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Developing and Testing Models for Sea Surface Wind Speed Estimation with GNSS-R Delay Doppler Maps and Delay Waveforms

机译:用GNSS-R延迟多普勒地图和延迟波形的海面风速估算开发和测试模型

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摘要

This paper focuses on sea surface wind speed estimation based on cyclone global navigation satellite system reflectometry (GNSS-R) data. In order to extract useful information from delay-Doppler map (DDM) data, three delay waveforms are presented for wind speed estimation. The delay waveform without Doppler shift is defined as central delay waveform (CDW), and the integral of the delay waveforms with different Doppler shift values is defined as integral delay waveform (IDW), while the difference between normalized IDW (NIDW) and normalized CDW (NCDW) is defined as differential delay waveform (DDW). We first propose a data filtering method based on threshold setting for data quality control. This method can select good-quality DDM data by adjusting the root mean square (RMS) threshold of cleaned DDW. Then, the normalized bistatic radar scattering cross section (NBRCS) and the leading edge slope (LES) of IDW are calculated using clean DDM data. Wind speed estimation models based on NBRCS and LES observations are then developed, respectively, and on this basis, a combination wind speed estimation model based on determination coefficient is further proposed. The CYGNSS data and ECMWF reanalysis data collected from 12 May 2020 to 12 August 2020 are used, excluding data collected on land, to evaluate the proposed models. The evaluation results show that the wind speed estimation accuracy of the piecewise function model based on NBRCS is 2.3 m/s in terms of root mean square error (RMSE), while that of the double-parameter and triple-parameter models is 2.6 and 2.7 m/s, respectively. The wind speed estimation accuracy of the double-parameter and triple-parameter models based on LES is 3.3 and 2.5 m/s. The results also demonstrate that the RMSE of the combination method is 2.1 m/s, and the coefficient of determination is 0.906, achieving a considerable performance gain compared with the individual NBRCS- and LES-based methods.
机译:本文重点基于旋风全局导航卫星系统反射测量(GNSS-R)数据的海面风速估计。为了从延迟 - 多普勒地图(DDM)数据中提取有用的信息,提出了三个延迟波形以进行风速估计。没有多普勒频移的延迟波形被定义为中心延迟波形(CDW),并且具有不同多普勒换档值的延迟波形的积分被定义为整体延迟波形(IDW),而归一化IDW(NIDW)和归一化CDW之间的差异。 (NCDW)被定义为差动延迟波形(DDW)。我们首先提出基于数据质量控制的阈值设置的数据过滤方法。该方法可以通过调整清洁DDW的根均线(RMS)阈值来选择良好质量的DDM数据。然后,使用Clean DDM数据计算IDW的归一化的双晶雷达散射截面(NBRC)和前沿斜率(LES)。然后,进一步提出了基于NBRC和LES观测的基于NBRC和LES观察的风速估计模型,并进一步提出了基于确定系数的组合风速估计模型。从2020年5月12日到2020年5月12日收集的CyGNS数据和ECMWF重新分析数据被使用,不包括在陆地上收集的数据,以评估所提出的模型。评估结果表明,基于NBRC的分段函数模型的风速估计精度在根均方误差(RMSE)方面是2.3米/秒,而双参数和三重参数模型的速度为2.6和2.7 M / s分别。基于LES的双参数和三级参数模型的风速估计精度为3.3和2.5 m / s。结果还表明,组合方法的RMSE为2.1米/秒,测定系数为0.906,与基于个体的NBRC和LES的方法相比,实现了相当大的性能增益。

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