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1.Albedo Monte Carlo Method and MORSE-ALBC Code
反照蒙特卡罗方法和MORSE-ALBC程序收藏指正
2.Global BRDF and Albedo from the EOS ?MODIS and MISR Sensors
用EOS MODIS和MISR数据计算全球BRDF和反照率(英文)收藏指正
3.Retrieval of the Land Surface Albedo over Arid Oasis of Northwest China from EOS-MODIS Data
应用EOS-MODIS卫星资料反演西北干旱绿洲的地表反照率收藏指正
4.Undressed ore for nature massive, the monthly output may amount to 5,000 tons; Undressed ore albedo above 95.
原矿为自然块状,月产量可达5000吨;原矿白度95以上。收藏指正
5.For the wavelength shorter than 500nm, the single scattering albedo (SSA) is higher in summer and lower in spring.
在波长小于500nm时,单次散射返照率是夏季较高,春季较低;收藏指正
6.(2) the relationship between the NDVI and the albedo is a power function in the fully covered areas by vegetation, and between the surface temperature and the albedo is a linear function in the dry or wet condition;
农田植被和天然植被的植被指数变化规律不同; 在植被全覆盖区域,植被指数与反照率成幂函数关系,在极干或极湿情况下,地表温度与反照率成线性关系;收藏指正
7.Otherwise, six parameter of model outputs and medial parameters, including APAR, NPP, albedo, EET, LUE were produced as public production for users.
6个数据参数包括:N即、APAR、C、LUE(LightUtility EffiCienCy)、albedo和EET(EStimated Evapotranspiration)。收藏指正
8.The data resources and the methods for calculating important parameters in RTE, including optical thickness, phase function and single-scattering albedo, were completely discussed.
(5)就求解离散坐标法所用到的光学厚度、相函数和单次散射反照率等参数的来源及其计算方法进行了介绍。收藏指正
9.Land surface models, e. g. Biosphere Atmosphere Transfer Scheme(BATS), estimate albedo of trees over snow roughly with the parameters of roughness length, Z 0, and snow depth, d .
目前在地表模型 (如BATS模型 )中 ,是通过空气动力学粗糙度Z0 与降雪深度d两个参数来估计雪地上树冠的反照率的。收藏指正
10.Based on measured albedo data of dry snow cover in field,the numerical range of spectralalbedo in band 0.38- 3.2,0.38-0,7 and 0,7-3,2 is given.
据积雪反照率实测资料,分析了本区干积雪在0.38——0.7μ,0.7——3.2μ及0.38——3.2μ三个波段的光谱反照率的数值范围,讨论了太阳高度角、云及雪面污化等因素影响下的变化规律。收藏指正
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