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upward radiation
相关语句
  向上辐射
     However, inthe middle region influenced by sun glitter, the reflection energy acutely increasesdozens of times more than the water body's upward radiation energy, which nearlymakes the sensor saturated, and can not distill water body information from the totalradiation energy.
     但是,在受太阳耀光影响的中心区域,反射光能量非常强,比水体向上辐射量高出几十倍,传感器几乎达到饱和,根本无法从总的辐射量中提取水体信息。 水体可见光遥感过程中大都必须避开太阳光的直接反射,而接收到由水体后向散射过程中的上行辐射,这就使传感器接收到的海洋水体信息非常微弱。
短句来源
     After the 6S model was discussed,some opinions were presented:(1) In consideration of difficult calculation of some components,inaccurate calculation results and the sum of five components being not strictly equivalent to the total radiation intensity,it is unnecessary to divide the upward radiation intensity into five components in the 6S model.
     对6S模型中的算法进行了探讨,并提出了不同的看法:a. 6S模型中将向上辐射强度分解为5个组分是没有必要的,事实上其中有些组分很难计算,其计算结果也不够精确,同时这5个组分之和也并不严格等于总辐射强度;
短句来源
     A method for dividing the upward radiation intensity was proposed,by which the atmospheric correction was done conveniently.
     最后,提出了一种更便于大气订正的向上辐射强度划分方法.
短句来源
  “upward radiation”译为未确定词的双语例句
     CLIMATOLOGICAL CALCULATION AND SPACE-TIME PATTERN OF ATMOSPHERIC UPWARD RADIATION
     中国大气向上辐射的气候计算及其分布特征
短句来源
     Based on radiomersonde data lrom 8 land stations in indra for the MONEX period of May-August 1979, a study is made of atmospheric upward radiation (AUR) at varicus isobaric levels with the calculation expression proposed, viz. ,
     本文根据1979年5—8月季风试验(MONEX)期间印度8个陆地辐射探空站资料,讨论并提出了各等压面大气向上辐射的气候计算式: U↑=ρT~4[a-bln(1+e)] 该式具有形式简单,拟合精度较高的优点。 在此基础上计管并讨论了全国104站500hPa等压面大气向上辐射的时空分布特征,得到一些有意义的结果。
短句来源
  相似匹配句对
     Radiation and Life
     辐射与生命
短句来源
     RADIATION PROCESSING
     辐射加工工艺
短句来源
     CLIMATOLOGICAL CALCULATION AND SPACE-TIME PATTERN OF ATMOSPHERIC UPWARD RADIATION
     中国大气向上辐射的气候计算及其分布特征
短句来源
     The diurnal variations of downward and upward short wave radiation were same.
     向下和反射的短波辐射具有相同的日变化规律。
短句来源
     Upward Slicing Method
     恒底上行分层采煤法
短句来源
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  upward radiation
The model implies the presence of two hydrobiological characteristics in the algorithm for the spectral composition of upward radiation, namely the phytoplankton pigment concentration and the total particulate organic matter.
      
Combined use of spectral brightness and polarization characteristics of upward radiation in remote sensing of inland waterbodies
      
The longwave upward radiation was calculated for an urban canopy by using a Monte Carlo model.
      
This pattern of upward radiation from stretched ankle muscles was not as clear for anterior platform displacements, where early neck flexor muscle responses were observed during the ascending sequence on the flexor surface of the body.
      
sky), and the other set is the canopy reflectance (αb) and transmittance βb for the upward radiation from below the canopy (i.e., ground).
      
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Based on radiomersonde data lrom 8 land stations in indra for the MONEX period of May-August 1979, a study is made of atmospheric upward radiation (AUR) at varicus isobaric levels with the calculation expression proposed, viz.,

本文根据1979年5—8月季风试验(MONEX)期间印度8个陆地辐射探空站资料,讨论并提出了各等压面大气向上辐射的气候计算式: U↑=ρT~4[a-bln(1+e)] 该式具有形式简单,拟合精度较高的优点。在此基础上计管并讨论了全国104站500hPa等压面大气向上辐射的时空分布特征,得到一些有意义的结果。

After the 6S model was discussed,some opinions were presented:(1) In consideration of difficult calculation of some components,inaccurate calculation results and the sum of five components being not strictly equivalent to the total radiation intensity,it is unnecessary to divide the upward radiation intensity into five components in the 6S model.(2) There is a relatively marked error in the computation by 6S model for the adjacency effect.(3) The computation of 1-D ground-atmosphere coupled radiation...

After the 6S model was discussed,some opinions were presented:(1) In consideration of difficult calculation of some components,inaccurate calculation results and the sum of five components being not strictly equivalent to the total radiation intensity,it is unnecessary to divide the upward radiation intensity into five components in the 6S model.(2) There is a relatively marked error in the computation by 6S model for the adjacency effect.(3) The computation of 1-D ground-atmosphere coupled radiation is a simple question,it would be better to choose discrete ordinates method developed by the international radiation heat transfer circle to solve it.(4) It would be better to use the backward Monte Carlo method to calculate the adjacency effect.The developed multi-steps method was further expanded to calculate more upward radioactive components.A method for dividing the upward radiation intensity was proposed,by which the atmospheric correction was done conveniently.

对6S模型中的算法进行了探讨,并提出了不同的看法:a.6S模型中将向上辐射强度分解为5个组分是没有必要的,事实上其中有些组分很难计算,其计算结果也不够精确,同时这5个组分之和也并不严格等于总辐射强度;b.6S模型对邻近效应的计算也存在着较大误差;c.一维地-气耦合辐射的数值计算只是一个很简单的问题,宜首选国际辐射传热界发展的离散坐标法来求解;d.宜选用逆向蒙特卡罗法来分析邻近效应.另外,对最近提出的多步法做了进一步扩展,以使其能计算更多的向上辐射强度组分.最后,提出了一种更便于大气订正的向上辐射强度划分方法.

The net pyrradiometer is used to measure the differences of irradiance between downward and upward radiation including downward short-wave radiation,downward long-wave radiation,upward short-wave radiation and long-wave radiation. The sensitivity of net pyrradiometer can be tested by two pyrgeometers and two pyranometers.

净全辐射表是测量太阳与大气向下发射的全辐射和地面向上发射的全辐射之差值的仪器,它的灵敏度可用二台长波辐射表和二台短波辐射表来测试。

 
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