[1] Rossow W B, Schiffer R A. Advances in understanding clouds from ISCCP[J]. Bulletin of the American Meteorological Society, 1999, 80(11):2261-2287[2] Kuze A, Chance K V. Analysis of cloud top height and cloud coverage from satellites using the O2 A and B bands[J]. Journal of Geophysical Research: Atmospheres, 1994, 99(D7):14481-14491[3] Loyola D, Ruppert T. A new PMD cloud-recognition algorithm for GOME[J]. ESA Earth Observation Quarterly, 1998, 58: 45-47. [4] Koelemeijer R B A, Stammes P, Hovenier J W, et al. Global distributions of effective cloud fraction and cloud top pressure derived from oxygen A band spectra measured the Global Ozone Monitoring Experiment: Comparison to ISCCP data[J]. Journal of Geophysical Research, 2002, 107(D12): 4151.[5] Fournier N, Stammes P, de Graaf M, et al. Improving cloud information over deserts from SCIAMACHY Oxygen A-band measurements [J]. Atmospheric Chemistry and Physics, 2006, 6:163–172.[6] Wang P, Stammes P, van der A R, et al. FRESCO+: an improved O2 A-band cloud retrieval algorithm for tropospheric trace gas retrievals[J]. Atmospheric Chemistry and Physics, 2008, 8: 6565-6576.[7] Wang P, Stammes P. Evaluation of SCIAMACHY Oxygen A band cloud heights using Cloudnet measurements[J]. Atmospheric Measurement Techniques, 2014, 7: 1331-2014.[8] Loyola D, Thomas W, Livschitz Y, et al. Cloud properties derived from GOME/ERS-2 backscatter data for trace gas retrieval [J]. IEEE Transactions on Geoscience and Remote Sensing, 2007, 45(9): 2747–2758.[9] Rozanov V V. Semianalytical cloud retrieval algorithm as applied to the cloud top altitude and die cloud geometrical thickness determination from top-of-atmosphere reflectance measurements in the oxygen A band[J]. Journal of Geophysical Research: Atmospheres, 2004, 109(D5):1-21.[10] Acarreta J R, De Haan J F, Stammes P. Cloud pressure retrieval using the O4 absorption band at 477 nm[J], Journal of Geophysical Research:Atmospheres, 2004,109(D5):1-11.[11] Joiner J, Vasilkov A P, Flittner D E, et al. Retrieval of cloud pressure and chlorophyll content using Raman scattering in GOME ultraviolet spectra[J]. Journal of Geophysical Research:Atmospheres, 2004, 109(D1): 1-13.[12] Veefkind J P, de Haan J F, Sneep M, et al. Improvements to the OMI operational cloud algorithm and comparisons with ground-based radar-lidar observations[J]. Atmospheric Measurement Techniques, 2016, 9(12): 6035-6049.[13] Loyola D G, Gimeno García S, Lutz R, et al. The operational cloud retrieval algorithms from TROPOMI on board Sentinel-5 Precursor[J]. Atmospheric Measurement Techniques, 2018, 11: 409-427.[14] Loyola D, Lutz R, Argyrouli A, et al. S5P/TROPOMI ATBD Cloud Products [EB/OL]. (2018-04-30) [2019-11-25]https://sentinels.copernicus.eu/documents/247904/2476257/Sentinel-5P-TROPOMI-ATBD-Clouds.[15] Zhao M J, Si F Q, Zhou H J, et al. Preflight calibration of the Chinese Environmental Trace Gases Monitoring Instrument (EMI)[J]. Atmospheric Measurement Techniques, 2018, 11: 5403–5419.[16] Yang Taiping, Si Fuqi, PingWang, et al. Research on Cloud Fraction Inversion Algorithm of Environmental Trace Gas Monitoring Instrument [J]. Acta Optica Sinica, 2020, 40(9): 0901001 (in Chinese)杨太平, 司福祺, PingWang, 等. 大气痕量气体差分吸收光谱仪云量反演算法研究[J]. 光学学报, 2020, 40(9): 0901001 |