Widespread Decline in Terrestrial Water Storage and Its Link to Teleconnections across Asia and Eastern Europe

Recent global changes in terrestrial water storage (TWS) and associated freshwater availability raise major concerns over the sustainability of global water resources. However, our knowledge regarding the long-term trend in TWS and its components is still not well documented. In this work, we charac...

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Main Authors: Liu, Xianfeng, Feng, Xiaoming, Ciais, Philippe, Fu, Bojie
Format: Text
Language:English
Published: 2019
Subjects:
Online Access:https://doi.org/10.5194/hess-2019-281
https://www.hydrol-earth-syst-sci-discuss.net/hess-2019-281/
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spelling ftcopernicus:oai:publications.copernicus.org:hessd77230 2023-05-15T15:09:20+02:00 Widespread Decline in Terrestrial Water Storage and Its Link to Teleconnections across Asia and Eastern Europe Liu, Xianfeng Feng, Xiaoming Ciais, Philippe Fu, Bojie 2019-08-15 application/pdf https://doi.org/10.5194/hess-2019-281 https://www.hydrol-earth-syst-sci-discuss.net/hess-2019-281/ eng eng doi:10.5194/hess-2019-281 https://www.hydrol-earth-syst-sci-discuss.net/hess-2019-281/ eISSN: 1607-7938 Text 2019 ftcopernicus https://doi.org/10.5194/hess-2019-281 2019-12-24T09:48:43Z Recent global changes in terrestrial water storage (TWS) and associated freshwater availability raise major concerns over the sustainability of global water resources. However, our knowledge regarding the long-term trend in TWS and its components is still not well documented. In this work, we characterize the spatiotemporal variations in TWS and its components over the Asian and Eastern European regions during the period of April 2002 to June 2017 using multiple sources of data, including Gravity Recovery and Climate Experiment (GRACE) satellite observations, land surface model simulations and precipitation observations. The connections of TWS and global major teleconnections (TCs) are also discussed. The results indicate a widespread decline in TWS during 2002–2017, and five hotspots of TWS negative trends were identified with trends between −8.94 mm yr −1 and −21.79 mm yr −1 . TWS partitioning suggests that these negative trends are primarily attributed to the intensive overextraction of groundwater and warm-induced surface water loss, but the contributions of each hydrological component vary among hotspots. The results also indicate that the El Niño-Southern Oscillation, Arctic Oscillation and North Atlantic Oscillation are the three largest, dominant factors controlling the variations in TWS through the covariability effect on climate variables. However, seasonal results suggest a divergent response of hydrological components to TCs among seasons and hotspots. Our findings provide insights into changes in TWS and its components over the Asian and Eastern European regions, where there is a growing demand for food grains and water supplies. Text Arctic North Atlantic North Atlantic oscillation Copernicus Publications: E-Journals Arctic
institution Open Polar
collection Copernicus Publications: E-Journals
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language English
description Recent global changes in terrestrial water storage (TWS) and associated freshwater availability raise major concerns over the sustainability of global water resources. However, our knowledge regarding the long-term trend in TWS and its components is still not well documented. In this work, we characterize the spatiotemporal variations in TWS and its components over the Asian and Eastern European regions during the period of April 2002 to June 2017 using multiple sources of data, including Gravity Recovery and Climate Experiment (GRACE) satellite observations, land surface model simulations and precipitation observations. The connections of TWS and global major teleconnections (TCs) are also discussed. The results indicate a widespread decline in TWS during 2002–2017, and five hotspots of TWS negative trends were identified with trends between −8.94 mm yr −1 and −21.79 mm yr −1 . TWS partitioning suggests that these negative trends are primarily attributed to the intensive overextraction of groundwater and warm-induced surface water loss, but the contributions of each hydrological component vary among hotspots. The results also indicate that the El Niño-Southern Oscillation, Arctic Oscillation and North Atlantic Oscillation are the three largest, dominant factors controlling the variations in TWS through the covariability effect on climate variables. However, seasonal results suggest a divergent response of hydrological components to TCs among seasons and hotspots. Our findings provide insights into changes in TWS and its components over the Asian and Eastern European regions, where there is a growing demand for food grains and water supplies.
format Text
author Liu, Xianfeng
Feng, Xiaoming
Ciais, Philippe
Fu, Bojie
spellingShingle Liu, Xianfeng
Feng, Xiaoming
Ciais, Philippe
Fu, Bojie
Widespread Decline in Terrestrial Water Storage and Its Link to Teleconnections across Asia and Eastern Europe
author_facet Liu, Xianfeng
Feng, Xiaoming
Ciais, Philippe
Fu, Bojie
author_sort Liu, Xianfeng
title Widespread Decline in Terrestrial Water Storage and Its Link to Teleconnections across Asia and Eastern Europe
title_short Widespread Decline in Terrestrial Water Storage and Its Link to Teleconnections across Asia and Eastern Europe
title_full Widespread Decline in Terrestrial Water Storage and Its Link to Teleconnections across Asia and Eastern Europe
title_fullStr Widespread Decline in Terrestrial Water Storage and Its Link to Teleconnections across Asia and Eastern Europe
title_full_unstemmed Widespread Decline in Terrestrial Water Storage and Its Link to Teleconnections across Asia and Eastern Europe
title_sort widespread decline in terrestrial water storage and its link to teleconnections across asia and eastern europe
publishDate 2019
url https://doi.org/10.5194/hess-2019-281
https://www.hydrol-earth-syst-sci-discuss.net/hess-2019-281/
geographic Arctic
geographic_facet Arctic
genre Arctic
North Atlantic
North Atlantic oscillation
genre_facet Arctic
North Atlantic
North Atlantic oscillation
op_source eISSN: 1607-7938
op_relation doi:10.5194/hess-2019-281
https://www.hydrol-earth-syst-sci-discuss.net/hess-2019-281/
op_doi https://doi.org/10.5194/hess-2019-281
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