Analysis of the Variability and Future Evolution of Snowfall Trends in the Huaihe River Basin Under Climate Change

Global warming changes the characteristics of regional climate and crop growth environments and affects human production and life in the long term. In this study, historical snowfall observation data from 199 conventional meteorological stations in the Huaihe River Basin were analyzed with the clima...

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Main Authors: Hengxin Dong, Qiangyu Li, Xiaochen Zhu, Xinyu Zhang, Zilu Zhang, Jian Shi, Yongjian He
Format: Article
Language:English
Published: Frontiers Media S.A. 2020-10-01
Series:Frontiers in Earth Science
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/feart.2020.594704/full
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spelling doaj-af0a1b6cebc44762ada46c418d2a2d0b2020-11-25T03:34:42ZengFrontiers Media S.A.Frontiers in Earth Science2296-64632020-10-01810.3389/feart.2020.594704594704Analysis of the Variability and Future Evolution of Snowfall Trends in the Huaihe River Basin Under Climate ChangeHengxin Dong0Qiangyu Li1Xiaochen Zhu2Xinyu Zhang3Zilu Zhang4Jian Shi5Yongjian He6School of Applied Meteorology, Nanjing University of Information Science and Technology, Nanjing, ChinaSchool of Applied Meteorology, Nanjing University of Information Science and Technology, Nanjing, ChinaSchool of Applied Meteorology, Nanjing University of Information Science and Technology, Nanjing, ChinaSchool of Applied Meteorology, Nanjing University of Information Science and Technology, Nanjing, ChinaSchool of Applied Meteorology, Nanjing University of Information Science and Technology, Nanjing, ChinaZhuji Meteorological Bureau, Zhuji, ChinaSchool of Geographical Sciences, Nanjing University of Information Science and Technology, Nanjing, ChinaGlobal warming changes the characteristics of regional climate and crop growth environments and affects human production and life in the long term. In this study, historical snowfall observation data from 199 conventional meteorological stations in the Huaihe River Basin were analyzed with the climate trend method, the nonparametric Mann-Kendall (M-K) test and the sliding t test to determine the variability and abrupt changes in climate trends in the Huaihe River Basin during 1951–2018. Then, the Coupled Model Intercomparison Project phase 6 datasets were used to analyze the evolutionary trend of snowfall under four climate change scenarios in 2015–2065. The results show the following: 1) Due to climate warming, both the historical data and the simulated data under different climate change scenarios show declining snowfall in the Huaihe River Basin. 2) Based on the analysis of historical data from meteorological stations, the snow events had a clear latitudinal distribution—the higher the latitude, the lower the occurrence of snow events. In contrast, as shown by the analysis results obtained under different climate change scenarios, the snow mass flux had a clear longitudinal distribution—the higher the longitude, the higher the snow mass flux. 3) In Scenario SSP370, 2050 is important because the snowfall changes from decreasing to increasing, and in 2065, the snowfall in most areas of the basin is greater than that in 2050. Furthermore, the snowfall along the southeastern coast of the basin has the greatest variability.https://www.frontiersin.org/articles/10.3389/feart.2020.594704/fullclimate warmingsnowfalltrend changeanalysis of abrupt changesclimate change scenario
collection DOAJ
language English
format Article
sources DOAJ
author Hengxin Dong
Qiangyu Li
Xiaochen Zhu
Xinyu Zhang
Zilu Zhang
Jian Shi
Yongjian He
spellingShingle Hengxin Dong
Qiangyu Li
Xiaochen Zhu
Xinyu Zhang
Zilu Zhang
Jian Shi
Yongjian He
Analysis of the Variability and Future Evolution of Snowfall Trends in the Huaihe River Basin Under Climate Change
Frontiers in Earth Science
climate warming
snowfall
trend change
analysis of abrupt changes
climate change scenario
author_facet Hengxin Dong
Qiangyu Li
Xiaochen Zhu
Xinyu Zhang
Zilu Zhang
Jian Shi
Yongjian He
author_sort Hengxin Dong
title Analysis of the Variability and Future Evolution of Snowfall Trends in the Huaihe River Basin Under Climate Change
title_short Analysis of the Variability and Future Evolution of Snowfall Trends in the Huaihe River Basin Under Climate Change
title_full Analysis of the Variability and Future Evolution of Snowfall Trends in the Huaihe River Basin Under Climate Change
title_fullStr Analysis of the Variability and Future Evolution of Snowfall Trends in the Huaihe River Basin Under Climate Change
title_full_unstemmed Analysis of the Variability and Future Evolution of Snowfall Trends in the Huaihe River Basin Under Climate Change
title_sort analysis of the variability and future evolution of snowfall trends in the huaihe river basin under climate change
publisher Frontiers Media S.A.
series Frontiers in Earth Science
issn 2296-6463
publishDate 2020-10-01
description Global warming changes the characteristics of regional climate and crop growth environments and affects human production and life in the long term. In this study, historical snowfall observation data from 199 conventional meteorological stations in the Huaihe River Basin were analyzed with the climate trend method, the nonparametric Mann-Kendall (M-K) test and the sliding t test to determine the variability and abrupt changes in climate trends in the Huaihe River Basin during 1951–2018. Then, the Coupled Model Intercomparison Project phase 6 datasets were used to analyze the evolutionary trend of snowfall under four climate change scenarios in 2015–2065. The results show the following: 1) Due to climate warming, both the historical data and the simulated data under different climate change scenarios show declining snowfall in the Huaihe River Basin. 2) Based on the analysis of historical data from meteorological stations, the snow events had a clear latitudinal distribution—the higher the latitude, the lower the occurrence of snow events. In contrast, as shown by the analysis results obtained under different climate change scenarios, the snow mass flux had a clear longitudinal distribution—the higher the longitude, the higher the snow mass flux. 3) In Scenario SSP370, 2050 is important because the snowfall changes from decreasing to increasing, and in 2065, the snowfall in most areas of the basin is greater than that in 2050. Furthermore, the snowfall along the southeastern coast of the basin has the greatest variability.
topic climate warming
snowfall
trend change
analysis of abrupt changes
climate change scenario
url https://www.frontiersin.org/articles/10.3389/feart.2020.594704/full
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