Trends of Hydroclimate Variables in the Upper Huai River Basin: Implications of Managing Water Resource for Climate Change Mitigation

The present study attempted to investigate the trends of mean annual temperature, precipitation, and streamflow changes to determine their relationships in the upper Huai river basin. The Mann–Kendall (MK), Sen’s slope test estimator, and innovative trend detection (ф) (ITA) methods were used to det...

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Main Authors: Abel Girma, Denghua Yan, Hao Wang, Xinshan Song, Tianlin Qin, Batsuren Dorjsuren, Mohammed Gedefaw, Asaminew Abiyu, Dagim Fikir, Jianwei Wang, Otgonbayar Yadamjav
Format: Article
Language:English
Published: Wiley 2020-01-01
Series:Advances in Meteorology
Online Access:http://dx.doi.org/10.1155/2020/8817068
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author Abel Girma
Denghua Yan
Hao Wang
Xinshan Song
Tianlin Qin
Batsuren Dorjsuren
Mohammed Gedefaw
Asaminew Abiyu
Dagim Fikir
Jianwei Wang
Otgonbayar Yadamjav
author_facet Abel Girma
Denghua Yan
Hao Wang
Xinshan Song
Tianlin Qin
Batsuren Dorjsuren
Mohammed Gedefaw
Asaminew Abiyu
Dagim Fikir
Jianwei Wang
Otgonbayar Yadamjav
author_sort Abel Girma
collection DOAJ
description The present study attempted to investigate the trends of mean annual temperature, precipitation, and streamflow changes to determine their relationships in the upper Huai river basin. The Mann–Kendall (MK), Sen’s slope test estimator, and innovative trend detection (ф) (ITA) methods were used to detect the trends. According to the findings, average annual precipitation shows a descending trend (ф = −0.17) in most stations. An increasing trend was found only in Fuyang station (ф = 1.02). In all stations, the trends of mean annual temperature (ф = 0.36) were abruptly increased. During the past 57 years, the mean air temperature has considerably increased by 12°C/10a. The river streamflow showed a dramatic declining trend in all stations for the duration of the study period (1960–2016) (ф = −4.29). The climate variability in the study region affects the quantity of the streamflow. The river streamflow exhibits decreasing trends from 1965 onwards. The main possible reason for the declining stream flow in the study area is the declining amount of precipitation on some specific months due to the occurrence of climate change. The outcomes of this study could create awareness for the policymakers and members of the scientific community, informing them about the hydroclimatic evolutions across the study basin, and become an inordinate resource for advanced scientific research.
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id doaj-art-2afed38bc33446fabf2790cb99b3189d
institution Kabale University
issn 1687-9309
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language English
publishDate 2020-01-01
publisher Wiley
record_format Article
series Advances in Meteorology
spelling doaj-art-2afed38bc33446fabf2790cb99b3189d2025-02-03T01:27:57ZengWileyAdvances in Meteorology1687-93091687-93172020-01-01202010.1155/2020/88170688817068Trends of Hydroclimate Variables in the Upper Huai River Basin: Implications of Managing Water Resource for Climate Change MitigationAbel Girma0Denghua Yan1Hao Wang2Xinshan Song3Tianlin Qin4Batsuren Dorjsuren5Mohammed Gedefaw6Asaminew Abiyu7Dagim Fikir8Jianwei Wang9Otgonbayar Yadamjav10College of Environmental Science and Engineering, Donghua University, Shanghai, ChinaCollege of Environmental Science and Engineering, Donghua University, Shanghai, ChinaCollege of Environmental Science and Engineering, Donghua University, Shanghai, ChinaCollege of Environmental Science and Engineering, Donghua University, Shanghai, ChinaState Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, Beijing, ChinaCollege of Environmental Science and Engineering, Donghua University, Shanghai, ChinaCollege of Environmental Science and Engineering, Donghua University, Shanghai, ChinaCollege of Environmental Science and Engineering, Donghua University, Shanghai, ChinaState Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, Beijing, ChinaState Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, Beijing, ChinaDepartment of Sociology and Social Work, School of Art and Sciences, National University of Mongolia, Ulaanbaatar 210646, MongoliaThe present study attempted to investigate the trends of mean annual temperature, precipitation, and streamflow changes to determine their relationships in the upper Huai river basin. The Mann–Kendall (MK), Sen’s slope test estimator, and innovative trend detection (ф) (ITA) methods were used to detect the trends. According to the findings, average annual precipitation shows a descending trend (ф = −0.17) in most stations. An increasing trend was found only in Fuyang station (ф = 1.02). In all stations, the trends of mean annual temperature (ф = 0.36) were abruptly increased. During the past 57 years, the mean air temperature has considerably increased by 12°C/10a. The river streamflow showed a dramatic declining trend in all stations for the duration of the study period (1960–2016) (ф = −4.29). The climate variability in the study region affects the quantity of the streamflow. The river streamflow exhibits decreasing trends from 1965 onwards. The main possible reason for the declining stream flow in the study area is the declining amount of precipitation on some specific months due to the occurrence of climate change. The outcomes of this study could create awareness for the policymakers and members of the scientific community, informing them about the hydroclimatic evolutions across the study basin, and become an inordinate resource for advanced scientific research.http://dx.doi.org/10.1155/2020/8817068
spellingShingle Abel Girma
Denghua Yan
Hao Wang
Xinshan Song
Tianlin Qin
Batsuren Dorjsuren
Mohammed Gedefaw
Asaminew Abiyu
Dagim Fikir
Jianwei Wang
Otgonbayar Yadamjav
Trends of Hydroclimate Variables in the Upper Huai River Basin: Implications of Managing Water Resource for Climate Change Mitigation
Advances in Meteorology
title Trends of Hydroclimate Variables in the Upper Huai River Basin: Implications of Managing Water Resource for Climate Change Mitigation
title_full Trends of Hydroclimate Variables in the Upper Huai River Basin: Implications of Managing Water Resource for Climate Change Mitigation
title_fullStr Trends of Hydroclimate Variables in the Upper Huai River Basin: Implications of Managing Water Resource for Climate Change Mitigation
title_full_unstemmed Trends of Hydroclimate Variables in the Upper Huai River Basin: Implications of Managing Water Resource for Climate Change Mitigation
title_short Trends of Hydroclimate Variables in the Upper Huai River Basin: Implications of Managing Water Resource for Climate Change Mitigation
title_sort trends of hydroclimate variables in the upper huai river basin implications of managing water resource for climate change mitigation
url http://dx.doi.org/10.1155/2020/8817068
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