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辐射气候
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  radiation climate
     THE CHARACTERISTICS OF RADIATION CLIMATE OF SANJIANG PLAIN
     三江平原的辐射气候特征
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     THE RADIATION CLIMATE OF TAIWAN, CHINA
     台湾省辐射气候特征
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     Then thelong time change feature of radiation climate over china is analyzed- The resultsshow that, the radiation climate changes a little before 1950s.
     通过总辐射年值的10年滑动平均曲线和累积距平曲线可以得到我国太阳总辐射气候长期变化的趋势特征是:50年代以前,我国的总辐射比较平稳,没有大的变化;
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  “辐射气候”译为未确定词的双语例句
     THE CLIMATIC CHANGE OF GLOBAL SOLAR RADIATIONOVER THE YELLOW RIVER BASIN DURING 1960-2000
     1960~2000年黄河流域太阳总辐射气候变化规律研究
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     global warming potential of greenhouse gases; radiative forcing and climate effect of tropospheric and stratospheric aerosols; impact of human activities on fu ture climate variability over East Asia and China and the climate variability in East Asia and China dur ing the period of the 20th century and the 21st century.
     系统总结和介绍了20世纪90年代以来作者所开展的有关人类活动对东亚和中国气候影响的一系列研究活动、其中包括温室气体辐射强迫及其气候效应,大气微量气体的全球增温潜能,对流层和平流层气溶胶的辐射气候效应,气候系统外部因子对中国气候影响的总体评估,人类活动对中国和东亚地区未来气候变化的影响,以及20世纪和21世纪东亚及中国的气候变化。
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     Using NOAA's monthly mean grided Out going Longwave Radiation(OLR) data with the grid of 2.5°×2.5° Lat/lon during the past 15 years,the radiation climatic feature over Yunnan and around areas have been analysed. The result shows OLR distribution is longitudinal pattern,it is low in north region and high in south region during winter monsoon,it is reversed during summer monsoon.
     利用美国NOAA卫星观测的15年2.5°×2.5°经纬度网格月平均射出长波辐射(OLR)资料对云南及其邻近地区的辐射气候特征进行了分析,发现OLR分布基本呈纬向型,冬季风期间呈北低南高,夏季风期间则相反。
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     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
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     The comparison of different simulation methods for the climate responses of the radiative forcing of anthropogenic sulfate aerosol over east Asia
     东亚地区人为硫酸盐气溶胶辐射气候效应不同模拟方法的对比
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  相似匹配句对
     THE CHARACTERISTICS OF RADIATION CLIMATE OF SANJIANG PLAIN
     三江平原的辐射气候特征
短句来源
     THE RADIATION CLIMATE OF TAIWAN, CHINA
     台湾省辐射气候特征
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     Climate of Uncertainty
     不确定的气候
短句来源
     On radiation from printed circuits
     印制电路的辐射
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     ,dry—cold climate;
     ,气候干冷 ;
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  radiation climatology
A contribution to the radiation climatology of Northern Europe
      
It has been in operation since 1995 and a complete radiation climatology of the data collected has not yet been complied.
      
  radiation climate
This shows that the distribution of regression coefficients is more closely related to the local seasonal radiation climate controlled by the prevailing winter monsoon, Bain, and the terrain features rather than to latitude or meann/N.
      
The new coefficients in the formulae for the effective emittance, which have been derived from meteorological data, demonstrate that these coefficients strongly depend on the radiation climate of the respective area.
      
Global radiation climate changes: The world network
      
Global radiation climate change at seven sites remote from surface sources of pollution
      
Radiation climate map for analyzing risks to astronauts on the mars surface from galactic cosmic rays
      
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The paper discusses the following aspects:1) A general formula for total radiation is derived and its agreement with existing empirical expressions is verified;2) The relationship between cloud cover n and sunshine s_1 is examined together with their effect on total radiation by utilization of hourly data in a 4-year period over Guilin (Guangxi) and Wujing (Jiangsu), respectively.

本文系《再论总辐射的气候学计算方法》的第一部分。讨论以下几个问题: 1.用半理论半经验的方法推导了总辐射气候学计算的一般式,并证实了它与现有各种经验式的一致性。2.利用桂林和武进四年逐时的资料,讨论了天空遮蔽度n与S_1的相互关系及其作用。

Data used come from 75 stations over China for 1957—1977.All factors in the formula and the calculating method are analyzed and compared. This results in a method more suitable for climatological calculation of total radiation for our country. Also, the spatial distributions of annual and monthly total insolation over the country are computed and shown on maps separately.

文中根据75个日射站的资科(1957—77年)对计算式中各因子和计算方法进行了分析比较,确定了一个比较适合我国的总辐射气候学计算方法。最后计算并绘制了我国年以及各月的总辐射空间分布图。

The present paper deals with the characteristicts of the radiation in loess plateau of China, The auther has obtained the following points of view:1. The annual total radiation is 115-160 kcal/cm~2, the maximum of annual variation occuss in June, and the minimum in December, The net radiation is 43-58 kcal/cm~2.2. The sunshine duration and amount of solar radiation for various slopes in loess plateau are given in tables 4—7.3. Based on the data of radiation observed from May to Augaust 1979 in Qinghai-Xizang...

The present paper deals with the characteristicts of the radiation in loess plateau of China, The auther has obtained the following points of view:1. The annual total radiation is 115-160 kcal/cm~2, the maximum of annual variation occuss in June, and the minimum in December, The net radiation is 43-58 kcal/cm~2.2. The sunshine duration and amount of solar radiation for various slopes in loess plateau are given in tables 4—7.3. Based on the data of radiation observed from May to Augaust 1979 in Qinghai-Xizang Plateau, the auther has obtained the formula which may be used to various altitude, i. e.F_p=F_(op)(1-0.45n_(hm)-0.71n_1)[1.572-0.689(((P-550)/(P_0)))~(0.2)]F_(op)=[δσT_0~(?)-δσT~4(0.63-0.03n+0.05(2~(1/e)][1.984-1.004(P/P_0)~(0.8)]This formula is capable to be used in loess plateau.

本文考虑了海拔高度和坡度坡向对辐射的影响,应用1959—1977年的日射观测资料分析了黄土高原的辐射气候特征,文中表4—7列举的坡地辐射数值可供有关部门应用。

 
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