Spatio-Temporal Variation Characteristics of Snow Depth and Snow Cover Days over the Tibetan Plateau

Changes in snow cover over the Tibetan Plateau (TP) have a significant impact on agriculture, hydrology, and ecological environment of surrounding areas. This study investigates the spatio-temporal pattern of snow depth (SD) and snow cover days (SCD), as well as the impact of temperature and precipi...

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Main Authors: Chi Zhang, Naixia Mou, Jiqiang Niu, Lingxian Zhang, Feng Liu
Format: Article
Language:English
Published: MDPI AG 2021-01-01
Series:Water
Subjects:
Online Access:https://www.mdpi.com/2073-4441/13/3/307
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spelling doaj-5edd1a84750d44cf8cce67d175966a462021-01-28T00:03:25ZengMDPI AGWater2073-44412021-01-011330730710.3390/w13030307Spatio-Temporal Variation Characteristics of Snow Depth and Snow Cover Days over the Tibetan PlateauChi Zhang0Naixia Mou1Jiqiang Niu2Lingxian Zhang3Feng Liu4College of Geodesy and Geomatics, Shandong University of Science and Technology, Qingdao 266590, ChinaCollege of Geodesy and Geomatics, Shandong University of Science and Technology, Qingdao 266590, ChinaSchool of Geographic Sciences, Xinyang Normal University, Xinyang 464099, ChinaCollege of Geodesy and Geomatics, Shandong University of Science and Technology, Qingdao 266590, ChinaCollege of Geodesy and Geomatics, Shandong University of Science and Technology, Qingdao 266590, ChinaChanges in snow cover over the Tibetan Plateau (TP) have a significant impact on agriculture, hydrology, and ecological environment of surrounding areas. This study investigates the spatio-temporal pattern of snow depth (SD) and snow cover days (SCD), as well as the impact of temperature and precipitation on snow cover over TP from 1979 to 2018 by using the ERA5 reanalysis dataset, and uses the Mann–Kendall test for significance. The results indicate that (1) the average annual SD and SCD in the southern and western edge areas of TP are relatively high, reaching 10 cm and 120 d or more, respectively. (2) In the past 40 years, SD (s = 0.04 cm decade<sup>–1</sup>, p = 0.81) and SCD (s = −2.3 d decade<sup>–1</sup>, p = 0.10) over TP did not change significantly. (3) The positive feedback effect of precipitation is the main factor affecting SD, while the negative feedback effect of temperature is the main factor affecting SCD. This study improves the understanding of snow cover change and is conducive to the further study of climate change on TP.https://www.mdpi.com/2073-4441/13/3/307climate changethe Tibetan Plateausnow depthsnow cover daysMann–Kendall test
collection DOAJ
language English
format Article
sources DOAJ
author Chi Zhang
Naixia Mou
Jiqiang Niu
Lingxian Zhang
Feng Liu
spellingShingle Chi Zhang
Naixia Mou
Jiqiang Niu
Lingxian Zhang
Feng Liu
Spatio-Temporal Variation Characteristics of Snow Depth and Snow Cover Days over the Tibetan Plateau
Water
climate change
the Tibetan Plateau
snow depth
snow cover days
Mann–Kendall test
author_facet Chi Zhang
Naixia Mou
Jiqiang Niu
Lingxian Zhang
Feng Liu
author_sort Chi Zhang
title Spatio-Temporal Variation Characteristics of Snow Depth and Snow Cover Days over the Tibetan Plateau
title_short Spatio-Temporal Variation Characteristics of Snow Depth and Snow Cover Days over the Tibetan Plateau
title_full Spatio-Temporal Variation Characteristics of Snow Depth and Snow Cover Days over the Tibetan Plateau
title_fullStr Spatio-Temporal Variation Characteristics of Snow Depth and Snow Cover Days over the Tibetan Plateau
title_full_unstemmed Spatio-Temporal Variation Characteristics of Snow Depth and Snow Cover Days over the Tibetan Plateau
title_sort spatio-temporal variation characteristics of snow depth and snow cover days over the tibetan plateau
publisher MDPI AG
series Water
issn 2073-4441
publishDate 2021-01-01
description Changes in snow cover over the Tibetan Plateau (TP) have a significant impact on agriculture, hydrology, and ecological environment of surrounding areas. This study investigates the spatio-temporal pattern of snow depth (SD) and snow cover days (SCD), as well as the impact of temperature and precipitation on snow cover over TP from 1979 to 2018 by using the ERA5 reanalysis dataset, and uses the Mann–Kendall test for significance. The results indicate that (1) the average annual SD and SCD in the southern and western edge areas of TP are relatively high, reaching 10 cm and 120 d or more, respectively. (2) In the past 40 years, SD (s = 0.04 cm decade<sup>–1</sup>, p = 0.81) and SCD (s = −2.3 d decade<sup>–1</sup>, p = 0.10) over TP did not change significantly. (3) The positive feedback effect of precipitation is the main factor affecting SD, while the negative feedback effect of temperature is the main factor affecting SCD. This study improves the understanding of snow cover change and is conducive to the further study of climate change on TP.
topic climate change
the Tibetan Plateau
snow depth
snow cover days
Mann–Kendall test
url https://www.mdpi.com/2073-4441/13/3/307
work_keys_str_mv AT chizhang spatiotemporalvariationcharacteristicsofsnowdepthandsnowcoverdaysoverthetibetanplateau
AT naixiamou spatiotemporalvariationcharacteristicsofsnowdepthandsnowcoverdaysoverthetibetanplateau
AT jiqiangniu spatiotemporalvariationcharacteristicsofsnowdepthandsnowcoverdaysoverthetibetanplateau
AT lingxianzhang spatiotemporalvariationcharacteristicsofsnowdepthandsnowcoverdaysoverthetibetanplateau
AT fengliu spatiotemporalvariationcharacteristicsofsnowdepthandsnowcoverdaysoverthetibetanplateau
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