Abstract
Rain Signatures on C-band Synthetic Aperture Radar (SAR) images acquired over ocean are common and can dominate the backscattered signal from the ocean surface. In many cases, the inability to decipher between ocean and rain signatures can disturb the analysis of SAR scenes for maritime applications. This study relies on Sentinel-1 SAR acquisitions in the Interferometric Wide swath mode and high-resolution measurements from ground-based weather radar to document the rain impact on the radar backscattered signal in both co- and cross-polarization channels. The dark and bright rain signatures are found in connection with the timeliness of the rain cells. In particular, the bright patches are demonstrated by the hydrometeors (graupels, hails) in the melting layer. In general, the radar backscatter under rain increases with rain rate for a given sea state and decreases when the sea state strengthens. The rain also has a stronger impact on the radar signal in both polarizations when the incidence angle increases. The complementary sensitivity of the SAR signal of rain in both channels is then used to derive a filter to locate the areas in SAR scenes where the signal is not dominated by rain. The filter optimized to match the rain observed by the ground-based weather radar is more efficient when both polarization channels are considered. Case studies are presented to discuss the advantages and limitations of such a filtering approach.
Highlights
Sentinel-1B (S-1B) launched in April 2014 and April 2016, respectively. They operate with four exclusive modes, Interferometric Wide Swath (IW) mode, Extra Wide Swath (EW) mode, StripMap (SM) mode, and Wave (WV) mode
We focus on S-1 IW acquisitions (VV + VH) from March 2015 to November 2020
The mean NRCSratio values are found to be positive excepted for low winds and light rain for which the ratio is found to be around zero
Summary
Publisher’s Note: MDPI stays neutral with regard to jurisdictional claims in published maps and institutional affiliations. Areas associated with bright patches on the VV images are visible as bright area on VH polarization channel and probably not due to Bragg scattering from ring waves but to enhanced roughness from splash products [17] or from scattering of hydrometeors in the melting layer [21] These continuous studies have revealed that the complicated mechanisms of rain signatures at C-band SAR images. We take advantage of the Sentinel-1 that provides a large amount of data close to the coast in co- and cross-polarization collocated with operational weather radar stations Based on this dataset, we aim to document the different behaviors of high-resolution co-/cross-pol NRCS in response to intensifying rain rate and wind speed.
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