Evaluation of Terrestrial Water Storage Changes and Major Driving Factors Analysis in Inner Mongolia, China

Quantitative assessment of the terrestrial water storage (TWS) changes and the major driving factors have been hindered by the lack of direct observations in Inner Mongolia, China. In this study, the spatial and temporal changes of TWS and groundwater storage (GWS) in Inner Mongolia during 2003–2021...

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Main Authors: Yi Guo, Fuping Gan, Baikun Yan, Juan Bai, Naichen Xing, Yue Zhuo
Format: Article
Language:English
Published: MDPI AG 2022-12-01
Series:Sensors
Subjects:
Online Access:https://www.mdpi.com/1424-8220/22/24/9665
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author Yi Guo
Fuping Gan
Baikun Yan
Juan Bai
Naichen Xing
Yue Zhuo
author_facet Yi Guo
Fuping Gan
Baikun Yan
Juan Bai
Naichen Xing
Yue Zhuo
author_sort Yi Guo
collection DOAJ
description Quantitative assessment of the terrestrial water storage (TWS) changes and the major driving factors have been hindered by the lack of direct observations in Inner Mongolia, China. In this study, the spatial and temporal changes of TWS and groundwater storage (GWS) in Inner Mongolia during 2003–2021 were evaluated using the satellite gravity data from the Gravity Recovery and Climate Experiment (GRACE) and the GRACE Follow On combined with data from land surface models. The results indicated that Inner Mongolia has experienced a widespread TWS loss of approximately 1.82 mm/yr from 2003–2021, with a more severe depletion rate of 4.15 mm/yr for GWS. Meteorological factors were the driving factors for water storage changes in northeastern and western regions. The abundant precipitation increased TWS in northeast regions at 2.36 mm/yr. Anthropogenic activities (agricultural irrigation and coal mining) were the driving factors for water resource decline in the middle and eastern regions (especially in the agropastoral transitional zone), where the decrease rates were 4.09 mm/yr and 3.69 mm/yr, respectively. In addition, the severities of hydrological drought events were identified based on water storage deficits, with average severity values of 17 mm, 18 mm, 24 mm, and 33 mm for the west, middle, east, and northeast regions, respectively. This study established a basic framework for water resource changes in Inner Mongolia and provided a scientific foundation for further water resources investigation.
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spelling doaj.art-3c1932e318e640a3bb0218753d6f5ed22023-11-24T17:53:17ZengMDPI AGSensors1424-82202022-12-012224966510.3390/s22249665Evaluation of Terrestrial Water Storage Changes and Major Driving Factors Analysis in Inner Mongolia, ChinaYi Guo0Fuping Gan1Baikun Yan2Juan Bai3Naichen Xing4Yue Zhuo5China Aero Geophysical Survey and Remote Sensing Center for Natural Resources, China Geological Survey, Beijing 100083, ChinaChina Aero Geophysical Survey and Remote Sensing Center for Natural Resources, China Geological Survey, Beijing 100083, ChinaChina Aero Geophysical Survey and Remote Sensing Center for Natural Resources, China Geological Survey, Beijing 100083, ChinaChina Aero Geophysical Survey and Remote Sensing Center for Natural Resources, China Geological Survey, Beijing 100083, ChinaChina Aero Geophysical Survey and Remote Sensing Center for Natural Resources, China Geological Survey, Beijing 100083, ChinaChina Aero Geophysical Survey and Remote Sensing Center for Natural Resources, China Geological Survey, Beijing 100083, ChinaQuantitative assessment of the terrestrial water storage (TWS) changes and the major driving factors have been hindered by the lack of direct observations in Inner Mongolia, China. In this study, the spatial and temporal changes of TWS and groundwater storage (GWS) in Inner Mongolia during 2003–2021 were evaluated using the satellite gravity data from the Gravity Recovery and Climate Experiment (GRACE) and the GRACE Follow On combined with data from land surface models. The results indicated that Inner Mongolia has experienced a widespread TWS loss of approximately 1.82 mm/yr from 2003–2021, with a more severe depletion rate of 4.15 mm/yr for GWS. Meteorological factors were the driving factors for water storage changes in northeastern and western regions. The abundant precipitation increased TWS in northeast regions at 2.36 mm/yr. Anthropogenic activities (agricultural irrigation and coal mining) were the driving factors for water resource decline in the middle and eastern regions (especially in the agropastoral transitional zone), where the decrease rates were 4.09 mm/yr and 3.69 mm/yr, respectively. In addition, the severities of hydrological drought events were identified based on water storage deficits, with average severity values of 17 mm, 18 mm, 24 mm, and 33 mm for the west, middle, east, and northeast regions, respectively. This study established a basic framework for water resource changes in Inner Mongolia and provided a scientific foundation for further water resources investigation.https://www.mdpi.com/1424-8220/22/24/9665GRACEland surface modelTWSGWSclimate changesagricultural irrigation
spellingShingle Yi Guo
Fuping Gan
Baikun Yan
Juan Bai
Naichen Xing
Yue Zhuo
Evaluation of Terrestrial Water Storage Changes and Major Driving Factors Analysis in Inner Mongolia, China
Sensors
GRACE
land surface model
TWS
GWS
climate changes
agricultural irrigation
title Evaluation of Terrestrial Water Storage Changes and Major Driving Factors Analysis in Inner Mongolia, China
title_full Evaluation of Terrestrial Water Storage Changes and Major Driving Factors Analysis in Inner Mongolia, China
title_fullStr Evaluation of Terrestrial Water Storage Changes and Major Driving Factors Analysis in Inner Mongolia, China
title_full_unstemmed Evaluation of Terrestrial Water Storage Changes and Major Driving Factors Analysis in Inner Mongolia, China
title_short Evaluation of Terrestrial Water Storage Changes and Major Driving Factors Analysis in Inner Mongolia, China
title_sort evaluation of terrestrial water storage changes and major driving factors analysis in inner mongolia china
topic GRACE
land surface model
TWS
GWS
climate changes
agricultural irrigation
url https://www.mdpi.com/1424-8220/22/24/9665
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