China Min Xu Shichang Kang Jiazhen Li 2015-01-01T00:00:00Z https://doi.org/10.1155/2015/681634 https://doaj.org/article/3885eadc7254434bb04888f092b635ab EN eng Wiley http://dx.doi.org/10.1155/2015/681634 https://doaj.org/toc/1687-9309 https://doaj.org/toc/1687-9317 1687-9309 1687-9317 doi:10.1155/2015/681634 https://doaj.org/article/3885eadc7254434bb04888f092b635ab Advances in Meteorology, Vol 2015 (2015) Meteorology. Climatology QC851-999 article 2015 ftdoajarticles https://doi.org/10.1155/2015/681634 2024-08-05T17:48:40Z The Gravity Recovery and Climate Experiment (GRACE) satellite mission provides measurements of Earth’s static and time-variable gravity fields with monthly resolution. In this study, changes of water storage in northwestern China were determined by GRACE monthly gravity field data obtained from 2003 to 2010. Comparisons of water storage change (WSC) simulated by a four-dimensional assimilation model (Noah) and observed by GRACE revealed similar patterns of change and a correlation coefficient of 0.71 (P<0.05). Trend analysis indicated significant changes in the spatiotemporal variation of WSC in northwestern China during the 8-year study period, which were stronger in the east than in the west and more pronounced in the south than in the north. The most pronounced increase in water storage occurred in Gansu and Qinghai provinces, but, overall, water storage increased by 0.61 mm/a over northwestern China during the study period. Clear seasonal variations of WSC and precipitation were found, because glacial meltwater and precipitation are the main sources of water in the hydrosphere; meanwhile, the distributions of glaciers and permafrost also affect the spatial distribution of WSC. Article in Journal/Newspaper permafrost Directory of Open Access Journals: DOAJ Articles Advances in Meteorology 2015 1 12
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Meteorology. Climatology
QC851-999
spellingShingle Meteorology. Climatology
QC851-999
Min Xu
Shichang Kang
Jiazhen Li
Evaluation of Water Storage Change of Inland Cryosphere in Northwestern China
topic_facet Meteorology. Climatology
QC851-999
description The Gravity Recovery and Climate Experiment (GRACE) satellite mission provides measurements of Earth’s static and time-variable gravity fields with monthly resolution. In this study, changes of water storage in northwestern China were determined by GRACE monthly gravity field data obtained from 2003 to 2010. Comparisons of water storage change (WSC) simulated by a four-dimensional assimilation model (Noah) and observed by GRACE revealed similar patterns of change and a correlation coefficient of 0.71 (P<0.05). Trend analysis indicated significant changes in the spatiotemporal variation of WSC in northwestern China during the 8-year study period, which were stronger in the east than in the west and more pronounced in the south than in the north. The most pronounced increase in water storage occurred in Gansu and Qinghai provinces, but, overall, water storage increased by 0.61 mm/a over northwestern China during the study period. Clear seasonal variations of WSC and precipitation were found, because glacial meltwater and precipitation are the main sources of water in the hydrosphere; meanwhile, the distributions of glaciers and permafrost also affect the spatial distribution of WSC.
format Article in Journal/Newspaper
author Min Xu
Shichang Kang
Jiazhen Li
author_facet Min Xu
Shichang Kang
Jiazhen Li
author_sort Min Xu
title Evaluation of Water Storage Change of Inland Cryosphere in Northwestern China
title_short Evaluation of Water Storage Change of Inland Cryosphere in Northwestern China
title_full Evaluation of Water Storage Change of Inland Cryosphere in Northwestern China
title_fullStr Evaluation of Water Storage Change of Inland Cryosphere in Northwestern China
title_full_unstemmed Evaluation of Water Storage Change of Inland Cryosphere in Northwestern China
title_sort evaluation of water storage change of inland cryosphere in northwestern china
publisher Wiley
publishDate 2015
url https://doi.org/10.1155/2015/681634
https://doaj.org/article/3885eadc7254434bb04888f092b635ab
genre permafrost
genre_facet permafrost
op_source Advances in Meteorology, Vol 2015 (2015)
op_relation http://dx.doi.org/10.1155/2015/681634
https://doaj.org/toc/1687-9309
https://doaj.org/toc/1687-9317
1687-9309
1687-9317
doi:10.1155/2015/681634
https://doaj.org/article/3885eadc7254434bb04888f092b635ab
op_doi https://doi.org/10.1155/2015/681634
container_title Advances in Meteorology
container_volume 2015
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op_container_end_page 12
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