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多源卫星遥感海面风速误差分析和交叉标定
引用本文:吕思睿,林文明,邹巨洪,等. 多源卫星遥感海面风速误差分析和交叉标定[J]. 海洋学报,2023,45(5):118–128 doi: 10.12284/hyxb2023066
作者姓名:吕思睿  林文明  邹巨洪  王志雄
作者单位:南京信息工程大学 海洋科学学院,江苏 南京 210044;南京信息工程大学 海洋科学学院,江苏 南京 210044;自然资源部空间海洋遥感与应用重点实验室,北京 100081;自然资源部空间海洋遥感与应用重点实验室,北京 100081;国家卫星海洋应用中心,北京 100081
基金项目:国家重点研发计划(2022YFC3104902)。
摘    要:利用多源卫星散射计和辐射计构建高时间分辨率的海面风遥感数据集是当前海洋遥感研究的热点。本文针对2019年同时期在轨运行的卫星散射计和辐射计,利用浮标数据和欧洲中期天气预报中心(ECMWF)第五代大气再分析数据(ERA5),定量评估了不同传感器获取的海面风速数据的误差特性和标定系数,阐明不同卫星遥感海面风单位误差相对大小,为多源卫星海面风场融合、同化等定量应用提供技术支撑。与常用的中性参考风相比,微波散射计和辐射计反演的风速更适合用等效应力风解释,以便实现卫星遥感数据的优化应用。现有微波散射计和辐射计遥感的海面风速与浮标和ERA5等效应力风在总体上具有良好的一致性,但在高风速条件下(风速大于20 m/s)呈明显的偏差。本文提出的一种用于风速误差横向对比的指示因子,实现了散射计与辐射计风速相对误差估计,为多源数据同化应用中的误差设置提供重要的参考。结果表明:5种散射计风速固有误差介于0.40~0.73之间,5种微波辐射计的风速固有误差介于0.86~1.23。总体而言,在0~20 m/s风速范围内,散射计的风速精度优于辐射计。

关 键 词:海面风  散射计  辐射计  等效应力风  误差估计
收稿时间:2022-07-29
修稿时间:2022-12-07

Error quantification and cross calibration of sea surface wind speeds from multiple remote sensing satellites
Lü Sirui,Lin Wenming,Zou Juhong, et al. Error quantification and cross calibration of sea surface wind speeds from multiple remote sensing satellites[J]. Haiyang Xuebao,2023, 45(5):118–128 doi: 10.12284/hyxb2023066
Authors:Lü Sirui  Lin Wenming  Zou Juhong  Wang Zhixiong
Affiliation:1. School of Marine Sciences, Nanjing University of Information Science and Technology, Nanjing 210044, China;;2. Key Laboratory of Space Ocean Remote Sensing and Application, Ministry of Natural Resources, Beijing 100081, China;;3. National Satellite Ocean Application Service, Beijing 100081, China
Abstract:In the field of ocean remote sensing research, the construction of a high temporal resolution sea surface wind (SSW) dataset through the use of multi-source satellite data has become a popular topic. This article aims to quantitatively evaluate the error characteristics and calibration coefficients of SSW speed data obtained from different sensors using buoy data and ERA5 for the satellites scatterometer and radiometer in orbit simultaneously in 2019. The unit error of various satellite remote sensing SSW is comparatively analyzed, providing technical support for quantitative applications such as multi-source satellite SSW blending and assimilation. Furthermore, compared with equal neutral wind speeds, the wind speeds inferred by microwave scatterometer and radiometer are better suited to be interpreted by stress-equivalent winds, which enables the optimal application of satellite remote sensing data. The SSW speeds remotely sensed by existing scatterometers and radiometers are generally consistent with the buoy and ERA5 stress-equivalent wind, but exhibit some deviations at high wind speeds (wind speed greater than 20 m/s). An indicator factor for lateral comparison of wind speed errors is proposed to achieve relative error estimation of scatterometer and radiometer wind speeds, which provides an important reference for error setting in multi-source data assimilation applications. The results demonstrate that the inherent wind speed errors of the five scatterometers range from 0.40 to 0.73, and the inherent wind speed errors of the five microwave radiometers range from 0.86 to 1.23. In conclusion, it can be observed that the scatterometers generally exhibit better accuracy in SSW speed estimation than radiometers in the wind speed range of 0 m/s to 20 m/s.
Keywords:sea surface wind  scatterometer  radiometer  stress-equivalent wind  error estimation
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