albedo造句

"albedo"是什么意思   

例句与造句

  1. The result images showed that the distribution of albedo has a close connection with terrain and snow
    对反照率及其变化进行分析,发现反照率的总体分布与地形及雪域密切相关。
  2. Retrieval of the surface albedo under clear sky over china and its characteristics analysis by using modis satellite date
    卫星资料反演中国地区晴空地表短波反照率及其特征分析
  3. The purpose of neutron albedo experiment is to check and scale the programs , parameters and methods used in engineering design
    摘要中子反照实验的目的是检验和标定工程设计使用的程序、参数和方法。
  4. The objective of this paper is to retrieve the albedo of the plateau and then to calculate the parameters about hot or cold source quantitatively
    本文的目的是对青藏高原地表反照率和冷热源参数进行定量反演。
  5. The effects of altitude , surface albedo , total ozone , aerosol and cloud on uv - b are studied with a radiative transfer model ? uv
    利用tuv辐射传输模式研究了海拔高度、地表反照率、臭氧总量、气溶胶和云等对uv - b的影响。
  6. It's difficult to find albedo in a sentence. 用albedo造句挺难的
  7. Snow covered surfaces have a high albedo ; the albedo of soils ranges from high to low ; vegetation covered surfaces and oceans have a low albedo
    覆雪表面具有高的反射率;土壤的反射率由高到低变化较大;植被表面和海洋的反射率较低。
  8. Based on this model , the scattering properties and albedo wq of melting particles have been calculated by use of the coated sphere bhcoat method
    第二,根据融化层的物理特性分析建立了更为切合实际且较简单的融化粒子涂水冰球模型。
  9. The daily albedo variation , which is big in the morning and afternoon and smallest at midday , emerge parabola above spring wheat and bare soil surface
    春小麦和裸地两种不同下垫面的地表反射率日变化均呈现出抛物线特征,早晚反射率较大,正午反射率最小。
  10. The parameterization of clear - sky surface solar net radiation under the conditions of various albedos is obtained through the error correction due to albedo variation
    然后将地表反射率的影响作为误差项进行订正,从而得到各种地表反射率条件下的晴天地表太阳净辐射的计算方法。
  11. The fine soil characters have little variation of albedo and absorbed solar radiation . the simulated sensible heat is lower than the result of the control run in clay case
    粘土反照率变化不大,因此吸收太阳辐射变化不明显,用于蒸发的潜热变化不明显,地温略降低,感热变小。
  12. Basing the radiative transfer model of terrain area , a new model for calculating the albedo over terrain area was put forwarded by improve irons " model of albedo calculation with 10 spectrurns
    在以上提出的山地辐射传输模型基础之上,对irons等提出的10波段反照率计算方法进行了发展,提出了高原山区的反照率计算模型。
  13. The biggest diurnal albedo is 0 . 24 and the smallest 0 . 11 . moreover , the peak occurs on the day that radiation is very strong and the soil surface is dry and the valley appears on the day that rainfall is much more before this day and the soil water content of upper layer is high
    就反射率的日际变化而言,最大反射率为0 . 24 ,最小为0 . 11 ,相差一倍以上,其峰值均出现在辐射比较强,地表比较干燥的日期,而谷底一般是在前期降雨较大,表层土壤湿润时出现。
  14. The surface solar total radiation is first calculated when albedo is fixed under clear - sky varying atmospheric conditions by using the radiation transfer model and the model atmosphere profile of the middle latitude summer , and a parameterization scheme is then proposed based on the result
    首先利用辐射传输模式和中纬度夏季标准大气廓线,分谱带计算晴天各种大气条件下地表反射率取定值时的地表太阳总辐射,并把所得的结果作为标准资料,提出参数化方案。
  15. One avhrr image of the yangtze delta at 13 : 00 on 15th apr . , 2003 is used to retrieve the regional parameter such as surface albedo , ndv1 , surface emissivity and surface temperature , which is based on regional trait of the yangtze delta to choose different model . all above will give a methodological support to gain the regional surface parameters , what ' s more , it will afford the parameter support to calculate the regional et too
    选取了2003年4月15日13时的avhrr影像,根据长江三角洲区域特点,选择不同的反演模型,分别对长江三角洲区域地表反照率、归一化植被指数、地表比辐射系数、地表温度进行了反演,为区域地表参数的获取提供了方法支持,也为长江三角洲的区域蒸散量求取提供了参数支持。
  16. Then basing the empirical formal proposed by weng burning , a method for reckon the average flux of energy transfer from ground surface to the air of a day according albedo and terrain parameters was put forwarded . it is considered that the flux is a proper index to decide if the area is a hot source or a cold source
    然后,在翁笃鸣等提出的有关半经验公式的基础上,提出了根据反照率和地形参数计算高原地面向大气输送能量的日平均通量的算法,并以此作为判定冷热源的标准。
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