A method and device for estimating instantaneous surface emissivity by passive microwave remote sensing
A passive microwave remote sensing and surface emissivity technology, which is applied in the field of remote sensing data geoscience parameter inversion, can solve problems such as difficulty and inversion error of land surface parameterization, and achieve the effect of fast data collection and accurate image resolution.
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Embodiment 1
[0124] Embodiment one, the embodiment of the present invention selects two places in China to carry out the emissivity estimation test of 10.7GHz and 18.7GHz, and the surface coverage in the test area is mainly grassland (southeast region of the Qinghai-Tibet Plateau) and crops (central part of China), using The tested instantaneous surface emissivity distribution map (12-08-2006 ascending orbit), using these two areas to test the predictive ability of PR and MPDI emissivity. The data format is EASE-GRID (Equal-Area Scalable EarthGrid) grid.
[0125] On August 12, 2008, the effective launch rate sampling points were 505 and 157 points respectively. The emissivity prediction equations of Equations 4.15 (quadratic polynomial) and 4.16 (multiple / univariate linear regression) were established using both PR and MPDI polarization parameters. Table 1 shows the root mean square error (RMSE) of the emissivity obtained by the equation and its horizontally polarized emissivity. It can ...
Embodiment 2
[0134] Embodiment 2, the result of calculating the global surface emissivity at 36.5 GHz vertical and polarized emissivity by using the above method. The results show the expected spatial structure. The V polarization is greater than the H polarization, which is in line with the description of the model. The polarization difference in ice and snow-covered areas, such as the Antarctic continent and the ice and snow surface of Greenland, is due to the scattering on the ice and snow surface. The effect of the effect. The same phenomenon is shown in desert and semi-arid regions. The Qinghai-Tibet Plateau has low emissivity in both polarizations, and the same phenomenon also occurs in deserts and semi-arid regions, such as the Sahara Desert and central Australia.
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