Research on Historical and Future Spatial-Temporal Variability of Precipitation in China

Based on observed data and data simulated by climate models, temporal variation and spatial distribution of precipitation in China from 1961 to 2050 were investigated. The slope of annual precipitation and Mann-Kendall statistical test were applied to quantify the trend magnitude and detect the sign...

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Main Authors: Jun Yin, Denghua Yan, Zhiyong Yang, Zhe Yuan, Yong Yuan, Hao Wang, Xiaoliang Shi
Format: Article
Language:English
Published: Wiley 2016-01-01
Series:Advances in Meteorology
Online Access:http://dx.doi.org/10.1155/2016/9137201
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author Jun Yin
Denghua Yan
Zhiyong Yang
Zhe Yuan
Yong Yuan
Hao Wang
Xiaoliang Shi
author_facet Jun Yin
Denghua Yan
Zhiyong Yang
Zhe Yuan
Yong Yuan
Hao Wang
Xiaoliang Shi
author_sort Jun Yin
collection DOAJ
description Based on observed data and data simulated by climate models, temporal variation and spatial distribution of precipitation in China from 1961 to 2050 were investigated. The slope of annual precipitation and Mann-Kendall statistical test were applied to quantify the trend magnitude and detect the significant trend, respectively. Besides, decadal and interannual variations of different rain belts were analyzed to reveal the spatial changing pattern of precipitation. Results indicated the following. (1) During 1961–2011, annual precipitation in Haihe River Basin decreased significantly while the annual precipitation in river basins in the northwest increased significantly. Although the annual precipitation of Yangtze River Basin has an indistinctive decreasing trend, that in the middle and lower reaches has increased and that in the upper reaches has decreased. Arid zone and humid zone are shrinking while semiarid and semihumid zone are expanding. Transformation between semiarid and arid zones, humid and semihumid zones is frequent. During 2011–2050, annual precipitation will not change much (−6~12%) except river basins in the southwest (more than 40%) compared with the baseline. Besides, the area of arid zone will decrease and humid zone area will increase. Transformation area between semiarid and arid zone and humid and semihumid zone is small.
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institution Kabale University
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language English
publishDate 2016-01-01
publisher Wiley
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series Advances in Meteorology
spelling doaj-art-78d29839aa4444a69977d25ba35e135f2025-02-03T01:22:39ZengWileyAdvances in Meteorology1687-93091687-93172016-01-01201610.1155/2016/91372019137201Research on Historical and Future Spatial-Temporal Variability of Precipitation in ChinaJun Yin0Denghua Yan1Zhiyong Yang2Zhe Yuan3Yong Yuan4Hao Wang5Xiaoliang Shi6State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, Department of Water Resources, China Institute of Water Resources and Hydropower Research, Beijing 100038, ChinaState Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, Department of Water Resources, China Institute of Water Resources and Hydropower Research, Beijing 100038, ChinaState Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, Department of Water Resources, China Institute of Water Resources and Hydropower Research, Beijing 100038, ChinaState Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, Department of Water Resources, China Institute of Water Resources and Hydropower Research, Beijing 100038, ChinaDivision of International Cooperation, China Institute of Water Resources and Hydropower Research, Beijing 100038, ChinaState Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, Department of Water Resources, China Institute of Water Resources and Hydropower Research, Beijing 100038, ChinaCollege of Geomatics, Xi’an University of Science and Technology, Xi’an 710054, ChinaBased on observed data and data simulated by climate models, temporal variation and spatial distribution of precipitation in China from 1961 to 2050 were investigated. The slope of annual precipitation and Mann-Kendall statistical test were applied to quantify the trend magnitude and detect the significant trend, respectively. Besides, decadal and interannual variations of different rain belts were analyzed to reveal the spatial changing pattern of precipitation. Results indicated the following. (1) During 1961–2011, annual precipitation in Haihe River Basin decreased significantly while the annual precipitation in river basins in the northwest increased significantly. Although the annual precipitation of Yangtze River Basin has an indistinctive decreasing trend, that in the middle and lower reaches has increased and that in the upper reaches has decreased. Arid zone and humid zone are shrinking while semiarid and semihumid zone are expanding. Transformation between semiarid and arid zones, humid and semihumid zones is frequent. During 2011–2050, annual precipitation will not change much (−6~12%) except river basins in the southwest (more than 40%) compared with the baseline. Besides, the area of arid zone will decrease and humid zone area will increase. Transformation area between semiarid and arid zone and humid and semihumid zone is small.http://dx.doi.org/10.1155/2016/9137201
spellingShingle Jun Yin
Denghua Yan
Zhiyong Yang
Zhe Yuan
Yong Yuan
Hao Wang
Xiaoliang Shi
Research on Historical and Future Spatial-Temporal Variability of Precipitation in China
Advances in Meteorology
title Research on Historical and Future Spatial-Temporal Variability of Precipitation in China
title_full Research on Historical and Future Spatial-Temporal Variability of Precipitation in China
title_fullStr Research on Historical and Future Spatial-Temporal Variability of Precipitation in China
title_full_unstemmed Research on Historical and Future Spatial-Temporal Variability of Precipitation in China
title_short Research on Historical and Future Spatial-Temporal Variability of Precipitation in China
title_sort research on historical and future spatial temporal variability of precipitation in china
url http://dx.doi.org/10.1155/2016/9137201
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