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Desert Roughness Retrieval Using CYGNSS GNSS-R Data

Authors
  • stilla, donato
  • zribi, mehrez
  • pierdicca, nazzareno
  • baghdadi, nicolas
  • huc, mireille
Publication Date
Feb 24, 2020
Identifiers
DOI: 10.3390/rs12040743
OAI: oai:mdpi.com:/2072-4292/12/4/743/
Source
MDPI
Keywords
Language
English
License
Green
External links

Abstract

The aim of this paper is to assess the potential use of data recorded by the Global Navigation Satellite System Reflectometry (GNSS-R) Cyclone Global Navigation Satellite System (CYGNSS) constellation to characterize desert surface roughness. The study is applied over the Sahara, the largest non-polar desert in the world. This is based on a spatio-temporal analysis of variations in Cyclone Global Navigation Satellite System (CYGNSS) data, expressed as changes in reflectivity (&Gamma / ). In general, the reflectivity of each type of land surface (reliefs, dunes, etc.) encountered at the studied site is found to have a high temporal stability. A grid of CYGNSS &Gamma / measurements has been developed, at the relatively fine resolution of 0.03&deg / &times / 0.03&deg / , and the resulting map of average reflectivity, computed over a 2.5-year period, illustrates the potential of CYGNSS data for the characterization of the main types of desert land surface (dunes, reliefs, etc.). A discussion of the relationship between aerodynamic or geometric roughness and CYGNSS reflectivity is proposed. A high correlation is observed between these roughness parameters and reflectivity. The behaviors of the GNSS-R reflectivity and the Advanced Land Observing Satellite-2 (ALOS-2) Synthetic Aperture Radar (SAR) backscattering coefficient are compared and found to be strongly correlated. An aerodynamic roughness (Z0) map of the Sahara is proposed, using four distinct classes of terrain roughness.

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