1) FAO56 Penman-Monteith method
FAO56Penman-Monteith方法
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 equation
Penman-Monteith方程
1.
Calculating alfalfa irrigation quota by FAO Penman-Monteith equation;
应用Penman-Monteith方程推算北京地区苜蓿的灌溉定额
2.
With 34 meteorological stations data including minimum and maximum air temperature,wind speed,air humidity and sunlight hours from 1951 to 2000,ET0 was obtained by FAO Penman-Monteith equation(P-M) for growing season in western Songnen Plain of Northeast China.
采用松嫩平原西部34个气象站1951￣2000年5个气象要素资料,运用FAO Penman-Monteith方程计算参考作物蒸散量,建立了各站与区域蒸散量序列。
3.
[Method] Penman-Monteith equation was adopted to calculate ET0 in Australia from 1998 to 2007.
[方法]利用Penman-Monteith方程计算澳大利亚1998～2007年的参考作物蒸散量(ET0),通过GIS方法分析ET0的时空变化特征并探讨ET0与主要气候因子的关系。
5) 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。
6) 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。
补充资料：[3-(aminosulfonyl)-4-chloro-N-(2.3-dihydro-2-methyl-1H-indol-1-yl)benzamide]
分子式：C16H16ClN3O3S
分子量：365.5
CAS号：26807-65-8
性质：暂无
制备方法：暂无
用途：用于轻、中度原发性高血压。
分子量：365.5
CAS号：26807-65-8
性质：暂无
制备方法：暂无
用途：用于轻、中度原发性高血压。
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