大气与环境光学学报 ›› 2024, Vol. 19 ›› Issue (3): 371-381.

• 光学遥感 • 上一篇    下一篇

基于CALIOP双波长数据的海面测风信号筛选方法研究

罗敦艺 1, 吴东 1,2*, 贺岩 3   

  1. 1 中国海洋大学信息科学与工程学部海洋技术学院, 山东 青岛 266100; 2 青岛海洋科学与技术试点国家实验室区域海洋动力学与数值模拟功能实验室, 山东 青岛 266237; 3 中国科学院上海光学精密机械研究所, 中国科学院空间激光信息传输与探测技术重点实验室, 上海 201800
  • 收稿日期:2022-11-18 修回日期:2023-01-13 出版日期:2024-05-28 发布日期:2024-06-11
  • 通讯作者: E-mail: dongwu@ouc.edu.cn E-mail:dongwu@ouc.edu.cn
  • 基金资助:
    中国科学院空间激光信息传输与探测技术重点实验室开放基金项目

Screening method of sea surface signals based on CALIOP dual-wavelength data

LUO Dunyi 1, WU Dong 1,2*, HE Yan 3   

  1. 1 College of Marine Technology, Faculty of Information Science and Engineering, Ocean University of China, Qingdao 266100, China; 2 Laboratory for Regional Oceanography and Numerical Modeling, Qingdao Laboratory for Marine Science and Technology, Qingdao 266237, China; 3 Key Laboratory of Space Laser Communication and Detection Technology, Shanghai Institute of Optics and Fine Mechanics, Chinese Academy of Sciences, Shanghai 201800, China
  • Received:2022-11-18 Revised:2023-01-13 Online:2024-05-28 Published:2024-06-11
  • Contact: Dong WU E-mail:dongwu@ouc.edu.cn
  • About author:罗敦艺 (1997- ), 四川内江人, 硕士研究生, 主要从事海洋与大气激光探测方面的研究。E-mail: luodunyi@163.com

摘要: 基于海面后向散射模型, 提出了一种利用CALIOP双波长海面信号进行数据质量控制的星载激光雷达数据筛 选方法。选取CALIOP 2018 年1―9 月Version 4.1.0 level 1 数据进行全球海面风速反演, 为提高数据可利用率, 在无云 海域探测海面风速的条件下增加了可穿透云CALIOP数据, 经过大气校正和双波长信号质量控制后进行风速反演, 以 准同步AMSR-2 风速数据作为参考值进行检验。分别采用Cox-Munk 和Hu模型的经验关系反演风速, 对于1―3 月数 据,前者标准偏差分别为1.14、1.18、1.16 m/s, 相关系数分别为0.90、0.91、0.91; 后者标准偏差分别为1.17、1.19、1.17 m/s, 相关系数分别为0.91、0.91、0.91。而相较于无云海域的反演研究, 可利用数据量提高约45.5%, 表明利用该方法既能保 证反演精度同时又能有效提高数据可利用率, 可为海面风场研究提供更多的数据源。

关键词: 遥感, 星载激光雷达, 海面后向散射, 海面风速, 信号提取

Abstract: Based on the sea surface backscattering model, a space-borne lidar data screening method using CALIOP dual-wavelength sea surface signal for data quality control is proposed. The global sea surface wind speed is retrieved from CALIOP's Version 4.1.0 level 1 data from January to September 2018. In order to improve data availability, under the condition of detecting sea surface wind speed in cloudless sea area, the cloud-penetrating CALIOP data were added, and then wind speed inversion was carried out after atmospheric correction and dual-wavelength signal quality control. At last, quasi-synchronous AMSR-2 wind speed data were used as reference values for verification. The two empirical relationships of Cox- Munk model and Hu model were used to invert wind speed respectively. For the data from January to March, the standard deviations of the former model are 1.14, 1.18 and 1.16m /s, respectively, with correlation coefficients of 0.90, 0.91 and 0.91, while the standard deviations of the latter are 1.17, 1.19 and 1.17m /s, respectively, with correlation coefficients of 0.91, 0.91 and 0.91. In addition, compared with the inversion study in cloudless sea, the available data amount using the proposed method increases by about 45.5%. The results show that the method proposed can not only ensure the accuracy of inversion but also effectively improve the utilization rate of data, which can provide more data sources for the study of sea surface wind field.

Key words: remote sensing, spaceborne lidar, sea surface backscatter, sea surface wind speed, signal extraction

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