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泾河上游典型站近45年参考作物蒸散量变化特征
引用本文:杨小利,王丽娜.泾河上游典型站近45年参考作物蒸散量变化特征[J].干旱地区农业研究,2012,30(6):238-242.
作者姓名:杨小利  王丽娜
作者单位:1. 中国气象局兰州干旱气象研究所,甘肃省干旱气候变化与减灾重点实验室,中国气象局干旱气候变化与减灾重点开放实验室,甘肃兰州730020;甘肃省平凉市气象局,甘肃平凉744000
2. 甘肃省平凉市气象局,甘肃平凉,744000
基金项目:国家科技部公益行业(气象)科研专项"多时间尺度干旱监测与预警、评估技术研究"
摘    要:为了更好地探讨泾河上游地区植被耗水的变化情况,利用泾河上游4个典型站点近45 a的逐日气象资料,采用Penman-Monteith公式,计算了日参考作物蒸散量,并对ETo的日、月、年值的变化特征进行了分析,同时分析了影响ET0的主要气候因子.结果表明:泾河上游ET0的日均值和月均值与大气温度、日照时数等气象要素均达到极显著相关,与风速的相关程度最低,ET0日变化和月变化均呈现为相似的单峰型变化趋势,峰值出现在夏季7月份.近45年来,只有隆德ET0年值呈显著性增加,其他站ET0年值变化不明显.固原的夏季,隆德的冬、夏、秋季的ET0呈显著性变化,其他站各季节变化均不明显.

关 键 词:参考作物蒸散量  变化特征  泾河上游

Variation characteristics of reference crop evapotranspiiration of typical stations in upper basin of the jinghe River in recent 45 years
YANG Xiaoli,Wang Lina.Variation characteristics of reference crop evapotranspiiration of typical stations in upper basin of the jinghe River in recent 45 years[J].Agricultural Research in the Arid Areas,2012,30(6):238-242.
Authors:YANG Xiaoli  Wang Lina
Institution:Institue of Arid Meteorology, China Meteorological Administration, Key Laboralory of Arid Climatic Change and Reducing Disaster of Gansu Province, Key Open Laboratory of Arid Change and Disasier Reduction of CMA, Lanshou, Gansu 730020, China; Pingliang Meteorological Bureau, Pingliang, Gansu 744000, China
Abstract:To study variation characteristics of vegetation evapotranspiration in the upper basin of Jinghe river, using the meteorological data collected from 4 typical stations in recent 45 years in the upper basin of Jinghe river, the refer-ence crop evapotranspiration(ET0)of each station was calculated with Penman-Monteith equation. The variation charac-teristics of daily, monthly and annual ET0were analysed, and he main meteorological factors which influced ET0 were anlysed. The results show that there is a very significant correlation between the daily, monthly ET0and temperature, sunshine hours and vapor pressure, and the correlation between ET0 and wind speed is relatively smaller. Both daily and montly average ET0 curves have single peak, and the peak appears in July. In reccnt 45 years, there is a significant in-creasing trend of annual ET0 in Longde, while there are no signifieant changes in other stations. There is a significant change trend of ET0 in Guyuan in summer and in Longde in winter, summer and autumn, while therer are no significant change in each season of other stations.
Keywords:reference crop evapotranspiration  variation characteristics  the upper basin of Jinghe river
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