PDF下载 分享
[1]韦成强,赵鹏国.青藏高原及其临近区域云特性及云垂直结构分布特征[J].成都信息工程大学学报,2025,40(05):643-651.[doi:10.16836/j.cnki.jcuit.2025.05.011]
 WEI Chengqiang,ZHAO Pengguo.Cloud Macrophysical and Microphysical Properties and Vertical Structure Distribution Characteristics over the Tibetan Plateau and its Adjacent Regions[J].Journal of Chengdu University of Information Technology,2025,40(05):643-651.[doi:10.16836/j.cnki.jcuit.2025.05.011]
点击复制

青藏高原及其临近区域云特性及云垂直结构分布特征

参考文献/References:

[1] King M D,Platnick S,Menzel W P,et al.Spatial and temporal distribution of clouds observed by MODIS onboard the Terra and Aqua satellites[J]. IEEE transactionson geoscience and remote sensing,2013,51(7):3826-3852.
[2] Surface Coatings International,Part A.Coatings Journal Group.Climate Change Second IPCC report published[J]. Surface Coatings International,Part A.Coatings Journal:JOCCA Journal of the Oil & Colour Chemists’ Association,2022(2):105.
[3] Wu G,Liu Y,Zhang Q,et al.The influence of mechanical and thermalforcing by the Tibetan Plateau on Asian climate[J]. Journal of Hydrometeorology,2007,8(4):770-789.
[4] Ye D Z,Wu G X.The role of the heat source of the Tibetan Plateau in the general circulation[J]. Meteorology and Atmospheric Physics,1998,67:181-198.
[5] 周思儒,信忠保.近20年青藏高原水资源时空变化[J]. 长江科学院院报,2022,39(6):31-39.
[6] 王慧,张璐,石兴东,等.2000年后青藏高原区域气候的一些新变化[J]. 地球科学进展,2021,36(8):785-796.
[7] 马耀明,胡泽勇,王宾宾,等.青藏高原多圈层地气相互作用过程研究进展和回顾[J]. 高原气象,2021,40(6):1241-1262.
[8] 范思睿,王维佳,林丹.基于ISCCP云资料的中国地区不同类型云的时空分布[J]. 干旱气象,2020,38(2):213-225.
[9] 余忠水,陈华,德吉白玛,等.基于ERA-Interim的青藏高原近40年云量的时空分布特征[J]. 山地学报,2022,40(6):811-822.
[10] 汪会,罗亚丽,张人禾.用CloudSat/CALIPSO资料分析亚洲季风区和青藏高原地区云的季节变化特征[J]. 大气科学,2011,35(6):1117-1131.
[11] Li Y,Yu R,Xu Y,et al.Spatial distribution and seasonal variation of cloud over China based on ISCCP data and surface observations[J]. Journal of the Meteorological Society of Japan.Ser.II,2004,82(2):761-773.
[12] Jin X,Wu T,Li L,et al.Cloudiness characteristics over Southeast Asia from satellite FY-2C and their comparison to three other cloud data sets[J]. Journal of Geophysical Research:Atmospheres,2009,114(D17).
[13] Eck T F,Holben B N,Reid J S,et al.Fog-and cloud-induced aerosol modification observed by the Aerosol Robotic Network(AERONET)[J]. Journal of Geophysical Research:Atmospheres,2012,117(D7).
[14] Sharma S,Dass A,Mishra A K,et al.A decadal climatology of cloud vertical structure over the Indo-Gangetic Plain using radiosonde and radar observations[J]. Atmospheric Research,2022,266:105949.
[15] Lal D M,Patil S D,Singh H N,et al.Influence of aerosol on clouds over the Indo-Gangetic Plain,India[J]. Climate dynamics,2013,41:601-612.
[16] 位晶,段克勤,辛蕊.青藏高原地区云出现概率及其辐射强迫变化特征[J]. 冰川冻土,2020,42(2):368-377.
[17] 李霖.青藏高原云水资源时空变化及降水效率评估[D]. 兰州:西北师范大学,2023.
[18] Zhao P,Xiao H,Liu J,et al.Precipitation efficiency of cloud and itsinfluencing factors over the Tibetan plateau[J]. International Journal of Climatology,2022,42(1):416-434.
[19] 陈玲,周筠珺.青藏高原和四川盆地夏季降水云物理特性差异[J]. 高原气象,2015,34(3):621-632.
[20] 范思睿,王维佳,刘贵华,等.基于NPP卫星反演四川盆地夏季云降水微物理特征[J]. 成都信息工程大学学报,2021,36(4):467-471.
[21] 陈逸豪,范广洲.春季地表云辐射效应与7月高原低涡之间的联系[J]. 高原气象,2022,41(5):1266-1280.
[22] Zhu J,Xia X,Che H,et al.Spatiotemporal variation of aerosol and potential long-range transport impact over the Tibetan Plateau,China[J]. Atmospheric Chemistry and Physics,2019,19(23):14637-14656.
[23] Srivastava A K,Tiwari S,Devara P C S,et al.Pre-monsoon aerosol characteristics over the Indo-Gangetic Basin:implications to climatic impact[J]. Annales Geophysicae.Göttingen,Germany:Copernicus Publications,2011,29(5):789-804.
[24] Fan H,Zhao C,Yang Y.A comprehensive analysis of the spatio-temporal variation of urban air pollution in China during 2014-2018[J]. Atmospheric Environment,2020,220:117066.
[25] Giles D M,Holben B N,Tripathi S N,et al.Aerosol properties over the Indo-Gangetic Plain:A mesoscale perspective from the TIGERZ experiment[J]. Journal of Geophysical Research:Atmospheres,2011,116(D18).
[26] 冯晓,蔡宏珂,陈权亮,等.基于CALIOP资料的中国及周边地区云出现概率时空分布特征分析[J]. 西南大学学报(自然科学版),2018,40(7):133-143.
[27] Karlsson K G,Anttila K,Trentmann J,et al.CLARA-A2:the second edition of the CM SAF cloud and radiation data record from 34 years of global AVHRR data[J]. Atmospheric Chemistry and Physics,2017,17(9):5809-5828.
[28] Karlsson K G,Devasthale A.Inter-comparison and evaluation of the four longest satellite-derived cloud climate data records:CLARA-A2,ESACloud CCI V3,ISCCP-HGM,and PATMOS-x[J]. Remote Sensing,2018,10(10):1567.
[29] Tzallas V,Hatzianastassiou N,Benas N,et al.Evaluation of CLARA-A2 and ISCCP-H cloud cover climate data records over Europe with ECA&D ground-based measurements[J]. Remote Sensing,2019,11(2):212.
[30] Kummerow C,Olson W S,Giglio L.A simplified scheme for obtainingprecipitation and vertical hydrometeor profiles from passive microwave sensors[J]. IEEE Transactions on Geoscience and Remote Sensing,1996,34(5):1213-1232.
[31] Kummerow C,Hong Y,Olson W S,et al.The evolution of the Goddard Profiling Algorithm(GPROF)for rainfall estimation from passive microwave sensors[J]. Journal of Applied Meteorology,2001,40(11):1801-1820.
[32] 华珊.青藏高原气溶胶-云相互作用及云辐射效应研究[D]. 兰州:兰州大学,2020.
[33] Hua S,Liu Y,Jia R,et al.Role of clouds in accelerating cold-season warming during 2000-2015 over the Tibetan Plateau[J]. International Journal of Climatology,2018,38(13):4950-4966.

备注/Memo

收稿日期:2024-01-22
基金项目:国家自然科学基金资助项目(42075086、41905126)
通信作者:赵鹏国.E-mail:zpg@cuit.edu.cn

更新日期/Last Update: 2025-10-31