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卫星遥感业务系统海表温度误差控制方法

毛志华 朱乾坤 潘德炉

毛志华, 朱乾坤, 潘德炉. 卫星遥感业务系统海表温度误差控制方法[J]. 海洋学报, 2003, 25(5): 49-57.
引用本文: 毛志华, 朱乾坤, 潘德炉. 卫星遥感业务系统海表温度误差控制方法[J]. 海洋学报, 2003, 25(5): 49-57.
MAO Zhi-hua, ZHU Qian-kun, PAN De-lu. A temperature error control technology for an operational satellite application system[J]. Haiyang Xuebao, 2003, 25(5): 49-57.
Citation: MAO Zhi-hua, ZHU Qian-kun, PAN De-lu. A temperature error control technology for an operational satellite application system[J]. Haiyang Xuebao, 2003, 25(5): 49-57.

卫星遥感业务系统海表温度误差控制方法

基金项目: 国家"863"计划海洋监测主题资助项目(818-11-02;2002AA639220;2001AA630701);国家自然科学基金资助项目(40006011);国家重点基础研究发展规划资助项目(G1999043701).

A temperature error control technology for an operational satellite application system

  • 摘要: 提高卫星遥感海表温度的反演精度是各种反演模型追求的目标,也是遥感系统业务化应用的关键.据相关文献报道,在晴空无云的条件下遥感海表温度的精度达到了0.5℃,但考虑到影响海表温度反演精度的多种因素,在遥感业务系统真正实现SST精度在1℃以内是非常困难的.在北太平洋渔场速报制作系统中,对遥感海表温度与船测温度误差统计显示均方根误差达到5.71℃,匹配点误差分布显示存在大量较大的负误差值,最大的为-17.2℃,遥感温度图也反映出存在片状温度低值区,这些区域很可能被错误地当作冷涡或冷锋区,严重干扰渔情分析,这些异常的温度误差很难通过海表温度反演模式和云检测技术来消除.采用一种标准海表温度参考图用于温度误差控制技术,可有效地检测温度反演异常值,将均方根值从5.71℃降低到1.75℃,如果采用2℃阈值控制计算均方根值,则海表温度精度达到0.785℃.该方法基本消除了遥感海表温度的低值现象,明显提高了遥感海表温度的精度,并已成功地应用于北太平洋渔区的海况速报产品制作中.
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    MCMILLIN L M, CROSBY D S. Theory and validation of the multiple window sea surface temperature technique[J]. J Geophys Res, 1984, 89:3 655-3 661.
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    高郭平,钱成春,鲍献文,等.中国东部海域卫星遥感PFSST和现场观测资料的差异[J].海洋学报,2001,23(4):121-126.
    SIMPSON J J, MCINTIRE T J, STITT J R, et al. Improved cloud detecting in AVHRR daytime and night-time scenes over the ocean[J]. Int J Remote Sensing, 2001,22:2 585-2 615.
    KUMAR A, MINNETT P J, PODESTA G, et al. Error characteristics of the atmospheric correction algorithms used in retrieval of sea surface temperatures from infrared satellite measurements: global and regional aspects[J]. J Atmos Science,2001,60: 575-585.
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出版历程
  • 收稿日期:  2002-11-22
  • 修回日期:  2003-04-30

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