Drought index construction method based on passive microwave remote sensing
A technology of passive microwave remote sensing and drought index, applied in the direction of electrical digital data processing, special data processing applications, instruments, etc., to achieve the effect of overcoming the influence of meteorological conditions
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Embodiment 1
[0037] Such as figure 1 As shown, a drought index construction method based on passive microwave remote sensing includes the following specific steps:
[0038] 1) Construct a diurnal mask and an intermonthly mask to eliminate the influence of mixed pixels of glaciers, snow cover and water bodies on AMSR-E data when inverting temperature;
[0039] 2) Construct a land surface temperature inversion model using AMSR-E's 10.8GHz and 89.0GHz vertical polarization channels Tb for inversion of land surface temperature, where Tb is brightness temperature data from passive microwave remote sensing;
[0040] 3) A microwave normalized difference vegetation index model was constructed based on the microwave polarization difference index (MPDI);
[0041] 4) Based on the established surface temperature inversion model and vegetation index model, construct the dry-edge and wet-edge equations of the MTVDI model;
[0042] 5) Establish the MTVDI model to simulate and monitor the monthly drough...
Embodiment 2
[0067] Such as Figure 6 As shown, the microwave vegetation drought index model takes 2010 as an example to analyze the annual spatio-temporal variation of the M-TVDI results. The results showed that during the period from October to March, the drought mainly occurred in the south China area of Yunnan, Guangxi and Guangdong. The drought in South China eased from April to September, reaching the lowest point of drought intensity in June. In northern China, the drought mainly occurs in the Inner Mongolia-Xinjiang area from April to September. The reason may be that the period from April to September is the rainy season in southern China, and the abundant precipitation effectively slows down the drought; however, due to the rising temperature and low precipitation in the northern Xinjiang and Inner Mongolia areas at this time, the surface evaporation is strong, resulting in Drought is more severe.
[0068] Such as Figure 7 As shown, in order to further understand the tempo...
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