Integrated Hydrologic Modelling of Groundwater-Surface Water Interactions in Cold Regions

Groundwater-surface water (GW-SW) interaction, as a key component in the cold region hydrologic cycle, is extremely sensitive to seasonal and climate change. Specifically, the dynamic change of snow cover and frozen soil bring additional challenges in observing and simulating hydrologic processes un...

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Published in:Frontiers in Earth Science
Main Authors: Yang, Xiaofan, Hu, Jinhua, Ma, Rui, Sun, Ziyong
Format: Article in Journal/Newspaper
Language:unknown
Published: Frontiers Media SA 2021
Subjects:
Online Access:http://dx.doi.org/10.3389/feart.2021.721009
https://www.frontiersin.org/articles/10.3389/feart.2021.721009/full
id crfrontiers:10.3389/feart.2021.721009
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spelling crfrontiers:10.3389/feart.2021.721009 2024-09-09T20:03:16+00:00 Integrated Hydrologic Modelling of Groundwater-Surface Water Interactions in Cold Regions Yang, Xiaofan Hu, Jinhua Ma, Rui Sun, Ziyong 2021 http://dx.doi.org/10.3389/feart.2021.721009 https://www.frontiersin.org/articles/10.3389/feart.2021.721009/full unknown Frontiers Media SA https://creativecommons.org/licenses/by/4.0/ Frontiers in Earth Science volume 9 ISSN 2296-6463 journal-article 2021 crfrontiers https://doi.org/10.3389/feart.2021.721009 2024-08-13T04:04:55Z Groundwater-surface water (GW-SW) interaction, as a key component in the cold region hydrologic cycle, is extremely sensitive to seasonal and climate change. Specifically, the dynamic change of snow cover and frozen soil bring additional challenges in observing and simulating hydrologic processes under GW-SW interactions in cold regions. Integrated hydrologic models are promising tools to simulate such complex processes and study the system behaviours as well as its responses to perturbations. The cold region integrated hydrologic models should be physically representative and fully considering the thermal-hydrologic processes under snow cover variations, freeze-thaw cycles in frozen soils and GW-SW interactions. Benchmarking and integration with scarce field observations are also critical in developing cold region integrated hydrologic models. This review summarizes the current status of hydrologic models suitable for cold environment, including distributed hydrologic models, cryo-hydrogeologic models, and fully-coupled cold region GW-SW models, with a specific focus on their concepts, numerical methods, benchmarking, and applications across scales. The current research can provide implications for cold region hydrologic model development and advance our understanding of altered environments in cold regions disturbed by climate change, such as permafrost degradation, early snow melt and water shortage. Article in Journal/Newspaper permafrost Frontiers (Publisher) Frontiers in Earth Science 9
institution Open Polar
collection Frontiers (Publisher)
op_collection_id crfrontiers
language unknown
description Groundwater-surface water (GW-SW) interaction, as a key component in the cold region hydrologic cycle, is extremely sensitive to seasonal and climate change. Specifically, the dynamic change of snow cover and frozen soil bring additional challenges in observing and simulating hydrologic processes under GW-SW interactions in cold regions. Integrated hydrologic models are promising tools to simulate such complex processes and study the system behaviours as well as its responses to perturbations. The cold region integrated hydrologic models should be physically representative and fully considering the thermal-hydrologic processes under snow cover variations, freeze-thaw cycles in frozen soils and GW-SW interactions. Benchmarking and integration with scarce field observations are also critical in developing cold region integrated hydrologic models. This review summarizes the current status of hydrologic models suitable for cold environment, including distributed hydrologic models, cryo-hydrogeologic models, and fully-coupled cold region GW-SW models, with a specific focus on their concepts, numerical methods, benchmarking, and applications across scales. The current research can provide implications for cold region hydrologic model development and advance our understanding of altered environments in cold regions disturbed by climate change, such as permafrost degradation, early snow melt and water shortage.
format Article in Journal/Newspaper
author Yang, Xiaofan
Hu, Jinhua
Ma, Rui
Sun, Ziyong
spellingShingle Yang, Xiaofan
Hu, Jinhua
Ma, Rui
Sun, Ziyong
Integrated Hydrologic Modelling of Groundwater-Surface Water Interactions in Cold Regions
author_facet Yang, Xiaofan
Hu, Jinhua
Ma, Rui
Sun, Ziyong
author_sort Yang, Xiaofan
title Integrated Hydrologic Modelling of Groundwater-Surface Water Interactions in Cold Regions
title_short Integrated Hydrologic Modelling of Groundwater-Surface Water Interactions in Cold Regions
title_full Integrated Hydrologic Modelling of Groundwater-Surface Water Interactions in Cold Regions
title_fullStr Integrated Hydrologic Modelling of Groundwater-Surface Water Interactions in Cold Regions
title_full_unstemmed Integrated Hydrologic Modelling of Groundwater-Surface Water Interactions in Cold Regions
title_sort integrated hydrologic modelling of groundwater-surface water interactions in cold regions
publisher Frontiers Media SA
publishDate 2021
url http://dx.doi.org/10.3389/feart.2021.721009
https://www.frontiersin.org/articles/10.3389/feart.2021.721009/full
genre permafrost
genre_facet permafrost
op_source Frontiers in Earth Science
volume 9
ISSN 2296-6463
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3389/feart.2021.721009
container_title Frontiers in Earth Science
container_volume 9
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