1) Penman's formula
Penman法
2) Penman-Monteith method
Penman-Monteith法
1.
The water surplus and deficiency(WSD) was calculated with precipitation and reference crop evapotranspiration which were calculated with Penman-Monteith method recommended by FAO in 1990,based on climatic data of 93 meteorological stations in the Yellow River Basin(YRB) authorized by the National Climatic Bureau from 1957 to 2001.
针对黄河流域水资源匮乏日益严重的状况,根据国家气象局整编的1957~2001年(45 a)黄河流域93个气象站点气象资料,应用1998年FAO最新推荐的Penman-Monteith法计算潜在蒸散量,研究黄河流域水分变化特点,尤其是水分亏缺时空格局。
2.
The arid index was calculated with Penman-Monteith method recommended by the FAO in 1990,based on climatic data of 93 meteorological stations in Yellow River Basin(YRB) authorized by the National Meteorological Bureau from 1957 to 2001,and the arid index distribution in Yellow River basin was also created through the kriging method.
根据国家气象局整编的1957~2001年(45 a)黄河流域93个气象站点气象资料,应用1998年FAO最新推荐的Penman-Monteith法计算干燥度中的潜在蒸散项,并在此基础上使用克里格(kriging)插值法生成黄河流域干燥度的分布图。
3) Penman-Monteith equation
Penman-Monteith方法
1.
The Penman-Monteith equation was used as a standard to be comp.
该文根据1996～2000年陕西省榆林、延安与西安三站的逐日气象资料,以FAO推荐的Penman-Monteith方法为标准,对计算参考作物蒸散量的10种方法进行比较。
2.
Based on field test data generated by use of lysimeters,the reference crop evapotranspiration was calculated with the Penman-Monteith equation and the PriestleyTaylor approach,and the actual evapotranspiration from turfgrass was determined with the water balance equation for agricultural land.
根据蒸渗仪试验实测资料,分别利用Penman-Monteith方法和Priestley-Taylor方法计算了参考作物蒸发蒸腾量,并利用农田水量平衡方程计算了草坪草实际蒸发蒸腾量,由此计算了草坪草作物系数,分析了草坪草作物系数的变化规律,构建了作物系数与观测期旬序数之间的回归关系模型。
4) Penman-Monteith method
Penman-Monteith方法
5) Penman method
Penman
1.
Comparative study on Priestley-Taylor and Penman methods in calculating reference crop evapotranspiration;
Priestley-Taylor与Penman法计算参照作物腾发量的结果比较
6) Penman hypothesis
Penman假设
补充资料：法性属法为法性土
【法性属法为法性土】
谓真如法性之理，譬如虚空，遍一切处，乃是法身所证之体，即为所依之土，故名法性属法，为法性土。
谓真如法性之理，譬如虚空，遍一切处，乃是法身所证之体，即为所依之土，故名法性属法，为法性土。
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