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首页> 外文期刊>Agricultural and Forest Meteorology >Temporal variation of reference evapotranspiration during 1961-2005 in the Taoer River basin of Northeast China
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Temporal variation of reference evapotranspiration during 1961-2005 in the Taoer River basin of Northeast China

机译:1961-2005年中国东北Tao河流域参考蒸散量的时空变化

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摘要

Evapotranspiration is an important flux term in the water cycle that integrates atmospheric demands and surface conditions. Thus, analysis of the temporal variation of reference evapotranspiration (ET_o) will help us to understand climate change and its effect on hydrology. In this paper, we present an analysis of the monthly ET_o at 15 stations during 1961 -2005 in the Taoer River basin in China, calculated by the FAO Penman-Monteith method. We derived the growing season and annual total ET_o time series and using the Mann-Kendall method, moving t test and Morlet wavelet conducted comprehensive time series analysis to characterize significance test, abrupt change and period in the ET_o data sets. The results present that: (i) in terms of the seasonal cycle, monthly ET_o reaches its peak in May and growing season ET_o accounts for 60.7% of annual total. Long term growing season ET_o fluctuates in accordance with annual ET_o, both having turning points in 1982 and 1993; (ii) with respect to the longterm persistence, the trends for growing season and annual ET_o show the same spatial patterns: high positive values in the west study area in the upper reach and negative values in the Southeast study area in the lower reach. The spatial distribution of annual tendencies suggests an influence from the altitude and latitude; (iii) for individual station, abrupt changes in annual ET_o are more pronounced than those in growing season ET_o. The timings for the abrupt changes in ET_o series at individual stations are consistent with those in regional ET_o. Abrupt changes detected in the early 1980s are all increasing changes, while those in earlier 1990 are all decreasing changes; and (iv) based on the Morlet wavelet analysis, there exist significant periods of 1, 3 and 7.3 years in annual ET_o series and significant 1 year period and 7.3 years period in growing season ET_o series. Maximum air temperature, mean air temperature, relative humidity and bright sunshine hours are main climate variables responsible for the periodicity in ET_o.
机译:蒸散量是水循环中重要的通量,它综合了大气需求和地表条件。因此,对参考蒸散量(ET_o)随时间变化的分析将有助于我们了解气候变化及其对水文学的影响。本文通过粮农组织Penman-Monteith方法,对1961年至2005年中国陶尔河流域15个站的月ET_o进行了分析。我们推导了生长季节和年度总ET_o时间序列,并使用Mann-Kendall方法,移动t检验和Morlet小波进行了全面的时间序列分析,以表征ET_o数据集中的显着性检验,突变和周期。结果表明:(i)就季节周期而言,每月ET_o在5月达到峰值,生长季节ET_o占年度总量的60.7%。长期生长期ET_o根据年度ET_o波动,这两个年份的转折点分别为1982年和1993年。 (ii)就长期持久性而言,生长季节和年度ET_o的趋势显示出相同的空间格局:上游的西部研究区的正值较高,而下游的东南研究区的负值较高。年趋势的空间分布表明受到海拔和纬度的影响。 (iii)对于单个气象站,年度ET_o的突变比生长季节ET_o的突变更为明显。各个台站ET_o系列突然变化的时间与区域ET_o一致。 1980年代初发现的突然变化都是不断变化的变化,而1990年代初则是不断变化的变化。 (iv)基于Morlet小波分析,年度ET_o系列存在1、3和7.3年的有效期,而生长季ET_o系列则存在1年和7.3年的有效期。最高气温,平均气温,相对湿度和明媚的日照时间是决定ET_o周期性的主要气候变量。

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