Abstract

This article describes the first step toward the development of the geophysical model function (GMF) for the retrieval of wind speed and wind stress in hurricanes, based on developing a relation between the cross-polarized satellite SAR data from Sentinel-1 and winds/stress observed from collocated NOAA GPS-dropsondes data. Field measurements and remote sensing data for tropical cyclones in the Atlantic Ocean were analyzed. Using the data measured by GPS-dropsondes, average wind velocity profiles were obtained, while the parameters of the wind boundary layer (drag coefficient and friction velocity) were restored from the “wake” part of the velocity profiles using the self-similarity property. The self-similarity of the velocity profile “defect” in the boundary layer, known from the fluid dynamics, was used to retrieve the parameters of the atmospheric boundary layer (the surface wind velocity, drag coefficient, and friction velocity) from the dropsonde wind velocity profiles in ten major hurricanes. Based on the processing of the measurements in the hurricanes Irma 2017/09/07 and Maria 2017/09/21 and 2017/09/23 at a time close to the time of acquisition of the Sentinel-1 images, the dependencies of the cross-polarized normalized radar cross section on the wind speed and wind friction velocity were obtained and used for constructing the GMFs.

Highlights

  • This article presents the first results of studies on the development of the dependency of normalized radar crosssection (NRCS) on turbulent wind stress based on combined Sentinel-1 SAR data and field measurements of wind velocity profiles obtained by NOAA

  • Be emphasized that the proposed modified profiling method for determining the parameters of the atmospheric boundary layer enables the use of data measured at a large distance from the underlying surface. This makes it possible to utilize a much larger amount of data than within the traditional profiling method, applicable only to the limited dataset acquired near the water surface where measurements have a large error. This approach makes it possible to reduce the number of wind velocity profiles necessary for averaging and retrieving the parameters of the atmospheric boundary layer from data acquired in a certain hurricane at a certain time

  • This paper describes the first step towards the development of geophysical model function (GMF) for retrieval wind speed and wind stress in hurricanes basing on calibration of the cross-polarized satellite SAR data from Sentinel-1 by the collocated NOAA GPS-dropsondes data

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Summary

Introduction

This article presents the first results of studies on the development of the dependency of NRCS on turbulent wind stress (or friction velocity) based on combined Sentinel-1 SAR data and field measurements of wind velocity profiles obtained by NOAA The self-similar laws for velocity profiles in the turbulent boundary layer are applicable only to values averaged over a statistical ensemble.

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