Author Affiliations
1Anhui Meteorological Observatory, Key Lab. of Strong Weather Analysis and Forecast, Hefei 23003, China2Anhui Institute of Meteorological ,Anhui Key Lab. of Atmospheric Science and Satellite Remote Sensing, Hefei30031, China3Anhui Climate Center, Hefei 2001, Chinashow less
Fig. 1. Weight function of H8/AHI channel 7 to 16 based on RTTOV model
Fig. 2. Area Coverage of Anhui zone and Huaihe river basin
Fig. 3. Comparison of radiance characteristics for precipitation and non-precipitation FOVs, average brightness temperature of H8/AHI(left) and brightness temperature gradient (right)
Fig. 4. Probability density distribution of GPM precipitation (left) and mean changes of infrared spectral brightness temperature of H8/AHI in different precipitation grades(right)
Fig. 5. FOVs brightness temperature gradient of the non-precipitation and precipitation(left) and mean brightness temperature in different precipitation grades (right)
Fig. 6. Scatter distribution of the different channels between brightness temperatures of H8/AHI
Fig. 7. Optimized contribution rate of the brightness temperature of H8/AHI channel to objective function based on the BMA
Fig. 8. Distribution of retrieval precipitation of different BMA methods and GPM precipitation
Fig. 9. Scatter of H8/AHI retrieval precipitation of different historical sample dictionary, the GPM precipitation and PDF of precipitation difference
Fig. 10. Sequence changes of H8/AHI brightness temperature (left), retrieval precipitation (middle) and GPM precipitation (right)
通道 | 中心波长/µm | 探测目的 | 通道 | 中心波长/µm | 探测目的 |
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7 | 3.89 | 地表和云、晚雾、火和风 | 12 | 9.64 | 总臭氧、湍流和风 | 8 | 6.24 | 高层大气水汽、风和降雨 | 13 | 10.41 | 地表和云 | 9 | 6.94 | 中层大气水汽、风和降雨 | 14 | 11.24 | 海温、云和降雨 | 10 | 7.35 | 低层大气水汽、风和SO2 | 15 | 12.38 | 总水量、火山灰和海温 | 11 | 8.59 | 总水量、云相态、粉尘、SO2和降雨 | 16 | 13.28 | 气温、云高和云量 |
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Table 1. Himawari-8/AHI channel-specific central wavelengths and primary purpose
方法 | R | SSIM | NMI | PSNR | POD(%) | FAR(%) | CSI(%) |
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BMA-Gamma | 0.6787 | 0.7457 | 0.6788 | 18.2047 | 96.34 | 5.10 | 91.60 | BMA-Normal | 0.6529 | 0.7402 | 0.6858 | 17.8366 | 95.73 | 4.70 | 91.41 | BMA-Heteroscedastic | 0.6436 | 0.7376 | 0.6870 | 17.8252 | 95.70 | 4.75 | 91.34 |
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Table 2. Quantified index score of retrieval precipitation with different channel contribution rates
样本量 | R | SSIM | NMI | PSNR | POD(%) | FAR(%) | CSI(%) |
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07时 | 0.6037 | 0.7789 | 0.6503 | 16.9828 | 94.54 | 5.25 | 89.83 | 08时 | 0.6267 | 0.7382 | 0.7365 | 15.9193 | 92.07 | 4.16 | 88.53 | 07+08时 | 0.6357 | 0.7564 | 0.7002 | 16.4999 | 93.43 | 4.20 | 89.75 |
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Table 3. Results of quantitative index scoring for precipitation retrieval with different sample sizes