• Journal of Infrared and Millimeter Waves
  • Vol. 40, Issue 3, 391 (2021)
Bei-Bei ZHANG1、2, Ning WANG1、*, Wei-Yuan YAO1、**, Yong-Gang QIAN1, Ling-Ling MA1, Chuan-Rong LI1, Ling-Li TANG1, Yao-Kai LIU1, and Cai-Xia GAO1
Author Affiliations
  • 1Key Laboratory of Quantitative Remote Sensing Information Technology, Aerospace Information Research Institute, Chinese Academy of Sciences, Beijing 100094, China
  • 2School of Electronic, Electrical and Communication Engineering, University of Chinese Academy of Sciences, Beijing 100049, China
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    DOI: 10.11972/j.issn.1001-9014.2021.03.016 Cite this Article
    Bei-Bei ZHANG, Ning WANG, Wei-Yuan YAO, Yong-Gang QIAN, Ling-Ling MA, Chuan-Rong LI, Ling-Li TANG, Yao-Kai LIU, Cai-Xia GAO. Channel selection for carbon monoxide retrievals based on ultra-spectral thermal infrared data[J]. Journal of Infrared and Millimeter Waves, 2021, 40(3): 391 Copy Citation Text show less
    China's regional annual average distribution of CO columns from March 2000 to February 2009[20]
    Fig. 1. China's regional annual average distribution of CO columns from March 2000 to February 200920
    Channel sensitivities to CO2, H2O, N2O, O3, CO, CH4, NO, NO2, and SO2 at the 4.67 μm band
    Fig. 2. Channel sensitivities to CO2, H2O, N2O, O3, CO, CH4, NO, NO2, and SO2 at the 4.67 μm band
    The distributions of the 300 channels in the spectrum of CO brightness temperature change selected by analyzing the STI ratio(STI>1) for the air masses of Beijing-Tianjin area in winter
    Fig. 3. The distributions of the 300 channels in the spectrum of CO brightness temperature change selected by analyzing the STI ratio(STI>1) for the air masses of Beijing-Tianjin area in winter
    Jacobians of the initial channel group for the air masses of Beijing-Tianjin area in winter
    Fig. 4. Jacobians of the initial channel group for the air masses of Beijing-Tianjin area in winter
    Jacobians of the channel at the top and bottom of characteristic peak of the CO brightness temperature change spectrum among the initial channel group for the air masses of Beijing-Tianjin area in winter
    Fig. 5. Jacobians of the channel at the top and bottom of characteristic peak of the CO brightness temperature change spectrum among the initial channel group for the air masses of Beijing-Tianjin area in winter
    Schematic diagram of channel selection from the initial channel group at the peak of the CO brightness temperature change spectrum(a)three channels(b)four channels
    Fig. 6. Schematic diagram of channel selection from the initial channel group at the peak of the CO brightness temperature change spectrum(a)three channels(b)four channels
    The distribution in the CO brightness temperature change spectrum of the channels selected by the Peak sampling channel selection method for the air masses of four regions in(a)winter and(b)summer.
    Fig. 7. The distribution in the CO brightness temperature change spectrum of the channels selected by the Peak sampling channel selection method for the air masses of four regions in(a)winter and(b)summer.
    The RMSEs of the retrieved CO profiles by the Peak sampling channel set, OSP channel set and all 4001-channel set for the winter air masses in(a)Beijing-Tianjin(b)Alxa(c)Yangtze River Delta(d)Pearl River Delta
    Fig. 8. The RMSEs of the retrieved CO profiles by the Peak sampling channel set, OSP channel set and all 4001-channel set for the winter air masses in(a)Beijing-Tianjin(b)Alxa(c)Yangtze River Delta(d)Pearl River Delta
    The RMSEs of the retrieved CO profiles by the Peak sampling channel set, OSP channel set and all 4001-channel set for the summer air masses in(a)Beijing-Tianjin(b)Alxa(c)Yangtze River Delta(d)Pearl River Delta
    Fig. 9. The RMSEs of the retrieved CO profiles by the Peak sampling channel set, OSP channel set and all 4001-channel set for the summer air masses in(a)Beijing-Tianjin(b)Alxa(c)Yangtze River Delta(d)Pearl River Delta
    The biases of the retrieved CO profiles by the Peak sampling channel set and OSP channel set for the winter air masses in(a)Beijing-Tianjin(b)Alxa(c)Yangtze River Delta(d)Pearl River Delta
    Fig. 10. The biases of the retrieved CO profiles by the Peak sampling channel set and OSP channel set for the winter air masses in(a)Beijing-Tianjin(b)Alxa(c)Yangtze River Delta(d)Pearl River Delta
    地区方法RMSE(10-8g/g)
    冬季夏季
    北京-天津所有通道3.151.09
    OSP3.231.07
    峰采样3.071.07
    阿拉善所有通道0.430.25
    OSP0.440.25
    峰采样0.410.24
    长江三角洲所有通道2.620.36
    OSP2.650.33
    峰采样2.510.34
    珠江三角洲所有通道2.230.37
    OSP2.210.09
    峰采样2.100.06
    Table 1. The RMSEs of the retrieved CO profiles for the simulated ultra-spectral infrared data from the air masses of four regions in winter and summer with different channel sets
    Bei-Bei ZHANG, Ning WANG, Wei-Yuan YAO, Yong-Gang QIAN, Ling-Ling MA, Chuan-Rong LI, Ling-Li TANG, Yao-Kai LIU, Cai-Xia GAO. Channel selection for carbon monoxide retrievals based on ultra-spectral thermal infrared data[J]. Journal of Infrared and Millimeter Waves, 2021, 40(3): 391
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