Impacts of climate change on water resources in the Huaihe River Basin

The Huaihe river basin, located in the transitional area of the humid zone to the semi arid zone, is a subtropical monsoon zone. By analysis of historical observation data, the annual average surface temperature increased by 0.5℃ over the past 50 years. However, the precipitation showed a fluctuatio...

Full description

Bibliographic Details
Main Authors: kai Wang, mingkai Qian, shijing Xu, shuxian Liang, hongyu Chen, youbin Hu, cui Su, mengjie Zhao, wenjie Li, jingteng Wang
Format: Article
Language:English
Published: EDP Sciences 2018-01-01
Series:MATEC Web of Conferences
Online Access:https://doi.org/10.1051/matecconf/201824601090
id doaj-f5c9bf2c5e594e27a006f73d2eeaa47b
record_format Article
spelling doaj-f5c9bf2c5e594e27a006f73d2eeaa47b2021-03-02T11:10:49ZengEDP SciencesMATEC Web of Conferences2261-236X2018-01-012460109010.1051/matecconf/201824601090matecconf_iswso2018_01090Impacts of climate change on water resources in the Huaihe River Basinkai Wangmingkai Qianshijing Xushuxian Lianghongyu Chenyoubin Hucui Sumengjie Zhaowenjie Lijingteng WangThe Huaihe river basin, located in the transitional area of the humid zone to the semi arid zone, is a subtropical monsoon zone. By analysis of historical observation data, the annual average surface temperature increased by 0.5℃ over the past 50 years. However, the precipitation showed a fluctuation trend. Based on the hydrological and meteorological data of Huaihe River Basin, this paper studies impacts of climate change on water resources in Huaihe basin by using the Xinanjiang monthly hydrological model in conjunction with prediction products of NCAR climate model. The results show that the precipitation in the basin had a fluctuating upward trend under RCP8.5 and RCP4.5 scenarios, and the increase or decrease trend of precipitation in RCP2.6 scenario is not significant. The model predicted that the temperature of the river basin in the 3 scenarios shows significant rising trend from year 2001 to 2100. However, the annual runoff of the Huaihe River Basin shows an increasing trend but not significant from year 2001 to 2100.https://doi.org/10.1051/matecconf/201824601090
collection DOAJ
language English
format Article
sources DOAJ
author kai Wang
mingkai Qian
shijing Xu
shuxian Liang
hongyu Chen
youbin Hu
cui Su
mengjie Zhao
wenjie Li
jingteng Wang
spellingShingle kai Wang
mingkai Qian
shijing Xu
shuxian Liang
hongyu Chen
youbin Hu
cui Su
mengjie Zhao
wenjie Li
jingteng Wang
Impacts of climate change on water resources in the Huaihe River Basin
MATEC Web of Conferences
author_facet kai Wang
mingkai Qian
shijing Xu
shuxian Liang
hongyu Chen
youbin Hu
cui Su
mengjie Zhao
wenjie Li
jingteng Wang
author_sort kai Wang
title Impacts of climate change on water resources in the Huaihe River Basin
title_short Impacts of climate change on water resources in the Huaihe River Basin
title_full Impacts of climate change on water resources in the Huaihe River Basin
title_fullStr Impacts of climate change on water resources in the Huaihe River Basin
title_full_unstemmed Impacts of climate change on water resources in the Huaihe River Basin
title_sort impacts of climate change on water resources in the huaihe river basin
publisher EDP Sciences
series MATEC Web of Conferences
issn 2261-236X
publishDate 2018-01-01
description The Huaihe river basin, located in the transitional area of the humid zone to the semi arid zone, is a subtropical monsoon zone. By analysis of historical observation data, the annual average surface temperature increased by 0.5℃ over the past 50 years. However, the precipitation showed a fluctuation trend. Based on the hydrological and meteorological data of Huaihe River Basin, this paper studies impacts of climate change on water resources in Huaihe basin by using the Xinanjiang monthly hydrological model in conjunction with prediction products of NCAR climate model. The results show that the precipitation in the basin had a fluctuating upward trend under RCP8.5 and RCP4.5 scenarios, and the increase or decrease trend of precipitation in RCP2.6 scenario is not significant. The model predicted that the temperature of the river basin in the 3 scenarios shows significant rising trend from year 2001 to 2100. However, the annual runoff of the Huaihe River Basin shows an increasing trend but not significant from year 2001 to 2100.
url https://doi.org/10.1051/matecconf/201824601090
work_keys_str_mv AT kaiwang impactsofclimatechangeonwaterresourcesinthehuaiheriverbasin
AT mingkaiqian impactsofclimatechangeonwaterresourcesinthehuaiheriverbasin
AT shijingxu impactsofclimatechangeonwaterresourcesinthehuaiheriverbasin
AT shuxianliang impactsofclimatechangeonwaterresourcesinthehuaiheriverbasin
AT hongyuchen impactsofclimatechangeonwaterresourcesinthehuaiheriverbasin
AT youbinhu impactsofclimatechangeonwaterresourcesinthehuaiheriverbasin
AT cuisu impactsofclimatechangeonwaterresourcesinthehuaiheriverbasin
AT mengjiezhao impactsofclimatechangeonwaterresourcesinthehuaiheriverbasin
AT wenjieli impactsofclimatechangeonwaterresourcesinthehuaiheriverbasin
AT jingtengwang impactsofclimatechangeonwaterresourcesinthehuaiheriverbasin
_version_ 1724235275193810944