Effects of climate change and agricultural expansion on groundwater storage in the Amur River Basin

Since the 1990s, the climate in the Amur River Basin (ARB) has changed, and large-scale wetlands in the region have been reclaimed for paddy fields. The study of the influence of climate change and agricultural expansion on groundwater storage is of great significance to the evaluation of regional w...

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Main Authors: Zhengang Zhang, Changchun Song, Yuedong Guo, Panxing He, Ning Chen, Jianzhao Liu, Yifei Zhang, Yunjiang Zuo, Xing Zhang
Format: Article
Language:English
Published: Frontiers Media S.A. 2023-01-01
Series:Frontiers in Earth Science
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/feart.2022.1037688/full
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author Zhengang Zhang
Zhengang Zhang
Changchun Song
Changchun Song
Yuedong Guo
Panxing He
Ning Chen
Jianzhao Liu
Jianzhao Liu
Yifei Zhang
Yifei Zhang
Yunjiang Zuo
Yunjiang Zuo
Xing Zhang
Xing Zhang
author_facet Zhengang Zhang
Zhengang Zhang
Changchun Song
Changchun Song
Yuedong Guo
Panxing He
Ning Chen
Jianzhao Liu
Jianzhao Liu
Yifei Zhang
Yifei Zhang
Yunjiang Zuo
Yunjiang Zuo
Xing Zhang
Xing Zhang
author_sort Zhengang Zhang
collection DOAJ
description Since the 1990s, the climate in the Amur River Basin (ARB) has changed, and large-scale wetlands in the region have been reclaimed for paddy fields. The study of the influence of climate change and agricultural expansion on groundwater storage is of great significance to the evaluation of regional water resource balance and the promotion of ecological protection and agricultural development. In this work, the groundwater storage anomaly (GWSA) in the ARB and its drivers were analyzed for the period 2003–2016 using Gravity Recovery and Climate Experiment (GRACE) satellite data, a Global Land Data Assimilation System model, and in situ observations of groundwater levels. Results indicated that 1) the GWSA in the ARB increased at a rate of 2.0–2.4 mm/yr from 2003 to 2016; the GWSA in the upper reaches of the ARB increased, whereas the GWSA in the middle and lower reaches decreased during the study period. 2) The GWSA in the middle and lower reaches of the ARB was greatly influenced by temperature (Tmp) and evapotranspiration (ET). Tmp was positively correlated with GWSA, whereas ET was negatively correlated with GWSA (p < 0.05). 3) Extreme rainfall had a delayed effect on groundwater recharge. Wetland degradation and agricultural development were the main factors causing the decrease of the GWSA in the middle and lower reaches of the ARB. In summary, temperature and evapotranspiration affect groundwater storage by regulating the water–heat balance, wetland reclamation reduces the regional storage capacity, and the irrigation required for reclaimed farmland is the main source of groundwater loss.
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spelling doaj.art-34c6a58a9b8c4bd5b2e17a370ae6d9ab2023-01-09T05:21:19ZengFrontiers Media S.A.Frontiers in Earth Science2296-64632023-01-011010.3389/feart.2022.10376881037688Effects of climate change and agricultural expansion on groundwater storage in the Amur River BasinZhengang Zhang0Zhengang Zhang1Changchun Song2Changchun Song3Yuedong Guo4Panxing He5Ning Chen6Jianzhao Liu7Jianzhao Liu8Yifei Zhang9Yifei Zhang10Yunjiang Zuo11Yunjiang Zuo12Xing Zhang13Xing Zhang14Key Laboratory of Wetland Ecology and Environment, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun, ChinaUniversity of Chinese Academy Sciences, Beijing, ChinaKey Laboratory of Wetland Ecology and Environment, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun, ChinaSchool of Hydraulic Engineering, Dalian University of Technology, Dalian, ChinaKey Laboratory of Wetland Ecology and Environment, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun, ChinaMinistry of Education Key Laboratory for Western Arid Region Grassland Resources and Ecology, Xinjiang Agricultural University, Urumqi, ChinaKey Laboratory of Wetland Ecology and Environment, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun, ChinaKey Laboratory of Wetland Ecology and Environment, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun, ChinaUniversity of Chinese Academy Sciences, Beijing, ChinaKey Laboratory of Wetland Ecology and Environment, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun, ChinaUniversity of Chinese Academy Sciences, Beijing, ChinaKey Laboratory of Wetland Ecology and Environment, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun, ChinaUniversity of Chinese Academy Sciences, Beijing, ChinaKey Laboratory of Wetland Ecology and Environment, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun, ChinaUniversity of Chinese Academy Sciences, Beijing, ChinaSince the 1990s, the climate in the Amur River Basin (ARB) has changed, and large-scale wetlands in the region have been reclaimed for paddy fields. The study of the influence of climate change and agricultural expansion on groundwater storage is of great significance to the evaluation of regional water resource balance and the promotion of ecological protection and agricultural development. In this work, the groundwater storage anomaly (GWSA) in the ARB and its drivers were analyzed for the period 2003–2016 using Gravity Recovery and Climate Experiment (GRACE) satellite data, a Global Land Data Assimilation System model, and in situ observations of groundwater levels. Results indicated that 1) the GWSA in the ARB increased at a rate of 2.0–2.4 mm/yr from 2003 to 2016; the GWSA in the upper reaches of the ARB increased, whereas the GWSA in the middle and lower reaches decreased during the study period. 2) The GWSA in the middle and lower reaches of the ARB was greatly influenced by temperature (Tmp) and evapotranspiration (ET). Tmp was positively correlated with GWSA, whereas ET was negatively correlated with GWSA (p < 0.05). 3) Extreme rainfall had a delayed effect on groundwater recharge. Wetland degradation and agricultural development were the main factors causing the decrease of the GWSA in the middle and lower reaches of the ARB. In summary, temperature and evapotranspiration affect groundwater storage by regulating the water–heat balance, wetland reclamation reduces the regional storage capacity, and the irrigation required for reclaimed farmland is the main source of groundwater loss.https://www.frontiersin.org/articles/10.3389/feart.2022.1037688/fullgroundwater storagegraceclimate changeAmur River Basinagricultural expansion
spellingShingle Zhengang Zhang
Zhengang Zhang
Changchun Song
Changchun Song
Yuedong Guo
Panxing He
Ning Chen
Jianzhao Liu
Jianzhao Liu
Yifei Zhang
Yifei Zhang
Yunjiang Zuo
Yunjiang Zuo
Xing Zhang
Xing Zhang
Effects of climate change and agricultural expansion on groundwater storage in the Amur River Basin
Frontiers in Earth Science
groundwater storage
grace
climate change
Amur River Basin
agricultural expansion
title Effects of climate change and agricultural expansion on groundwater storage in the Amur River Basin
title_full Effects of climate change and agricultural expansion on groundwater storage in the Amur River Basin
title_fullStr Effects of climate change and agricultural expansion on groundwater storage in the Amur River Basin
title_full_unstemmed Effects of climate change and agricultural expansion on groundwater storage in the Amur River Basin
title_short Effects of climate change and agricultural expansion on groundwater storage in the Amur River Basin
title_sort effects of climate change and agricultural expansion on groundwater storage in the amur river basin
topic groundwater storage
grace
climate change
Amur River Basin
agricultural expansion
url https://www.frontiersin.org/articles/10.3389/feart.2022.1037688/full
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