[1] HUANG L, JIANG J H, WANG Z, et al. Climatology of cloud water content associated with different cloud types observed by A-Train satellites[J]. Journal of Geophysical Research: Atmospheres, 2015, 120(9): 4196-4212. [2] LIU D, LIU Q, QI L, et al. Oceanic single-layer warm clouds missed by the Cloud Profiling Radar as inferred from MODIS and CALIOP measurements[J]. Journal of Geophysical Research:Atmospheres,2016,121(21): 12947-12965. [3] BAKER M B. Cloud microphysics and climate[J]. Science, 276(5315): 1072-1078. [4] 周毓荃, 欧建军. 利用探空数据分析云垂直结构的方法及其应用研究[J]. 气象, 2010, 35(11):50-58. [5] ZHANG J, LI Z, CHEN H, et al. Cloud vertical distribution from radiosonde, remote sensing, and model simulations[J]. Climate Dynamics, 2014, 43:1129-1140. [6] ZENG S, RIEDI J, TREPTE C R, et al. Study of global cloud droplet number concentration with A-Train satellites[J]. Atmospheric Chemistry and Physics, 2014, 14(14): 7125-7134. [7] HU Y, VAUGHAN M, MCCLAIN C, et al. Global statistics of liquid water content and effective number concentration of water clouds over ocean derived from combined CALIPSO and MODIS measurements[J]. Atmospheric Chemistry and Physics, 2007, 7(12): 3353-3359. [8] 周天, 黄忠伟, 黄建平, 等. 黄土高原地区云垂直结构的激光雷达遥感研究[J]. 干旱气象, 2013, 31(2): 246-253. [9] 段皓, 刘煜. 近20年中国地区云量变化趋势[J]. 气象科技, 2011, 39(3): 280-288. [10] NAKAJIMA T Y, SUZUKI K, STEPHENS G L. Droplet growth in warm water clouds observed by the A-Train. Part I: Sensitivity analysis of the MODIS-derived cloud droplet sizes[J]. Journal of the Atmospheric Sciences, 2010, 67(6): 1884-1896. [11] 谢磊, 刘奇. 基于卫星遥感的全球洋面降水暖云与非降水暖云的云参数差异[J]. 中国科学技术大学学报, 2017, 47(12):1006-1014. [12] COSTANTINO L, BRéON F M. Aerosol indirect effect on warm clouds over South-East Atlantic, from co-located MODIS and CALIPSO observations[J]. Atmospheric Chemistry and Physics, 2013, 13(1): 69-88. [13] WEISZ E, LI J, MENZEL W P, et al. Comparison of AIRS, MODIS, CloudSat and CALIPSO cloud top height retrievals[J]. Geophysical Research Letters, 2007, 34:L17811. [14] IM E, WU C, DURDEN S L. Cloud profiling radar for the CloudSat mission[J]. IEEE Aerospace and Electronic Systems Magazine, 2005, 20(10): 15-18. [15] KATO S, ROSE F G, SUN-MACK S, et al. Improvements of top-of-atmosphere and surface irradiance computations with CALIPSO-, CloudSat-, and MODIS-derived cloud and aerosol properties[J]. Journal of Geophysical Research: Atmospheres, 2011, 116:D19209. [16] CHAN M A, COMISO J C. Arctic cloud characteristcs as derived from MODIS, CALIPSO, and CloudSat[J]. Journal of Climate, 2013, 26(10): 3285-3306. [17] NAKAJIMA T Y, SUZUKI K, STEPHENS G L. Droplet growth in warm water clouds observed by the A-Train. Part II: A multisensor view[J]. Journal of the Atmospheric Sciences, 2010, 67(6): 1897-1907. [18] MASSIE S T, DELANO J, BARDEEN C G, et al. Changes in the shape of cloud ice water content vertical structure due to aerosol variations[J]. Atmospheric Chemistry and Physics, 2016, 16(10): 6091-6105. [19] 赵姝慧, 班显秀, 袁健, 等. 8,9月沈阳地区卫星观测云垂直结构的气候特征分析[J]. 高原气象, 2014, 33(6):1640-1647. [20] 安洁. 基于CloudSat资料的东海及周边云层垂直分布特征[J]. 海洋预报, 2018, 35(5):60-73. [21] CHAI Q M, WANG W C, HUANG Z W. Analyzing the cloud micro-and macro-physical properties of the cyclone eye wall and its surrounding spiral cloud bands based on CloudSat and TRMM data[J]. Journal of Tropical Meteorology, 2018, 24(2): 253-262. [22] 尚博, 周毓荃, 刘建朝, 等. 基于Cloudsat的降水云和非降水云垂直特征[J]. 应用气象学报, 2012, 23(1):1-9. [23] SUZUKI K, STEPHENS G L. Global identification of warm cloud microphysical processes with combined use of A-Train observations[J]. Geophysical Research Letters, 2008, 35(8):L08805. [24] DE SZOEKE S P, VERLINDEN K L, COVERT D. Cloud-scale droplet number sensitivity to liquid water path in marine stratocumulus[J]. Journal of Geophysical Research: Atmospheres, 2018,123(10):5320-5334. [25] STEPHENS G L, VANE D G, BOAIN R J, et al. The CloudSat mission and the A-Train: A new dimension of space-based observations of clouds and precipitation[J]. Bulletin of the American Meteorological Society, 2002, 83(12): 1771-1790. [26] MARCHAND R, MACE G G, ACKERMAN T, et al. Hydrometeor detection using Cloudsat-An earthorbiting 94-GHz cloud radar[J]. Journal of Atmospheric and Oceanic Technology, 2008, 25: 519-533. [27] WOOD N. Level 2B radar-visible optical depth cloud water content (2B-CWC-RVOD) process description document[J]. Version, 2008, 5: 1-26.
() () |