The Trend and Influencing Factors of Potential Evapotranspiration in the Yellow River

Based on the Penman-Monteith formula recommended by the World Food and Agriculture Organization (FAO) and the Mann-Kendall trend test method, the variation trend of potential evapotranspiration in the Yellow River Basin from 1952 to 2014 is analyzed. The results showed that the potential evapotransp...

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Main Authors: Dai Yanyu, Lu Fan, Zhu Kui, Song Xinyi, Xu Yiran
Format: Article
Language:English
Published: EDP Sciences 2018-01-01
Series:MATEC Web of Conferences
Online Access:https://doi.org/10.1051/matecconf/201824601020
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spelling doaj-782c1f3d91e9423fbddf5090166cd64b2021-02-02T04:09:54ZengEDP SciencesMATEC Web of Conferences2261-236X2018-01-012460102010.1051/matecconf/201824601020matecconf_iswso2018_01020The Trend and Influencing Factors of Potential Evapotranspiration in the Yellow RiverDai YanyuLu Fan0Zhu Kui1Song Xinyi2Xu YiranWater Resources Institute, China Institute of Water Resources and Hydropower ResearchSchool of Resources and Geosciences, China University of Mining and TechnologyWater Resources Institute, China Institute of Water Resources and Hydropower ResearchBased on the Penman-Monteith formula recommended by the World Food and Agriculture Organization (FAO) and the Mann-Kendall trend test method, the variation trend of potential evapotranspiration in the Yellow River Basin from 1952 to 2014 is analyzed. The results showed that the potential evapotranspiration of 43.3% of the 90 meteorological stations in the Yellow River Basin showed a significant upward trend. 30% of the stations showed a significant downward trend, and 26.7% of the stations had no obvious trend of change. In all the secondary areas of water resources, the stations above Longyangxia are basically marked upward. The Longyangxia to the northern part of Lanzhou, the Longmen to the east of Sanmenxia and the Sanmenxia to Huayuankou are all significant descending sites. The change trend of the sites below the Huayuankou is not obvious. In other partition three kinds of sites are distributed. Through the correlation analysis, it is found that the increase of temperature has a great influence on the stations where the potential evapotranspiration is significantly increased, and the decrease of wind speed is the main reason for the significant decrease of potential evapotranspiration in some stations.https://doi.org/10.1051/matecconf/201824601020
collection DOAJ
language English
format Article
sources DOAJ
author Dai Yanyu
Lu Fan
Zhu Kui
Song Xinyi
Xu Yiran
spellingShingle Dai Yanyu
Lu Fan
Zhu Kui
Song Xinyi
Xu Yiran
The Trend and Influencing Factors of Potential Evapotranspiration in the Yellow River
MATEC Web of Conferences
author_facet Dai Yanyu
Lu Fan
Zhu Kui
Song Xinyi
Xu Yiran
author_sort Dai Yanyu
title The Trend and Influencing Factors of Potential Evapotranspiration in the Yellow River
title_short The Trend and Influencing Factors of Potential Evapotranspiration in the Yellow River
title_full The Trend and Influencing Factors of Potential Evapotranspiration in the Yellow River
title_fullStr The Trend and Influencing Factors of Potential Evapotranspiration in the Yellow River
title_full_unstemmed The Trend and Influencing Factors of Potential Evapotranspiration in the Yellow River
title_sort trend and influencing factors of potential evapotranspiration in the yellow river
publisher EDP Sciences
series MATEC Web of Conferences
issn 2261-236X
publishDate 2018-01-01
description Based on the Penman-Monteith formula recommended by the World Food and Agriculture Organization (FAO) and the Mann-Kendall trend test method, the variation trend of potential evapotranspiration in the Yellow River Basin from 1952 to 2014 is analyzed. The results showed that the potential evapotranspiration of 43.3% of the 90 meteorological stations in the Yellow River Basin showed a significant upward trend. 30% of the stations showed a significant downward trend, and 26.7% of the stations had no obvious trend of change. In all the secondary areas of water resources, the stations above Longyangxia are basically marked upward. The Longyangxia to the northern part of Lanzhou, the Longmen to the east of Sanmenxia and the Sanmenxia to Huayuankou are all significant descending sites. The change trend of the sites below the Huayuankou is not obvious. In other partition three kinds of sites are distributed. Through the correlation analysis, it is found that the increase of temperature has a great influence on the stations where the potential evapotranspiration is significantly increased, and the decrease of wind speed is the main reason for the significant decrease of potential evapotranspiration in some stations.
url https://doi.org/10.1051/matecconf/201824601020
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