Response of Runoff to Extreme Land Use Change in the Permafrost Region of Northeastern China

To study the response of runoff to extreme changes in land use, the Soil and Water Assessment Tool (SWAT) model was used to construct historical, extreme, and future scenarios for several major landscape types in a permafrost region of northeastern China. The results show that the SWAT model is appl...

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Published in:Forests
Main Authors: Peng Hu, Tijiu Cai, Fengxiang Sui, Liangliang Duan, Xiuling Man, Xueqing Cui
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2021
Subjects:
Online Access:https://doi.org/10.3390/f12081021
https://doaj.org/article/ad4113ef94b84b0e8f9f63fa436418ca
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spelling ftdoajarticles:oai:doaj.org/article:ad4113ef94b84b0e8f9f63fa436418ca 2023-05-15T17:56:59+02:00 Response of Runoff to Extreme Land Use Change in the Permafrost Region of Northeastern China Peng Hu Tijiu Cai Fengxiang Sui Liangliang Duan Xiuling Man Xueqing Cui 2021-07-01T00:00:00Z https://doi.org/10.3390/f12081021 https://doaj.org/article/ad4113ef94b84b0e8f9f63fa436418ca EN eng MDPI AG https://www.mdpi.com/1999-4907/12/8/1021 https://doaj.org/toc/1999-4907 doi:10.3390/f12081021 1999-4907 https://doaj.org/article/ad4113ef94b84b0e8f9f63fa436418ca Forests, Vol 12, Iss 1021, p 1021 (2021) China land use and cover change permafrost hydrology runoff SWAT model Plant ecology QK900-989 article 2021 ftdoajarticles https://doi.org/10.3390/f12081021 2022-12-31T04:31:09Z To study the response of runoff to extreme changes in land use, the Soil and Water Assessment Tool (SWAT) model was used to construct historical, extreme, and future scenarios for several major landscape types in a permafrost region of northeastern China. The results show that the SWAT model is applicable in the Tahe River Basin; forestlands, shrublands, wetlands, and grasslands are the main land-use types in this basin, and the transfers among them from 1980–2015 have impacted runoff by less than 5%. Under extreme land use-change scenarios, the simulated runoff decreased from grasslands, to wetlands, shrublands, and finally, forestlands. The conversion of extreme land-use scenarios produces different hydrological effects. When forestland is converted to grassland, runoff increases by 25.32%, when forestland is converted to wetland, runoff increases by 13.34%, and the conversion of shrubland to forestland reduces runoff by 13.25%. In addition, the sensitivity of runoff to different land-use changes was much greater during flood seasons than in dry seasons. Compared to the reference year of 2015, the annual simulated runoff under the two future land-use scenarios (shrublands to forestlands and shrublands to wetland) was less. Also, both future land-use scenarios showed effects to decrease flooding and increased dryness, This study provided important insight into the integrated management of land use and water resources in the Tahe River Basin and the permafrost region of northeastern China. Article in Journal/Newspaper permafrost Directory of Open Access Journals: DOAJ Articles Forests 12 8 1021
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic China
land use and cover change
permafrost hydrology
runoff
SWAT model
Plant ecology
QK900-989
spellingShingle China
land use and cover change
permafrost hydrology
runoff
SWAT model
Plant ecology
QK900-989
Peng Hu
Tijiu Cai
Fengxiang Sui
Liangliang Duan
Xiuling Man
Xueqing Cui
Response of Runoff to Extreme Land Use Change in the Permafrost Region of Northeastern China
topic_facet China
land use and cover change
permafrost hydrology
runoff
SWAT model
Plant ecology
QK900-989
description To study the response of runoff to extreme changes in land use, the Soil and Water Assessment Tool (SWAT) model was used to construct historical, extreme, and future scenarios for several major landscape types in a permafrost region of northeastern China. The results show that the SWAT model is applicable in the Tahe River Basin; forestlands, shrublands, wetlands, and grasslands are the main land-use types in this basin, and the transfers among them from 1980–2015 have impacted runoff by less than 5%. Under extreme land use-change scenarios, the simulated runoff decreased from grasslands, to wetlands, shrublands, and finally, forestlands. The conversion of extreme land-use scenarios produces different hydrological effects. When forestland is converted to grassland, runoff increases by 25.32%, when forestland is converted to wetland, runoff increases by 13.34%, and the conversion of shrubland to forestland reduces runoff by 13.25%. In addition, the sensitivity of runoff to different land-use changes was much greater during flood seasons than in dry seasons. Compared to the reference year of 2015, the annual simulated runoff under the two future land-use scenarios (shrublands to forestlands and shrublands to wetland) was less. Also, both future land-use scenarios showed effects to decrease flooding and increased dryness, This study provided important insight into the integrated management of land use and water resources in the Tahe River Basin and the permafrost region of northeastern China.
format Article in Journal/Newspaper
author Peng Hu
Tijiu Cai
Fengxiang Sui
Liangliang Duan
Xiuling Man
Xueqing Cui
author_facet Peng Hu
Tijiu Cai
Fengxiang Sui
Liangliang Duan
Xiuling Man
Xueqing Cui
author_sort Peng Hu
title Response of Runoff to Extreme Land Use Change in the Permafrost Region of Northeastern China
title_short Response of Runoff to Extreme Land Use Change in the Permafrost Region of Northeastern China
title_full Response of Runoff to Extreme Land Use Change in the Permafrost Region of Northeastern China
title_fullStr Response of Runoff to Extreme Land Use Change in the Permafrost Region of Northeastern China
title_full_unstemmed Response of Runoff to Extreme Land Use Change in the Permafrost Region of Northeastern China
title_sort response of runoff to extreme land use change in the permafrost region of northeastern china
publisher MDPI AG
publishDate 2021
url https://doi.org/10.3390/f12081021
https://doaj.org/article/ad4113ef94b84b0e8f9f63fa436418ca
genre permafrost
genre_facet permafrost
op_source Forests, Vol 12, Iss 1021, p 1021 (2021)
op_relation https://www.mdpi.com/1999-4907/12/8/1021
https://doaj.org/toc/1999-4907
doi:10.3390/f12081021
1999-4907
https://doaj.org/article/ad4113ef94b84b0e8f9f63fa436418ca
op_doi https://doi.org/10.3390/f12081021
container_title Forests
container_volume 12
container_issue 8
container_start_page 1021
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