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首先把显热通量作为地表能量平衡的一部分,通过每半小时平均净辐射、潜热通量和土壤热通量的观测值来计算显热通量。然后,采用迭代法解显热通量的空气动力方程,并且考虑到非流线体(热量和动量交换粗糙高度的不同)和稳定度(地表和空气温度的不同)对空气动力阻力的校正,得到空气动力地表温度。这时会发现,在稳定(不稳定)大气条件下的空气动力温度比红外测温观测值要低(高)。而且,在阻力-能量平衡方程中用红外温度估算潜热通量时,这个估算值与观测值,通过回归分析,显示出高度的线性相关(r=0.96)与适中的标准差(47Wm~(-2)) 相似文献
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The NOAA is a special meteorological satellite. The first and second channels of the AVHRP (the sensor of NOAA) are much similar to the fifth and seventh channels of the resource satellite MSS, and their corresponding spectral response curves are much alike. The AVHRR'S first channel has a higher reflectivity from soil, and the second channel is highly reflected by vegetation. By virtue of its wide sensitivity range, multiple reception orbitals, economical and convenient, it has been used in the W.S.A. in the agricultural estimation.According to the characteristic spectra from the vegetation, and through the digital exchange of the measuraed values on the first and second channels of the NOAA/AVHRR, We established a servies of green models which can be need in making agricultural estimation satisfactorily.As expesimentally showed that these green models highly correlated to the yeild of crops. This has been presently becoming the main information sources for yield estiraatings. With the forecast of the 相似文献
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