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...

Full description

Bibliographic Details
Published in:Forests
Main Authors: Peng Hu, Tijiu Cai, Fengxiang Sui, Liangliang Duan, Xiuling Man, Xueqing Cui
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2021
Subjects:
Online Access:https://doi.org/10.3390/f12081021
id ftmdpi:oai:mdpi.com:/1999-4907/12/8/1021/
record_format openpolar
spelling ftmdpi:oai:mdpi.com:/1999-4907/12/8/1021/ 2023-08-20T04:09:11+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 agris 2021-07-31 application/pdf https://doi.org/10.3390/f12081021 EN eng Multidisciplinary Digital Publishing Institute Forest Hydrology https://dx.doi.org/10.3390/f12081021 https://creativecommons.org/licenses/by/4.0/ Forests; Volume 12; Issue 8; Pages: 1021 China land use and cover change permafrost hydrology runoff SWAT model Text 2021 ftmdpi https://doi.org/10.3390/f12081021 2023-08-01T02:20:06Z 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. Text permafrost MDPI Open Access Publishing Forests 12 8 1021
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic China
land use and cover change
permafrost hydrology
runoff
SWAT model
spellingShingle China
land use and cover change
permafrost hydrology
runoff
SWAT model
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
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 Text
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 Multidisciplinary Digital Publishing Institute
publishDate 2021
url https://doi.org/10.3390/f12081021
op_coverage agris
genre permafrost
genre_facet permafrost
op_source Forests; Volume 12; Issue 8; Pages: 1021
op_relation Forest Hydrology
https://dx.doi.org/10.3390/f12081021
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/f12081021
container_title Forests
container_volume 12
container_issue 8
container_start_page 1021
_version_ 1774721976139513856