It is proved that the theoretical results are in good agreement with the experiment data within the range of data ' s uncertainty 模拟结果表明，铁球壳外表面各测点处的中子活化反应率及反照系数在实验数据不确定度范围内符合。
The cause is that there are large distribution areas of moistly soil , wetly lands , and vegetative land , and smaller area of snow on the plateau 高原反照率年变化的主要原因是土壤含水量、雪盖分布面积及植被覆盖度的变化。
The results show good performance between vis , irl , sun zenith and net surface radiation . the correlation coefficient is up to 0 . 8259 通过理论部分推导出的关系可以看出：地面净辐射与太阳天顶角、地面及云面反照率等因子有关。
The simulated latent heat of coarse soil is smaller , and surface temperature and sensible heat is larger than the results of the control run 粗糙土壤，反照率大，造成地面吸收短波辐射减少。粗糙土壤用于蒸发的潜热减少，地温升高，感热大。
Human minds are not strange sports of a purposeless process of evolution - they are offshoots , or reflections , or " fulgurations " of the creative mind 人类的心灵不是一个没有目标的只是进化所得出的怪物? ?他们是“创始心灵”的分枝、反照或“闪光” 。
But we all , with open face beholding as in a glass the glory of the lord , are changed into the same image from glory to glory , even as by the spirit of the lord 18我们众人既然倘着脸，得以看见主的荣光，好像从镜子里反照，就变成主的形状，荣上加荣，如同从主的灵变成的。
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。
18 and we , who with unveiled faces all reflect [ 1 ] the lord ' s glory , are being transformed into his likeness with ever - increasing glory , which comes from the lord , who is the spirit 18我们众人既然敞著脸得以看见主的荣光，好像从镜子里反照，就变成主的形状，荣上加荣，如同从主的灵变成的。
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。
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。
