[1]HAO Zhen-chun,YAN Long-zeng,JU Qin,et al.Spatiotemporal Characteristics of Climate Variation in Different Kinds of Landforms of Haihe River Basin[J].Research of Soil and Water Conservation,2014,21(01):56-60.
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Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume:
21
Number of periods:
2014 01
Page number:
56-60
Column:
Public date:
2014-02-28
- Title:
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Spatiotemporal Characteristics of Climate Variation in Different Kinds of Landforms of Haihe River Basin
- Author(s):
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HAO Zhen-chun1, YAN Long-zeng1, JU Qin1, Dunzhu Jiacuo2
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1. College of Hydrology and Water Resources, Hohai University, Nanjing 210098, China;
2. Xigaze Branch of the Tibet Autonomous Region Hydrology Bureau, Xigaze, Tibet 857000, China
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- Keywords:
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Haihe River Basin; landforms; climate change; M-K test; potential evaporation
- CLC:
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P461.3
- DOI:
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- Abstract:
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Over the past century, global climate has become warming significantly, which changed the regional hydrologic cycle potentially. In recent 50 years, temperatures keep increasing; water deficit is serious in Haihe River Basin, which has affected the development of society and economy. In order to explore the spatiotemporal characteristics of climate change, the Haihe river basin is divided into three areas as Plateau, Hills, Plain according to the landforms’ spatial heterogeneity. The spatial and temporal patterns of 8 meteorological elements at 34 meteorological stations from 1958 to 2011 were analyzed by using linear trend for inter-annual trend; using the Mann-Kendall test for significance test; using Spearman method for correlation between meteorological elements and ET0 calculated by Penman-Monteith formula. This work is to reveal the regularity of temporal and spatial variation of meteorological elements and the possible driving forces of regional water cycle. The results show that there existed obvious climate change in Haihe River Basin, the temporal and spatial variation of meteorological elements presented obvious zonal, seasonal and interannual characteristics. The temperature went through dropping first and then rising up. Plateau rising speed was faster than Hills and Plain. Precipitation was generally falling. And precipitation of Plain region fell more than Plateau and Hills. Average wind speed, sunshine hours, relative humidity were obvious downward. The potential evaporation was negatively related to the relative humidity, positively related to daily temperature range in Haihe River Basin.