1) 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。
2) 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。
3) Penman-Monteith method
Penman-Monteith方法
4) Penman-Monteith formula
Penman-Monteith公式
1.
Influence of e_a on calculation of reference crop evapotranspiration with Penman-Monteith formula;
不同e_a计算方法对Penman-Monteith公式的影响
2.
The consult crops water demand ETO of every month (5~9 month) in ten years is calculated with Penman-Monteith formula.
根据抚顺地区3个气象站10年的气象资料,应用Penman-Monteith公式计算了10年来每年(5～9月)各月的参考作物需水量ET0,分析了ET0的月际变化和年际变化特征,同时分析了各气象因素对ET0的影响。
5) Penman-Monteith equation
Penman-Monteith公式
1.
Changes of reference crop evapotranspiration(ET0) and its causes were analyzed by the computed ET0 using Penman-Monteith equation which was recommended by FAO according to weather data of 41 years for 30 weather stations in Guanzhong Region of Shaanxi Province(Central Shaanxi Plain).
根据关中地区30个气象站41年的气象资料,采用FAO推荐的Penman-Monteith公式计算参考作物蒸发蒸腾量(ET0),分析了陕西关中地区ET0的变化及原因,结果表明,从长期来看,关中地区ET0在减少趋势的基础上表现出周期性变化,从阶段性来看,1980年之前和之后则主要表现为增加趋势。
2.
Based on the meteorological data collected from 3 stations in recent 10 years in Fushun region,the reference crop evapotranspiration(ET_0) was calculated with the Penman-Monteith equation recommended by FAO in 1990.
根据抚顺地区3个气象站的气象观测资料,应用1990年联合国粮农组织推荐的Penman-Monteith公式计算各站1995~2004年10年来的参考作物需水量ET0。
3.
Based on daily meteorological data from 1989 to 1996 of Aksu Water Balance Experimental Station, CAS in Alaer irrigated area in Tarim river basin, daily reference crop evapotranspirations are calculated by Penman-Monteith equation.
利用Penman-Monteith公式,根据阿克苏水平衡试验站1989～1996年逐日气象资料,计算了逐日参考作物潜在腾发量,分析了其变化特征,建立了其与其它气象要素、20cm蒸发皿蒸发量的相关关系。
6) Penman-Monteith model
Penman-Monteith模型
1.
Based on the Bowen ratio energy balance(BREB) measurements during 2004~2005 entire maize growing season,the performance of hourly and daily evapotranspiration(ET) was estimated by both the Shuttleworth-Wallace model and the Penman-Monteith model.
根据夏玉米生长季内逐时波文比系统观测资料和主要生育期的作物资料,以波文比-能量平衡法(BREB法)得到的蒸散量为实测值,对比研究了Shuttleworth-Wallace模型(以下简称S-W模型)、Penman-Monteith模型(以下简称P-M模型)对蒸散估计的差异。
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。
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