Evolution of meteorological factors during 1980–2015 in the Daqing River Basin, North China

Precipitation and temperature data, such as the homogeneity, trend, abrupt change, and periodicity, obtained at 40 meteorological stations in the Daqing River Basin from 1980 to 2015 are analyzed using the Mann–Kendall method, anomaly accumulation, Rescaled range analysis (R/S analysis) and wavelet...

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Autores principales: Yufei Jiao, Jia Liu, Chuanzhe Li, Qingtai Qiu, Xiaojiao Zhang, Fuliang Yu
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Lenguaje:EN
Publicado: IWA Publishing 2021
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Acceso en línea:https://doaj.org/article/ca8d59df346d482a9cd3f9f8dd758b37
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spelling oai:doaj.org-article:ca8d59df346d482a9cd3f9f8dd758b372021-11-09T23:59:20ZEvolution of meteorological factors during 1980–2015 in the Daqing River Basin, North China2040-22442408-935410.2166/wcc.2021.205https://doaj.org/article/ca8d59df346d482a9cd3f9f8dd758b372021-11-01T00:00:00Zhttp://jwcc.iwaponline.com/content/12/7/2977https://doaj.org/toc/2040-2244https://doaj.org/toc/2408-9354Precipitation and temperature data, such as the homogeneity, trend, abrupt change, and periodicity, obtained at 40 meteorological stations in the Daqing River Basin from 1980 to 2015 are analyzed using the Mann–Kendall method, anomaly accumulation, Rescaled range analysis (R/S analysis) and wavelet transform. The regularity of climate change is studied to provide guidelines for the rational utilization of water resources. The results show that the annual precipitation has an insignificant upward trend and suddenly changes in 2007. The precipitation evolution can be divided into three types of periodicity, that is, 22–32, 8–16, and 3–7 year time scales, where the 28 year scale is the first main period of precipitation change. The annual average temperature shows a notable upward trend, with 1992 as the change year. The annual average temperature can be divided into three types of periodicity, that is, the 25–32, 14–20, and 5–10 year time scales, where the 28 year scale is the first main period of temperature change. In conclusion, the climate of the Daqing River Basin gradually turns into humid and hot climate. The results provide valuable reference for the assessment of the effects of climate change, and the management of water resources. HIGHLIGHTS The evolution of precipitation and temperature is analyzed, including the homogeneity, trend, abrupt change, and periodicity, making use of the anomaly accumulation, Rescaled range analysis, Mann–Kendall method and wavelet transform in the Daqing River Basin, North China.; The conclusion is that the climate of the Daqing River Basin gradually turns into humid and hot.;Yufei JiaoJia LiuChuanzhe LiQingtai QiuXiaojiao ZhangFuliang YuIWA Publishingarticleabrupt changeperiodicityprecipitationtemperaturetrendsEnvironmental technology. Sanitary engineeringTD1-1066Environmental sciencesGE1-350ENJournal of Water and Climate Change, Vol 12, Iss 7, Pp 2977-2992 (2021)
institution DOAJ
collection DOAJ
language EN
topic abrupt change
periodicity
precipitation
temperature
trends
Environmental technology. Sanitary engineering
TD1-1066
Environmental sciences
GE1-350
spellingShingle abrupt change
periodicity
precipitation
temperature
trends
Environmental technology. Sanitary engineering
TD1-1066
Environmental sciences
GE1-350
Yufei Jiao
Jia Liu
Chuanzhe Li
Qingtai Qiu
Xiaojiao Zhang
Fuliang Yu
Evolution of meteorological factors during 1980–2015 in the Daqing River Basin, North China
description Precipitation and temperature data, such as the homogeneity, trend, abrupt change, and periodicity, obtained at 40 meteorological stations in the Daqing River Basin from 1980 to 2015 are analyzed using the Mann–Kendall method, anomaly accumulation, Rescaled range analysis (R/S analysis) and wavelet transform. The regularity of climate change is studied to provide guidelines for the rational utilization of water resources. The results show that the annual precipitation has an insignificant upward trend and suddenly changes in 2007. The precipitation evolution can be divided into three types of periodicity, that is, 22–32, 8–16, and 3–7 year time scales, where the 28 year scale is the first main period of precipitation change. The annual average temperature shows a notable upward trend, with 1992 as the change year. The annual average temperature can be divided into three types of periodicity, that is, the 25–32, 14–20, and 5–10 year time scales, where the 28 year scale is the first main period of temperature change. In conclusion, the climate of the Daqing River Basin gradually turns into humid and hot climate. The results provide valuable reference for the assessment of the effects of climate change, and the management of water resources. HIGHLIGHTS The evolution of precipitation and temperature is analyzed, including the homogeneity, trend, abrupt change, and periodicity, making use of the anomaly accumulation, Rescaled range analysis, Mann–Kendall method and wavelet transform in the Daqing River Basin, North China.; The conclusion is that the climate of the Daqing River Basin gradually turns into humid and hot.;
format article
author Yufei Jiao
Jia Liu
Chuanzhe Li
Qingtai Qiu
Xiaojiao Zhang
Fuliang Yu
author_facet Yufei Jiao
Jia Liu
Chuanzhe Li
Qingtai Qiu
Xiaojiao Zhang
Fuliang Yu
author_sort Yufei Jiao
title Evolution of meteorological factors during 1980–2015 in the Daqing River Basin, North China
title_short Evolution of meteorological factors during 1980–2015 in the Daqing River Basin, North China
title_full Evolution of meteorological factors during 1980–2015 in the Daqing River Basin, North China
title_fullStr Evolution of meteorological factors during 1980–2015 in the Daqing River Basin, North China
title_full_unstemmed Evolution of meteorological factors during 1980–2015 in the Daqing River Basin, North China
title_sort evolution of meteorological factors during 1980–2015 in the daqing river basin, north china
publisher IWA Publishing
publishDate 2021
url https://doaj.org/article/ca8d59df346d482a9cd3f9f8dd758b37
work_keys_str_mv AT yufeijiao evolutionofmeteorologicalfactorsduring19802015inthedaqingriverbasinnorthchina
AT jialiu evolutionofmeteorologicalfactorsduring19802015inthedaqingriverbasinnorthchina
AT chuanzheli evolutionofmeteorologicalfactorsduring19802015inthedaqingriverbasinnorthchina
AT qingtaiqiu evolutionofmeteorologicalfactorsduring19802015inthedaqingriverbasinnorthchina
AT xiaojiaozhang evolutionofmeteorologicalfactorsduring19802015inthedaqingriverbasinnorthchina
AT fuliangyu evolutionofmeteorologicalfactorsduring19802015inthedaqingriverbasinnorthchina
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