Abstract

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.

Highlights

  • Sea surface wind speed is a key factor that affects ocean circulation and global climate

  • In [36], a machine learning (ML) algorithm based on multi-hidden layer neural network (MHL-NN) is proposed to estimate sea surface wind speed, and the results showed that the MHL-NN algorithm, mainly based on DDMA and leading edge slope (LES) observations, is superior to other methods in terms of root mean square error (RMSE) and average absolute percentage error (MAPE) of wind speed estimation

  • This paper focused on empirical modeling for sea surface wind speed estimation using normalized bistatic radar scattering cross section (NBRCS) and LES observations which are generated by processing Global Navigation Satellite System Reflectometry (GNSS-R) delay Doppler map (DDM) data

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Summary

Introduction

Sea surface wind speed is a key factor that affects ocean circulation and global climate. As one of the most serious natural disasters, tropical cyclones greatly damage infrastructure and endanger lives. For these reasons, it is vital to monitor sea wind speed to study and predict some complex weather conditions, so as to enable tropical cyclone warnings. It is vital to monitor sea wind speed to study and predict some complex weather conditions, so as to enable tropical cyclone warnings Traditional observation tools, such as buoys and ships, can provide long-term observations of sea wind speeds, but they have some limitations for global observations, such as limited space sampling and high costs. GNSS-R has the advantages of low cost, large coverage, and operational under all-weather conditions

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