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利用高频天波返回散射反演台风中心和风速

鲁转侠 李雪 李吉宁 华彩成 吕哲

鲁转侠, 李雪, 李吉宁, 华彩成, 吕哲. 利用高频天波返回散射反演台风中心和风速[J]. 空间科学学报, 2018, 38(4): 508-516. doi: 10.11728/cjss2018.04.508
引用本文: 鲁转侠, 李雪, 李吉宁, 华彩成, 吕哲. 利用高频天波返回散射反演台风中心和风速[J]. 空间科学学报, 2018, 38(4): 508-516. doi: 10.11728/cjss2018.04.508
LU Zhuanxia, LI Xue, LI Jining, HUA Caicheng, LÜ Zhe. Reconstruction of the Typhoon Center and Wind Speed Distribution Using HF Sky-wave Backscatter Spectrumormalsize[J]. Chinese Journal of Space Science, 2018, 38(4): 508-516. doi: 10.11728/cjss2018.04.508
Citation: LU Zhuanxia, LI Xue, LI Jining, HUA Caicheng, LÜ Zhe. Reconstruction of the Typhoon Center and Wind Speed Distribution Using HF Sky-wave Backscatter Spectrumormalsize[J]. Chinese Journal of Space Science, 2018, 38(4): 508-516. doi: 10.11728/cjss2018.04.508

利用高频天波返回散射反演台风中心和风速

doi: 10.11728/cjss2018.04.508
基金项目: 

国家海洋局海洋遥测工程技术研究中心创新青年基金项目和2016年环渤海区域科技协同创新基金项目(QYXM201606)共同资助

详细信息
    作者简介:

    鲁转侠,E-mail:zhuanxialu@163.com

  • 中图分类号: P352

Reconstruction of the Typhoon Center and Wind Speed Distribution Using HF Sky-wave Backscatter Spectrumormalsize

  • 摘要: 通过分析高频天波返回散射地(海)杂波频谱分布特性,构建三谱滤波器模型,实现多类型频谱中一阶海杂波峰值比的提取,结果与实测数据吻合较好.基于台风中心与区域一阶海杂波峰值比相关性分析,结合后向差分法,有效确定了台风中心,结果与气象部门发布数据趋势上基本一致,平均绝对误差约38km.使用修正经验模型法初步开展了台风中心最大风速和台风中心附近的风速反演,结果与气象部门发布数据分布基本一致.研究结果表明高频天波返回散射探测对大范围、远距离海态监测具有重要意义.

     

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出版历程
  • 收稿日期:  2017-07-11
  • 修回日期:  2017-11-27
  • 刊出日期:  2018-07-15

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