Analysis of precipitation cycles based on MEM in the Yellow River basin

Using the monthly precipitation series of 32 meteorological stations in the Yellow River basin from 1951 to 2003, the precipitation cycles were discussed using the Maximum Entropy Method (MEM), the spatial distribution of the precipitation cycles were analysed, and the possible driving factors of th...

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Main Authors: Z. Li, T. Cheng, H. Song, J. Yu
Format: Article
Language:English
Published: Copernicus Publications 2015-05-01
Series:Proceedings of the International Association of Hydrological Sciences
Online Access:https://www.proc-iahs.net/368/114/2015/piahs-368-114-2015.pdf
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spelling doaj-3d25b417405e41cd987b12d0546cb4452020-11-24T22:38:38ZengCopernicus PublicationsProceedings of the International Association of Hydrological Sciences2199-89812199-899X2015-05-0136811411910.5194/piahs-368-114-2015Analysis of precipitation cycles based on MEM in the Yellow River basinZ. Li0T. Cheng1H. Song2Z. Li3J. Yu4College of Water Sciences, Beijing Normal University, Beijing, 100875, ChinaCollege of Water Sciences, Beijing Normal University, Beijing, 100875, ChinaCollege of Water Sciences, Beijing Normal University, Beijing, 100875, ChinaSchool of Water Resources and Environment, China University of Geosciences, Beijing, 100083, ChinaCollege of Water Sciences, Beijing Normal University, Beijing, 100875, ChinaUsing the monthly precipitation series of 32 meteorological stations in the Yellow River basin from 1951 to 2003, the precipitation cycles were discussed using the Maximum Entropy Method (MEM), the spatial distribution of the precipitation cycles were analysed, and the possible driving factors of the cycles investigated. The results show that the precipitation in the Yellow River has decadal (60a), inter-decadal (25a and 14a) and inter-annual cycles (9a and 3a). The main oscillations over the whole basin are 3a and 9a. There are clearer inter-decadal variations in the riverhead area with much greater water resources, and north of the region of LanHe main stream. The decadal signals are detected in the inner area with less precipitation and Wei River basin. These differences are possibly related to some physical processes, such as the mutual action of sea and atmosphere, and solar activities.https://www.proc-iahs.net/368/114/2015/piahs-368-114-2015.pdf
collection DOAJ
language English
format Article
sources DOAJ
author Z. Li
T. Cheng
H. Song
Z. Li
J. Yu
spellingShingle Z. Li
T. Cheng
H. Song
Z. Li
J. Yu
Analysis of precipitation cycles based on MEM in the Yellow River basin
Proceedings of the International Association of Hydrological Sciences
author_facet Z. Li
T. Cheng
H. Song
Z. Li
J. Yu
author_sort Z. Li
title Analysis of precipitation cycles based on MEM in the Yellow River basin
title_short Analysis of precipitation cycles based on MEM in the Yellow River basin
title_full Analysis of precipitation cycles based on MEM in the Yellow River basin
title_fullStr Analysis of precipitation cycles based on MEM in the Yellow River basin
title_full_unstemmed Analysis of precipitation cycles based on MEM in the Yellow River basin
title_sort analysis of precipitation cycles based on mem in the yellow river basin
publisher Copernicus Publications
series Proceedings of the International Association of Hydrological Sciences
issn 2199-8981
2199-899X
publishDate 2015-05-01
description Using the monthly precipitation series of 32 meteorological stations in the Yellow River basin from 1951 to 2003, the precipitation cycles were discussed using the Maximum Entropy Method (MEM), the spatial distribution of the precipitation cycles were analysed, and the possible driving factors of the cycles investigated. The results show that the precipitation in the Yellow River has decadal (60a), inter-decadal (25a and 14a) and inter-annual cycles (9a and 3a). The main oscillations over the whole basin are 3a and 9a. There are clearer inter-decadal variations in the riverhead area with much greater water resources, and north of the region of LanHe main stream. The decadal signals are detected in the inner area with less precipitation and Wei River basin. These differences are possibly related to some physical processes, such as the mutual action of sea and atmosphere, and solar activities.
url https://www.proc-iahs.net/368/114/2015/piahs-368-114-2015.pdf
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AT zli analysisofprecipitationcyclesbasedonmemintheyellowriverbasin
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