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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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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