Distribution and Trends in Reference Evapotranspiration in the North China Plain

文献类型： 外文期刊

第一作者： Zhang, H. L.

作者： Zhang, H. L.;Chen, F.;Song, Z. W.;Zhang, H. L.;Chen, F.;Snyder, R. L.;Anderson, F. E.;Song, Z. W.

作者机构：

期刊名称：JOURNAL OF IRRIGATION AND DRAINAGE ENGINEERING （ 影响因子：1.879； 五年影响因子：1.985 ）

ISSN： 0733-9437

年卷期： 2010 年 136 卷 4 期

页码：

收录情况： SCI

摘要： The distribution and trends in reference evapotranspiration (ETo) are extremely important to water resources planning for agriculture, and it is widely believed that rates of ETo will increase with global warming. This is a big concern in China, where water deficits are common in the North China Plain (NCP). In this study, Penman-Monteith reference evapotranspiration at 26 meteorological stations during 1961-2006 in and around the NCP was calculated. The temporal variations and spatial distribution of ETo were analyzed and the causes for the variations were discussed. The results showed that: (1) the NCP was divided into two climatic regions based on aridity values: a semiarid region that accounts for 69% of the area and subhumid regions that made of the remaining area; (2) over the entire NCP, the highest annual ETo occurred in the central and western areas and the lowest total ETo was observed in the east. Comparing the mean monthly ETo and annual ETo distributions, the high ETo values from May through July mainly determined the annual ETo distribution; (3) for the whole NCP, annual ETo showed a statistically significant decrease of 11.92 mm/decade over the 46 years of data collection in the NCP or approximately a 5% total decrease compared to the ETo values in 1961; (4) to determine which variable has the greatest effect on the decrease in ETo, decadal changes were observed for daily values of maximum air temperature (+0.16 degrees C), minimum air temperature (+0.35 degrees C), net radiation (-0.13 MJ m(-2)), and mean wind speed (-0.09 m s(-1)). These results indicate that the decreasing net radiation and wind speed had a bigger impact on ETo rates than the increases observed by the maximum and minimum temperatures.

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