1) reference crop evapotranspiration
参考作物蒸散量
1.
Estimation of reference crop evapotranspiration by Chinese pan;
利用小蒸发皿观测资料确定参考作物蒸散量方法研究
2.
Evaluation on several temprature-based methods for estimating reference crop evapotranspiration;
几种基于温度的参考作物蒸散量计算方法的评价
3.
Temporal-spatial changing characteristics of reference crop evapotranspiration in Gansu Province;
甘肃地区参考作物蒸散量时空变化研究
2) reference evapotranspiration
参考作物蒸散量
1.
Comparison of many equations for calculating reference evapotranspiration in the Loess Plateau of China;
黄土区参考作物蒸散量多种计算方法的比较研究
2.
Analysis of temporal-spatial characteristics of reference evapotranspiration based on GIS technology in Northeast China during 1991～2000;
GIS环境下1999～2000年中国东北参考作物蒸散量时空变化特征分析
3.
A distributed model of reference evapotranspiration based on the DEM;
参考作物蒸散量的分布式模型
3) The reference crop evapotranspiration
参考作物蒸散量
1.
The reference crop evapotranspiration(ETo) is the most important index that indicate the capability of atmospheric evaporative and assess the degree of the climatic drought, the consumption water of the vegetation, the potentiality of the production and the supply and demand balance of water resources.
参考作物蒸散量是表征大气蒸(散)发能力,评价气候干旱程度、植被耗水量、生产潜力以及水资源供需平衡的最重要的指标之一。
4) Reference crop evapotranspirations (ET_0)
参考作物蒸散量ET0
5) reference crop evapotranspiration
参考作物蒸散发
1.
Sensitivity of the reference crop evapotranspiration in growing season in the West Songnen Plain;
松嫩平原西部生长季参考作物蒸散发的敏感性分析
6) reference crop evapotranspiration
参考作物蒸散
1.
Based on the meteorological data collected from 616 weather stations in China during 1975—2004,daily,monthly and annual reference crop evapotranspiration(ET0) were calculated by using the Penman-Monteith equation recommended by FAO.
根据我国616个地面气象台站1975—2004年的观测资料,利用联合国粮农组织推荐的Penman-Monteith公式计算各年逐日、逐月参考作物蒸散值(ET0)和年总量。
2.
Based on FAO-Penman-monteith method and Hargreaves method, the paper studied the reference crop evapotranspiration (ET_0) of sixteen meteorological observatories in four climate zones of the northeastern China, and analyzed the results of the two methods.
运用FAO Penman monteith方法和Hargreaves方法对中国东北地区4个气候大区16个气象台站的参考作物蒸散(ET0)进行了研究,并对FAO Penman monteith方法和Hargreaves方法的计算结果进行分析。
补充资料：蒸散量
分子式：
CAS号：
性质：又称腾发量或总蒸发量。农田土壤蒸发和植物蒸腾的总耗水量。蒸散量是农田水分平衡的重要组成部分，一般受下述因素影响：大气干燥程度，辐射条件及风力大小，土壤湿润程度和导水能力，植被状况(包括植物群体结构、植物水分输导组织、叶片气孔数量、大小等)。
CAS号：
性质：又称腾发量或总蒸发量。农田土壤蒸发和植物蒸腾的总耗水量。蒸散量是农田水分平衡的重要组成部分，一般受下述因素影响：大气干燥程度，辐射条件及风力大小，土壤湿润程度和导水能力，植被状况(包括植物群体结构、植物水分输导组织、叶片气孔数量、大小等)。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条