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六种遥感海表温度产品的比对分析

蒋兴伟 奚萌 宋清涛

蒋兴伟, 奚萌, 宋清涛. 六种遥感海表温度产品的比对分析[J]. 海洋学报, 2013, 35(4): 88-97. doi: 10.3969/j.issn.0253-4193.2013.04.011
引用本文: 蒋兴伟, 奚萌, 宋清涛. 六种遥感海表温度产品的比对分析[J]. 海洋学报, 2013, 35(4): 88-97. doi: 10.3969/j.issn.0253-4193.2013.04.011
JIANG Xingwei, XI Meng, SONG Qingtao. A comparison analysis of six sea surface temperature products[J]. Haiyang Xuebao, 2013, 35(4): 88-97. doi: 10.3969/j.issn.0253-4193.2013.04.011
Citation: JIANG Xingwei, XI Meng, SONG Qingtao. A comparison analysis of six sea surface temperature products[J]. Haiyang Xuebao, 2013, 35(4): 88-97. doi: 10.3969/j.issn.0253-4193.2013.04.011

六种遥感海表温度产品的比对分析

doi: 10.3969/j.issn.0253-4193.2013.04.011
基金项目: 国家重点基础研究发展计划项目“南海海气相互作用与海洋环流和涡旋演变规律(2011CB403501)”;国家自然科学基金面上项目“中国近海海洋锋面中小尺度海气相互作用及其机理研究(41076012)”;国家自然科学基金面上项目“大气对小尺度海表温度结构的响应(41276019)”。

A comparison analysis of six sea surface temperature products

  • 摘要: 海表温度(sea surface temperature, SST)产品是研究全球海洋大气系统的重要数据源, 在海洋相关领域的研究和应用方面具有重要价值。对2007年1和7月的六种不同SST产品(AVHRR-only, AMSR+AVHRR, NCODA, RSS, RTG-HR和OSTIA)在南大洋阿古拉斯回流(Agulhas Return Current, ARC)与绕极环流交汇区域的产品特性进行了比对统计分析, 包括SST分析、SST梯度分析、统计参数分析和波数谱分析。分析结果表明产品之间SST时空变化分布的整体趋势一致, RTG-HR在空间分布上过于平滑, OSTIA解析的大洋锋面最弱, RSS包含噪声较多, NCODA相对其他产品存在较大偏差。发现在AVHRR数据的覆盖率较好的情况下与以红外数据构建的AVHRR-only相比, AMSR数据并不能提供更多的SST信息, 反而会降低产品的空间解析能力。
  • Mmrtin S.海洋遥感导论[M]. 蒋兴伟译. 北京:海洋出版社, 2008.
    Reynolds R W, Chelton D B. Comparisons of daily sea surface temperature analyses for 2007-08[J]. American Meteorological Society, 2010, 23:3545-3562.
    Chelton D B, Schlax M G, Freilich M H, et al. Satellite measurements reveal persistent small-scale features in ocean winds[J]. Science, 2004, 303:978-983.
    Song Q, Hara T, Cornillon P, et al. A comparison between observations and MM5 simulations of the marine atmospheric boundary layer across a temperature front[J]. Journal of Atmospheric and Oceanic Technology, 2004, 21: 170-178.
    Song Q, Cornillon P, Hara T. Surface wind response to oceanic fronts[J]. Journal of Geophysical Research, 2006, 111: C12006, doi: 10.1029/2006JC003680.
    Small R J, Xie S P, Wang Y, et al. Numerical simulation of boundary layer structure and crossequatorial flow in the Eastern Pacific[J].J Atmos. Sci, 2005, 62:1812-1830.
    Reynolds R W, Smith T M, Liu C, et al. Daily high-resolution blended analyses for sea surface temperature[J]. J Climate, 2007, 20:5473-5496.
    蒋兴伟, 宋清涛. 海洋卫星微波遥感技术发展现状与展望[J]. 科技导报, 2010, 28(3): 105-111.
    Cummings J A. Operational multivariate ocean data assimilation[J].Quart J Roy Meteor Soc, 2005, 131: 3583-3604.
    Chelton D B, Wentz F J. Global microwave satellite observations of sea surface temperature for numerical weather prediction and climate research[J]. Bull Amer Meteor Soc, 2005, 86: 1097-1115.
    Gentemann C L, Donlon C J, Stuart-Menteth A, et al.Diurnal signals in satellite sea surface temperature measurements[J]. Geophys Res Lett, 2003, 30: 1140, doi: 10.1029/2002GL016291.
    Gemmill W, Katz K, Li X. Daily real-time global sea surface temperature-high resolution analysis at NOAA/NCEP. NOAA/NWS/NCEP/MMAB Office Note 260, 39. 2007.
    Thiebaux J, Rogers E, Wang W, et al. A new high resolution blended real-time global sea surface temperature analysis[J]. Bull Amer Meteor Soc, 2003, 84:645-656.
    Reynolds R W, Smith T M. Improved global sea surface temperature analyses using optimum interpolation[J]. J Climate, 1994, 7: 929-948.
    Reynolds R W, Gentemann C L, Corlett G K. Evaluation of AATSR and TMI satellite SST data[J]. J Climate, 2010, 23: 152-165.
    Yocky D A. Image merging and data fusion by means of the discrete two-dimensional wavelet transform[J]. Journal of Optical Society of America, 1995.12(9):1834-1841.
    Song Q, Chelton D B, Esbensen S K, et al. Coupling between sea surface temperature and low-level winds in mesoscale numerical models[J]. Journal of Climate, 2009, 22: 146-164
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出版历程
  • 收稿日期:  2012-05-03
  • 修回日期:  2013-03-05

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