1) potential evapotranspiration
潜在蒸散量
1.
Method for computation of potential evapotranspiration in Yarlung Tsangpo River Basin;
雅鲁藏布江流域潜在蒸散量计算方法
2.
Make use of the climatic data during 1971—2006 observed by 11 meteorological stations in Bazhou regions of Xinjiang,the potential evapotranspiration in every station were calculated with the Penman-Monteith equation recommended by FAO in 1998,and the spatio-temporal changes of the variation characteristics of potential evapotranspiration in Bazhou regions were analyzed.
在利用巴州11个地面气象观测站1971—2006年的逐月历史气候资料和联合国粮农组织(FAO)推荐的Penman-Monteith公式计算出巴州各地逐年潜在蒸散量的基础上,采取线性回归、最大熵谱、Mann-Kendall以及自然正交分解(EOF)等方法,对近36a巴州潜在蒸散量的时空变化特征进行了分析,结果表明:①近36a巴州潜在蒸散量总体呈递减趋势,递减倾向率为-42。
3.
The aridity index is defined as a ratio of potential evapotranspiration to precipitation,and potential evapotranspiration is computed using FAO Penman-Monteith model.
利用河北省1970—2007年48个气象台站逐日资料,采用Penman-Monteith模型计算潜在蒸散量,由潜在蒸散量和降水量之比构建干燥度指数,并采用Kriging插值法进行空间插值以分析其区域特征。
2) latent evapotranspiration
潜在蒸散发量
1.
Comparison of latent evapotranspiration on the different land use type:a case study of second forest ecosystem and tea garden ecosystem;
不同土地利用型态下潜在蒸散发量比较——以二次林生态系统与茶园生态系统为例
3) wheat potential evapotranspiration
小麦潜在蒸散量
1.
According to the reference crop potential evapotranspiration model (FAO-Penman-Monteith),which modified by crop coefficient,radiation stress coefficient and wind speed reduced coefficient,the wheat potential evapotranspiration (ET_(pp)) model in an apple-wheat intercropping in the hilly land of Taihang Mountain was developed.
根据FAO(1991)推荐的参考作物需水量(ET0)计算模式(FAO Penman Monteith),并通过作物系数、农林复合系统作物光胁迫系数及风速减弱系数的综合订正,建立太行山低山丘陵区苹果 小麦复合系统小麦潜在蒸散量计算模型,并利用Li 1600稳态气孔仪实测得到小麦蒸腾量,经转换后得出蒸散量对模型进行验证,旨在探索农林复合系统中作物蒸散的计算方法,为进一步开展水分生态特征的研究提供可行性途径。
4) Evapotranspiration
[英][i,væpəu,trænspi'reiʃən] [美][ɪ,væpo,trænspə'reʃən]
潜在蒸散
1.
Spatial and Temporal Variations of Differences Between Evapotranspiration and Precipitation in Inner Mongolian Steppe during Warm Season;
本文利用1960-2004年内蒙古典型草原区及其周边38个气象台站的气候资料,采用Penman-Monteith公式计算暖季(4-8月)的潜在蒸散量及相应的蒸降差,用经验正交函数(EOF)和旋转正交函数(REOF)研究蒸降差的时空分异特征。
5) potential evapotranspiration
潜在蒸散
1.
Agricultural climate division of Hebei Province based on potential evapotranspiration and surface aridity index
基于潜在蒸散和干燥度指数的河北省农业气候区划
2.
The results indicated that in 1961-2006, the annual potential evapotranspiration was decreased with a rate of 13.
应用Penman-Monteith模型分析了西藏羊卓雍湖流域潜在蒸散、干湿指数的年际变化趋势、年代际变化特征,并讨论了影响干湿指数变化的气象因子。
3.
Based on the climate data of 77 meteorological stations covering 1958-2001 in northwestern China (the area is within the north of 35oN and west of 105oE in China), and using the integrated Penman formula, the mean potential evapotranspiration (PE) in our study area is calculated.
根据西北地区77个气象台站气候资料,并利用改进的Penman公式,计算了该地区1958年~2001年的44年平均潜在蒸散量的时空分布,并分析了与降水量变化之间的关系,得到4种类型潜在蒸散量与降水量年际变化的组合分布型。
6) potential evapotranspiration
潜在蒸散发
1.
Differences of changes in potential evapotranspiration and its factors over the upper,middle and lower reaches of Heihe River Basin
黑河流域上中下游潜在蒸散发变化及其影响因素的差异
补充资料：蒸散(见蒸发和蒸散量)
蒸散(见蒸发和蒸散量)
zhengsan蒸散见蒸发、燕散，。
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