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   气候计算 的翻译结果: 查询用时:0.408秒
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气候计算     
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  climatological calculation
     CLIMATOLOGICAL CALCULATION OF POSSIBLE DIRECT SOLAR RADIATION AND ITS DISTRIBUTIVE FEATURES OVER CHINA
     中国可能太阳直接辐射的气候计算及其分布特征
短句来源
     CLIMATOLOGICAL CALCULATION OF NET RADIATION ON SLOPES IN CHINA
     中国坡地净辐射的气候计算和分析
短句来源
     CLIMATOLOGICAL CALCULATION OF POSSIBLE GLOBAL RADIATION ALONG WITH ITS DISTRIBUTION OVER CHINA
     中国可能太阳总辐射的气候计算及其分布特征
短句来源
     A FURTHER RESEARCH ON THE CLIMATOLOGICAL CALCULATION METHOD OF THE GLOBAL SOLAR RADIATION OVER CHINA
     中国太阳总辐射气候计算方法的进一步研究
短句来源
     CLIMATOLOGICAL CALCULATION OF DOWNWARD ATMOSPHERIC RADIATION FOR CHINA AND ITS CHARACTERISTIC DISTRIBUTION
     中国大气逆辐射的气候计算及其分布特征
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  climatic calculation
     QINGHAI XIZANG SURFACE LONGWAVE RADIATION PARAMETERIZATION WITH ITS CLIMATIC CALCULATION
     青藏高原地表长波辐射参数化及其气候计算
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     The form of the profile from the presented scheme agrees' with tl1at from surface an(1aircraft observations at home and abroad. The climatic calculation of the total radiation for 6stations over the Tibetan highland agrees with measurethents.
     按本方案计算的各地晴天总辐射廓线形式,与国内外地面和飞艇探测结果一致。 对青藏高原6站所作晴天总辐射气候计算也与实例值相符。
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  “气候计算”译为未确定词的双语例句
     CLIMATICAL METHOD FOR DIRECT SOLAR RADIATION CALCULATION AND ITS DISTRIBUTION OVER CHINA
     中国太阳直接辐射的气候计算及其分布特征
短句来源
     CLIMATOLOGCAL CALCULATIONS AND DISTRIBUTION OF SOIL HEAT FLUX OVER CHINA
     中国土壤热通量的气候计算及其分布特征
短句来源
     A DISCUSSION ON THE COMPUTATION METHOD FOR THE CLIMATE FROM THE TOTAL QUANTITY OF EFFECTIVE RADIATION AT ARBITRARY PERIODS ON QINGZANG PLATEAU
     青藏高原有效辐射任意时段总量的气候计算方法探讨
短句来源
     CLIMATOLOGICAL CALCULATIONS AND DISTRIBUTION OF SURFACE LATENT HEAT OVER CHINA
     中国地表潜热的气候计算及其分布
短句来源
     If computer facilities andradiosonde data are available, it can be successfully used for climatologi-cal calculation of effective ground radiation.
     该式具有物理意义明确,计算精度较高,普适性好等优点、在有计算条件并具备探空资料的地区,是一种较理想的地面有效辐射气候计算方法。
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  climatological calculation
The climatological calculation equations of global and direct radiation are put forward.
      
Moreover, the 10-year period used for RH determination is not sufficient for a true climatological calculation.
      


The Berland's formula for calculating effective radiation is revised forpractical purposes over China. The revised formula offers clear physicalmeaning, high accuracy and wide application. If computer facilities andradiosonde data are available, it can be successfully used for climatologi-cal calculation of effective ground radiation.

本文在分析Верлянд,M.E.和Берлянд,Т.Г.理论公式的基础上,对该式进行了买用化处理,得到了适用于我国的有效辐射气候计算公式。该式具有物理意义明确,计算精度较高,普适性好等优点、在有计算条件并具备探空资料的地区,是一种较理想的地面有效辐射气候计算方法。

This paper discusses the climatic computational methods of effective radiation over the Qinghai-Xizang Plateau and its adjacent areas by using the data observed over the Qinghai-Xizang Plateau for the period from August 1982 to July 1983, and the distribution figures of the annual total and monthly totals over the Plateau and its adjacent areas are drawn. The results show that the high value of the annual total of effective radiation is in the western part of the Plateau, the values gradually reduce from western...

This paper discusses the climatic computational methods of effective radiation over the Qinghai-Xizang Plateau and its adjacent areas by using the data observed over the Qinghai-Xizang Plateau for the period from August 1982 to July 1983, and the distribution figures of the annual total and monthly totals over the Plateau and its adjacent areas are drawn. The results show that the high value of the annual total of effective radiation is in the western part of the Plateau, the values gradually reduce from western part to eastern past of the Plateau and the low value is in Sichuan Basin. The high and low centers move lightly with the seasonal variation, respectively.

本文利用1982年8月—1983年7月在青藏高原地区观测得到的有效辐射资料,讨论了高原地区有效辐射的气候计算方法,並根据拟合得到的气候计算公式,绘制了高原地区有效辐射的年、月分布图。结果表明,全年有效辐射的分布形势是:高原西部为有效辐射的高值区,由西向东逐渐减少,四川盆地为低位区。随着季节的变化,高低值中心略有偏移。

Based on the real-time observational data from 61 solar radiationstations, a method for climatological calculation of scattering radiationis discussed herein. Through detailed analysis of the effects of cloud-iness on scattering radiation, a semi-theoretical and semi-empiricalclimatological-statistical equation of scattering radiation is proposed,and using cloudiness data from 206 weather stations the scatteringradiation distribution over China is calculated and analyzed.

本文利用我国61个日射站的实测资料,讨论了太阳散射辐射的气候计算方法。在详细分析云对散射辐射影响的基础上,提出了半理论、半经验散射辐射气候计算式,并利用全国206个站的云量资料,计算并分析了散射辐射的全国分布。

 
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