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ISCCP产品和我国地面观测总云量差异

王旻燕 王伯民

王旻燕, 王伯民. ISCCP产品和我国地面观测总云量差异. 应用气象学报, 2009, 20(4): 411-418..
引用本文: 王旻燕, 王伯民. ISCCP产品和我国地面观测总云量差异. 应用气象学报, 2009, 20(4): 411-418.
Wang Minyan, Wang Bomin. Total cloud amount difference between ISCCP product and ground observation over China. J Appl Meteor Sci, 2009, 20(4): 411-418.
Citation: Wang Minyan, Wang Bomin. Total cloud amount difference between ISCCP product and ground observation over China. J Appl Meteor Sci, 2009, 20(4): 411-418.

ISCCP产品和我国地面观测总云量差异

资助项目: 

国家科技基础条件平台建设项目“气象科学数据共享中心” 2005DKA31700

国家自然科学基金项目 40605021

国家自然科学基金项目 40605011

Total Cloud Amount Difference Between ISCCP Product and Ground Observation over China

  • 摘要: 国际卫星云气候计划ISCCP是国际上较权威和客观的云气候性研究计划, 自1983年以来为研究全球云和辐射平衡、云水资源分布等提供了有价值的数据。在分析总云量卫星和地面两种观测方式差异的基础上, 研究了1984-2006年ISCCP D2产品和我国地面观测云资料数据集总云量空间及时间差异。尽管两套资料能一致揭示我国总云量的分布形势和气候变化特征, 但区域性差异仍比较明显。天基、地基数据可对比格点上, 全国平均而言总云量卫星观测结果比地面观测偏高8.46%, 华南地区差异最小、东北地区差异最大。气候变化趋势分析结果表明:近23年我国总云量呈减少趋势, ISCCP D2产品总云量每年减少速度为0.015%, 小于地面观测的总云量每年减少速度 (0.063%); 东北地区总云量缓慢增多, 而青藏高原、西北地区总云量减少。利用卫星和地面资料均以累积距平法检测出1984—2001年总云量减少、2002-2006年总云量显著增加。
  • 图  1  1984-2006年ISCCP D2产品总云量 (a) 和地面观测总云量 (b)(单位:%)

    Fig. 1  Total cloud amount of ISCCP D2 product (a) and ground observation (b) during 1984-2006(unit:%)

    图  2  比较2.5°×2.5°ISCCP D2产品和地面观测总云量的145个格点位置

    Fig. 2  Location of 145 grids to compare total cloud amount of 2.5°×2.5°ISCCP D2 product and ground observation

    图  3  1984-2006年ISCCP D2产品和地面观测格点总云量差 (单位:%)

    Fig. 3  Gridded total cloud amount difference between ISCCP D2 product and ground observation during 1984-2006(unit:%)

    图  4  1984-2006年各区域ISCCP D2产品和地面观测格点总云量多年变化

    Fig. 4  Inter-annual variation of grided total cloud amount of ISCCP D2 product and ground observation in the sub-regions during 1984-2006

    图  5  1984-2006年172个ISCCP D2格点和568个地面站点总云量多年变化 (a) 及总云量累积距平 (b)

    Fig. 5  Total cloud amount inter-annual variation of 172 ISCCP D2 grids and 568 stations (a) and their integral anomalies (b) during 1984-2006

    表  1  各区域范围、格点数、平均台站数及1984-2006年ISCCP D2产品和地面格点总云量

    Table  1  Scope of the sub-regions, grid number, average station number, grided total cloud amount of ISCCP D2 product, ground observation during 1984-2006

    表  2  各区域卫星和地面观测总云量多年变化相关情况

    Table  2  Relativity of total cloud inter-amount annual variation from satellite and ground observation results in the sub-regions

  • [1] Yu H, Kaufman Y J, Chin M, et al. A review of measurement-based as sessments of the aerosol direct radiative effect and forcing. Atmospheric Chemistry & Physics, 2006, 6: 613-666. https://www.researchgate.net/publication/29621094_A_review_of_measurement-based_assessments_of_the_aerosol_direct_radiative_effect_and_forcing
    [2] Stephens G S, Kummerow G D. The remote sensing of clouds and precipitation from space:A review. J Atmos Sci, 2007, 64(11):3742-3765. doi:  10.1175/2006JAS2375.1
    [3] Webb M J, Senior C A, Sexton D M H, et al. On the contribution of local feedback mechanisms to the range of climate sensitivity in two GCM ensembles. ClimateDynamics, 2006, 27:17-38. https://www.researchgate.net/publication/30846625_On_the_contribution_of_local_feedback_mechanisms_to_the_range_of_climate_sensitivity_in_two_GCM_ensembles
    [4] Ronald M Errico, George Ohring, Weng Fuzhong, et al. Assimilation of satellite cloud and precipitation observations in numerical weather prediction models:Introduction to the JAS special collection. J Atmos Sci, 2007, 64(11):3737-3741. doi:  10.1175/2007JAS2622.1
    [5] Schiffer R A, Rossow W B. The International Satellite Cloud Climatology Project (ISCCP):The First Project of the World Climate Research Programme. Bull Amer Meteor Soc, 1983, 64(7):779-784. https://www.mendeley.com/research-papers/international-satellite-cloud-climatology-project-isccp-first-project-world-climate-research-program/
    [6] Rossow W B, Walker A W, Garder L C. Comparison of ISCCP and other cloud amounts. J Climate, 1993, 6:2394-2418. doi:  10.1175/1520-0442(1993)006<2394:COIAOC>2.0.CO;2
    [7] Bryan C Weare. Near-global observations of low clouds. J Climate, 2000, 13(7):1255-1268. doi:  10.1175/1520-0442(2000)013<1255:NGOOLC>2.0.CO;2
    [8] Hahn Carole J, William B Rossow, Stephen G Warren. ISCCP cloud properties associated with standard cloud types identified in individual surface observations. J Climate, 2001, 14 (1):11-28. doi:  10.1175/1520-0442(2001)014<0011:ICPAWS>2.0.CO;2
    [9] Rossow W B, Garder L C. Cloud detection using satellite measurements of infrared and visible radiances for ISCCP. J Climate, 1993, 6:2341-2369. doi:  10.1175/1520-0442(1993)006<2341:CDUSMO>2.0.CO;2
    [10] Mokhov I I, Schlesinger M E. Analysis of global cloudiness 1. Comparison of Meteor, Nimbus 7, and International Satellite Cloud Climatology Project (ISCCP) satellite data. J Geophys Res Atmos, 1998(D7):12849-12868. doi:  10.1029/93JD00530/citedby
    [11] 魏丽, 钟强, 侯萍.中国大陆卫星反演云参数的评估.高原气象, 1996, 15(2):147-156. http://www.cnki.com.cn/Article/CJFDTOTAL-GYQX602.002.htm
    [12] 翁笃鸣, 韩爱梅.我国卫星总云量与地面总云量分布的对比分析.应用气象学报, 1998, 9(1):32-37. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=19980105&flag=1
    [13] 王可丽, 江灏, 陈世强.青藏高原地区的总云量—地面观测、卫星反演和同化资料的对比分析.高原气象, 2001, 20(3): 252-257. http://www.cnki.com.cn/Article/CJFDTOTAL-GYQX200103004.htm
    [14] 刘洪利, 朱文琴, 宜树华, 等.中国地区云的气候特征分析.气象学报, 2003, 61(4):465-473. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXB200304007.htm
    [15] 宜树华, 刘洪利, 李维亮, 等.中国西北地区云时空分布特征的初步分析.气象, 2003, 29(1):7-11. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXX200301001.htm
    [16] 丁守国, 石广玉, 赵春生.利用ISCCP D2资料分析近20年全球不同云类云量的变化及其对气候可能的影响.科学通报, 2004, 49(11):1105-1111. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200411016.htm
    [17] 刘瑞霞, 刘玉洁, 杜秉玉.中国云气候特征的分析.应用气象学报, 2004, 15(4):468-476. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=20040456&flag=1
    [18] Li Yunying, Yu Rucong, Xu Youping, et al. Spatial distribution and seasonal variation of cloud over China based on ISCCP data and surface observations. J Meteor Soc Japan, 2004, 82(2):761-773. doi:  10.2151/jmsj.2004.761
    [19] Chang F L, Li Z. A near-global climatology of single-layer and overlapped clouds and their optical properties retrieved from TE RRA/ MODIS data using a new algorithm. J Climate, 2005, 18: 4752-4771. doi:  10.1175/JCLI3553.1
    [20] Hahn C J, Warren S G, London J. The effect of moonlight on observation of cloud cover at night, and application to cloud climatology. J Climate, 1995(8):1429-1446. https://www.researchgate.net/publication/23843086_The_Effect_of_Moonlight_on_Observation_of_Cloud_Cover_at_Night_and_Application_to_Cloud_Climatology
    [21] Rossow W B, Schiffer R A. ISCCP cloud data products. Bull Amer Meteor Soc, 1991, 72(1):2-20. doi:  10.1175/1520-0477(1991)072<0002:ICDP>2.0.CO;2
    [22] 李晓文, 李维亮, 周秀骥.中国近30年太阳辐射状况研究.应用气象学报, 1998, 9(1):24-31. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=19980104&flag=1
    [23] Kaiser D P. Analysis of total cloud amount over China, 1951—1994. Geophys Res Let, 1998, 25:3599-3602. doi:  10.1029/98GL52784
    [24] Kaiser D P. Decreasing cloudiness over China:An updated analysis examining additional variables. Geophys Res Let, 2000, 27(15):2193-2196. doi:  10.1029/2000GL011358
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出版历程
  • 收稿日期:  2008-09-02
  • 修回日期:  2009-03-23
  • 刊出日期:  2009-08-31

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