Decrease in snowfall/rainfall ratio in the Tibetan Plateau from 1961 to 2013

On the basis of two gridded datasets of daily precipitation and temperature with a spatial resolution of 0.5°×0.5°, and meteorological station data released by the National Meteorological Information Center (NMIC) during 1961-2013, the spatial and temporal variations of total amount of precipitation...

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Published inJournal of geographical sciences Vol. 26; no. 9; pp. 1277 - 1288
Main Authors Wang, Jie, Zhang, Mingjun, Wang, Shengjie, Ren, Zhengguo, Che, Yanjun, Qiang, Fang, Qu, Deye
Format Journal Article
LanguageEnglish
Published Heidelberg Science Press 01.09.2016
Springer Nature B.V
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Abstract On the basis of two gridded datasets of daily precipitation and temperature with a spatial resolution of 0.5°×0.5°, and meteorological station data released by the National Meteorological Information Center (NMIC) during 1961-2013, the spatial and temporal variations of total amount of precipitation, amount of rainfall, amount of snowfall and snowfall/rainfall ratio (S/R) in the Tibetan Plateau (TP) are analyzed using Sen's slope, the Mann-Kendall mutation test, Inverse Distance Weighting (IDW) and the Morlet wavelet. Total amount of precipitation and amount of rainfall generally show statistically significant increasing trends of 0.6 mm·a^-1 and 1.3 mm·a^-1, respectively, while amount of snowfall and SIR have significant decreasing trends of-0.6 mm·a^-1 and -0.5% a^-1, respectively. In most regions, due to significant increasing trends in total amount of precipitation and amount of rainfall, and significant decreasing trends in amount of snowfall, SIR shows a decreasing trend in the TP. Abrupt changes in total amount of precipitation, amount of rainfall, amount of snowfall and S/R are detected for 2005, 2004, 1996 and 1998, respectively. Total amount of precipitation, amount of rainfall, amount of snowfall and SIR are concentrated in cycles of approximately 5 years, 10 years, 16 years and 20 years, respectively. The trend magnitudes for total amount of precipitation and amount of rainfall all show decreasing-to-increasing trends with elevation, while amount of snowfall and SIR show decreasing trends.
AbstractList On the basis of two gridded datasets of daily precipitation and temperature with a spatial resolution of 0.5°×0.5°, and meteorological station data released by the National Meteorological Information Center (NMIC) during 1961–2013, the spatial and temporal variations of total amount of precipitation, amount of rainfall, amount of snowfall and snowfall/rainfall ratio (S/R) in the Tibetan Plateau (TP) are analyzed using Sen’s slope, the Mann–Kendall mutation test, Inverse Distance Weighting (IDW) and the Morlet wavelet. Total amount of precipitation and amount of rainfall generally show statistically significant increasing trends of 0.6 mm·a–1 and 1.3 mm·a–1, respectively, while amount of snowfall and S/R have significant decreasing trends of–0.6 mm·a–1 and–0.5% a–1, respectively. In most regions, due to significant increasing trends in total amount of precipitation and amount of rainfall, and significant decreasing trends in amount of snowfall, S/R shows a decreasing trend in the TP. Abrupt changes in total amount of precipitation, amount of rainfall, amount of snowfall and S/R are detected for 2005, 2004, 1996 and 1998, respectively. Total amount of precipitation, amount of rainfall, amount of snowfall and S/R are concentrated in cycles of approximately 5 years, 10 years, 16 years and 20 years, respectively. The trend magnitudes for total amount of precipitation and amount of rainfall all show decreasing-to-increasing trends with elevation, while amount of snowfall and S/R show decreasing trends.
On the basis of two gridded datasets of daily precipitation and temperature with a spatial resolution of 0.5 degree 0.5 degree , and meteorological station data released by the National Meteorological Information Center (NMIC) during 1961-2013, the spatial and temporal variations of total amount of precipitation, amount of rainfall, amount of snowfall and snowfall/rainfall ratio (S/R) in the Tibetan Plateau (TP) are analyzed using Sen's slope, the Mann-Kendall mutation test, Inverse Distance Weighting (IDW) and the Morlet wavelet. Total amount of precipitation and amount of rainfall generally show statistically significant increasing trends of 0.6 mm.a super(-1) and 1.3 mm.a super(-1), respectively, while amount of snowfall and S/R have significant decreasing trends of-0.6 mm.a super(-1) and-0.5% a super(-1), respectively. In most regions, due to significant increasing trends in total amount of precipitation and amount of rainfall, and significant decreasing trends in amount of snowfall, S/R shows a decreasing trend in the TP. Abrupt changes in total amount of precipitation, amount of rainfall, amount of snowfall and S/R are detected for 2005, 2004, 1996 and 1998, respectively. Total amount of precipitation, amount of rainfall, amount of snowfall and S/R are concentrated in cycles of approximately 5 years, 10 years, 16 years and 20 years, respectively. The trend magnitudes for total amount of precipitation and amount of rainfall all show decreasing-to-increasing trends with elevation, while amount of snowfall and S/R show decreasing trends.
On the basis of two gridded datasets of daily precipitation and temperature with a spatial resolution of 0.5°×0.5°, and meteorological station data released by the National Meteorological Information Center (NMIC) during 1961-2013, the spatial and temporal variations of total amount of precipitation, amount of rainfall, amount of snowfall and snowfall/rainfall ratio (S/R) in the Tibetan Plateau (TP) are analyzed using Sen's slope, the Mann-Kendall mutation test, Inverse Distance Weighting (IDW) and the Morlet wavelet. Total amount of precipitation and amount of rainfall generally show statistically significant increasing trends of 0.6 mm·a^-1 and 1.3 mm·a^-1, respectively, while amount of snowfall and SIR have significant decreasing trends of-0.6 mm·a^-1 and -0.5% a^-1, respectively. In most regions, due to significant increasing trends in total amount of precipitation and amount of rainfall, and significant decreasing trends in amount of snowfall, SIR shows a decreasing trend in the TP. Abrupt changes in total amount of precipitation, amount of rainfall, amount of snowfall and S/R are detected for 2005, 2004, 1996 and 1998, respectively. Total amount of precipitation, amount of rainfall, amount of snowfall and SIR are concentrated in cycles of approximately 5 years, 10 years, 16 years and 20 years, respectively. The trend magnitudes for total amount of precipitation and amount of rainfall all show decreasing-to-increasing trends with elevation, while amount of snowfall and SIR show decreasing trends.
On the basis of two gridded datasets of daily precipitation and temperature with a spatial resolution of 0.5°×0.5°, and meteorological station data released by the National Meteorological Information Center (NMIC) during 1961–2013, the spatial and temporal variations of total amount of precipitation, amount of rainfall, amount of snowfall and snowfall/rainfall ratio (S/R) in the Tibetan Plateau (TP) are analyzed using Sen’s slope, the Mann–Kendall mutation test, Inverse Distance Weighting (IDW) and the Morlet wavelet. Total amount of precipitation and amount of rainfall generally show statistically significant increasing trends of 0.6 mm·a –1 and 1.3 mm·a –1 , respectively, while amount of snowfall and S/R have significant decreasing trends of–0.6 mm·a –1 and–0.5% a –1 , respectively. In most regions, due to significant increasing trends in total amount of precipitation and amount of rainfall, and significant decreasing trends in amount of snowfall, S/R shows a decreasing trend in the TP. Abrupt changes in total amount of precipitation, amount of rainfall, amount of snowfall and S/R are detected for 2005, 2004, 1996 and 1998, respectively. Total amount of precipitation, amount of rainfall, amount of snowfall and S/R are concentrated in cycles of approximately 5 years, 10 years, 16 years and 20 years, respectively. The trend magnitudes for total amount of precipitation and amount of rainfall all show decreasing-to-increasing trends with elevation, while amount of snowfall and S/R show decreasing trends.
Author WANG Jie ZHANG Mingjun WANG Shengjie REN Zhengguo CHE Yanjun QIANG Fang QU Deye
AuthorAffiliation College of Geography and Environmental Science, Northwest Normal University, Lanzhou 730070, China
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Keywords gridded data
snowfall/rainfall ratio
Tibetan Plateau
precipitation
Language English
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Notes On the basis of two gridded datasets of daily precipitation and temperature with a spatial resolution of 0.5°×0.5°, and meteorological station data released by the National Meteorological Information Center (NMIC) during 1961-2013, the spatial and temporal variations of total amount of precipitation, amount of rainfall, amount of snowfall and snowfall/rainfall ratio (S/R) in the Tibetan Plateau (TP) are analyzed using Sen's slope, the Mann-Kendall mutation test, Inverse Distance Weighting (IDW) and the Morlet wavelet. Total amount of precipitation and amount of rainfall generally show statistically significant increasing trends of 0.6 mm·a^-1 and 1.3 mm·a^-1, respectively, while amount of snowfall and SIR have significant decreasing trends of-0.6 mm·a^-1 and -0.5% a^-1, respectively. In most regions, due to significant increasing trends in total amount of precipitation and amount of rainfall, and significant decreasing trends in amount of snowfall, SIR shows a decreasing trend in the TP. Abrupt changes in total amount of precipitation, amount of rainfall, amount of snowfall and S/R are detected for 2005, 2004, 1996 and 1998, respectively. Total amount of precipitation, amount of rainfall, amount of snowfall and SIR are concentrated in cycles of approximately 5 years, 10 years, 16 years and 20 years, respectively. The trend magnitudes for total amount of precipitation and amount of rainfall all show decreasing-to-increasing trends with elevation, while amount of snowfall and SIR show decreasing trends.
Tibetan Plateau; gridded data; snowfall/rainfaU ratio; precipitation
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PublicationTitle Journal of geographical sciences
PublicationTitleAbbrev J. Geogr. Sci
PublicationTitleAlternate Journal of Geographical Sciences
PublicationYear 2016
Publisher Science Press
Springer Nature B.V
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SSID ssj0039462
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Snippet On the basis of two gridded datasets of daily precipitation and temperature with a spatial resolution of 0.5°×0.5°, and meteorological station data released by...
On the basis of two gridded datasets of daily precipitation and temperature with a spatial resolution of 0.5 degree 0.5 degree , and meteorological station...
SourceID proquest
crossref
springer
chongqing
SourceType Aggregation Database
Publisher
StartPage 1277
SubjectTerms Earth and Environmental Science
Geographical Information Systems/Cartography
Geography
Nature Conservation
Physical Geography
Precipitation
Rainfall
Remote Sensing/Photogrammetry
Snow
Trends
比率
气象信息中心
空间分辨率
西藏高原
降水总量
降水量
降雨量
降雪量
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Title Decrease in snowfall/rainfall ratio in the Tibetan Plateau from 1961 to 2013
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https://link.springer.com/article/10.1007/s11442-016-1326-8
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https://search.proquest.com/docview/1868340855
Volume 26
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