Ecological Base Flow Characteristics of Typical Rivers on the North Slope of Kunlun Mountains under Climate Change

Under climate change, river ecological base flow becomes particularly critical for the health and stability of inland river ecosystems in arid regions. Taking three typical seasonal inland rivers, including the Kriya River, the Niya River, and the Qarqan River, all on the northern slope of the Kunlu...

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Main Authors: Keke Hu, Wuerken Ailihazi, Sulitan Danierhan
Format: Article
Language:English
Published: MDPI AG 2023-05-01
Series:Atmosphere
Subjects:
Online Access:https://www.mdpi.com/2073-4433/14/5/842
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author Keke Hu
Wuerken Ailihazi
Sulitan Danierhan
author_facet Keke Hu
Wuerken Ailihazi
Sulitan Danierhan
author_sort Keke Hu
collection DOAJ
description Under climate change, river ecological base flow becomes particularly critical for the health and stability of inland river ecosystems in arid regions. Taking three typical seasonal inland rivers, including the Kriya River, the Niya River, and the Qarqan River, all on the northern slope of the Kunlun Mountains, as research objects, meteorological data from 1958 to 2019 and hydrological data from 1978 to 2014 were selected to analyze the characteristics of ecological base flow under climate change. The results show that in the past 60 years, the temperature in the Kriya River, Niya River, and Qarqan River basins has warmed at rates of 0.235 °C•(10a)<sup>−1</sup>, 0.223 °C•(10a)<sup>−1</sup>, and 0.177 °C•(10a)<sup>−1</sup>, respectively, while the precipitation has increased at the rates of 0.88 mm•(10a)<sup>−1</sup>, 3.90 mm•(10a)<sup>−1</sup>, and 7.92 mm•(10a)<sup>−1</sup>. The Tennant method was determined as the best algorithm for ecological base flow of inland rivers in arid regions. The interannual maximum values of ecological base flow all occurred in 2010, with three rivers increasing by 5.098 m<sup>3</sup>·s<sup>−1</sup>, 2.416 m<sup>3</sup>·s<sup>−1</sup>, and 11.343 m<sup>3</sup>·s<sup>−1</sup> respectively, and the regional average increasing by 6.286 m<sup>3</sup>·s<sup>−1</sup>. The maximum ecological base flow within the year is in July, and the minimum value is in January, with a high proportion of the flood season. The monthly ecological base flow of rivers has a strong correlation with the monthly temperature and precipitation, with the strongest correlation in the Qarqan River basin and the correlation coefficients of 0.876 and 0.917. We propose ecological base flow guarantee objectives for the three rivers during the dry season, and clarify that the flood season is the key point of ecological base flow guarantee. The guarantee objectives are 0.974 m<sup>3</sup>·s<sup>−1</sup>, 0.154 m<sup>3</sup>·s<sup>−1</sup>, and 2.167 m<sup>3</sup>·s<sup>−1</sup>, for the three rivers, respectively. Our research results can provide scientific reference for the management and regulation of water resources and ecological protection of the northern slope of the Kunlun Mountains.
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spelling doaj.art-c00375b115c84826a0f2819f7bc2a82f2023-11-18T00:25:38ZengMDPI AGAtmosphere2073-44332023-05-0114584210.3390/atmos14050842Ecological Base Flow Characteristics of Typical Rivers on the North Slope of Kunlun Mountains under Climate ChangeKeke Hu0Wuerken Ailihazi1Sulitan Danierhan2State Key Laboratory of Desert and Oasis Ecology (State Key Laboratory for Ecological Security and Sustainable Development in Arid Areas), Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, ChinaState Key Laboratory of Desert and Oasis Ecology (State Key Laboratory for Ecological Security and Sustainable Development in Arid Areas), Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, ChinaState Key Laboratory of Desert and Oasis Ecology (State Key Laboratory for Ecological Security and Sustainable Development in Arid Areas), Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, ChinaUnder climate change, river ecological base flow becomes particularly critical for the health and stability of inland river ecosystems in arid regions. Taking three typical seasonal inland rivers, including the Kriya River, the Niya River, and the Qarqan River, all on the northern slope of the Kunlun Mountains, as research objects, meteorological data from 1958 to 2019 and hydrological data from 1978 to 2014 were selected to analyze the characteristics of ecological base flow under climate change. The results show that in the past 60 years, the temperature in the Kriya River, Niya River, and Qarqan River basins has warmed at rates of 0.235 °C•(10a)<sup>−1</sup>, 0.223 °C•(10a)<sup>−1</sup>, and 0.177 °C•(10a)<sup>−1</sup>, respectively, while the precipitation has increased at the rates of 0.88 mm•(10a)<sup>−1</sup>, 3.90 mm•(10a)<sup>−1</sup>, and 7.92 mm•(10a)<sup>−1</sup>. The Tennant method was determined as the best algorithm for ecological base flow of inland rivers in arid regions. The interannual maximum values of ecological base flow all occurred in 2010, with three rivers increasing by 5.098 m<sup>3</sup>·s<sup>−1</sup>, 2.416 m<sup>3</sup>·s<sup>−1</sup>, and 11.343 m<sup>3</sup>·s<sup>−1</sup> respectively, and the regional average increasing by 6.286 m<sup>3</sup>·s<sup>−1</sup>. The maximum ecological base flow within the year is in July, and the minimum value is in January, with a high proportion of the flood season. The monthly ecological base flow of rivers has a strong correlation with the monthly temperature and precipitation, with the strongest correlation in the Qarqan River basin and the correlation coefficients of 0.876 and 0.917. We propose ecological base flow guarantee objectives for the three rivers during the dry season, and clarify that the flood season is the key point of ecological base flow guarantee. The guarantee objectives are 0.974 m<sup>3</sup>·s<sup>−1</sup>, 0.154 m<sup>3</sup>·s<sup>−1</sup>, and 2.167 m<sup>3</sup>·s<sup>−1</sup>, for the three rivers, respectively. Our research results can provide scientific reference for the management and regulation of water resources and ecological protection of the northern slope of the Kunlun Mountains.https://www.mdpi.com/2073-4433/14/5/842climate changenorth slope of the Kunlun Mountainecological base flowTennant methodSupport objectives
spellingShingle Keke Hu
Wuerken Ailihazi
Sulitan Danierhan
Ecological Base Flow Characteristics of Typical Rivers on the North Slope of Kunlun Mountains under Climate Change
Atmosphere
climate change
north slope of the Kunlun Mountain
ecological base flow
Tennant method
Support objectives
title Ecological Base Flow Characteristics of Typical Rivers on the North Slope of Kunlun Mountains under Climate Change
title_full Ecological Base Flow Characteristics of Typical Rivers on the North Slope of Kunlun Mountains under Climate Change
title_fullStr Ecological Base Flow Characteristics of Typical Rivers on the North Slope of Kunlun Mountains under Climate Change
title_full_unstemmed Ecological Base Flow Characteristics of Typical Rivers on the North Slope of Kunlun Mountains under Climate Change
title_short Ecological Base Flow Characteristics of Typical Rivers on the North Slope of Kunlun Mountains under Climate Change
title_sort ecological base flow characteristics of typical rivers on the north slope of kunlun mountains under climate change
topic climate change
north slope of the Kunlun Mountain
ecological base flow
Tennant method
Support objectives
url https://www.mdpi.com/2073-4433/14/5/842
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AT sulitandanierhan ecologicalbaseflowcharacteristicsoftypicalriversonthenorthslopeofkunlunmountainsunderclimatechange