Impact of Surface Soil Moisture Variations on Radar Altimetry Echoes at Ku and Ka Bands in Semi-Arid Areas

Radar altimetry provides information on the topography of the Earth surface. It is commonly used for the monitoring not only sea surface height but also ice sheets topography and inland water levels. The radar altimetry backscattering coefficient, which depends on surface roughness and water content...

Full description

Bibliographic Details
Main Authors: Christophe Fatras, Pierre Borderies, Frédéric Frappart, Eric Mougin, Denis Blumstein, Fernando Niño
Format: Article
Language:English
Published: MDPI AG 2018-04-01
Series:Remote Sensing
Subjects:
Online Access:http://www.mdpi.com/2072-4292/10/4/582
_version_ 1818958388366671872
author Christophe Fatras
Pierre Borderies
Frédéric Frappart
Eric Mougin
Denis Blumstein
Fernando Niño
author_facet Christophe Fatras
Pierre Borderies
Frédéric Frappart
Eric Mougin
Denis Blumstein
Fernando Niño
author_sort Christophe Fatras
collection DOAJ
description Radar altimetry provides information on the topography of the Earth surface. It is commonly used for the monitoring not only sea surface height but also ice sheets topography and inland water levels. The radar altimetry backscattering coefficient, which depends on surface roughness and water content, can be related to surface properties such as surface soil moisture content. In this study, the influence of surface soil moisture on the radar altimetry echo and backscattering coefficient is analyzed over semi-arid areas. A semi-empirical model of the soil’s complex dielectric permittivity that takes into account that small-scale roughness and large-scale topography was developed to simulate the radar echoes. It was validated using waveforms acquired at Ku and Ka-bands by ENVISAT RA-2 and SARAL AltiKa respectively over several sites in Mali. Correlation coefficients ranging from 0.66 to 0.94 at Ku-band and from 0.27 to 0.96 at Ka-band were found. The increase in surface soil moisture from 0.02 to 0.4 (i.e., the typical range of variations in semi-arid areas) increase the backscattering from 10 to 15 dB between the core of the dry and the maximum of the rainy seasons.
first_indexed 2024-12-20T11:24:57Z
format Article
id doaj.art-5fd741858c7745039ecefff9d8bbd6f9
institution Directory Open Access Journal
issn 2072-4292
language English
last_indexed 2024-12-20T11:24:57Z
publishDate 2018-04-01
publisher MDPI AG
record_format Article
series Remote Sensing
spelling doaj.art-5fd741858c7745039ecefff9d8bbd6f92022-12-21T19:42:25ZengMDPI AGRemote Sensing2072-42922018-04-0110458210.3390/rs10040582rs10040582Impact of Surface Soil Moisture Variations on Radar Altimetry Echoes at Ku and Ka Bands in Semi-Arid AreasChristophe Fatras0Pierre Borderies1Frédéric Frappart2Eric Mougin3Denis Blumstein4Fernando Niño5Office National d’Etudes et de Recherches Aerospatiales (ONERA), 2 Avenue Edouard Belin, 31055 Toulouse CEDEX 4, FranceOffice National d’Etudes et de Recherches Aerospatiales (ONERA), 2 Avenue Edouard Belin, 31055 Toulouse CEDEX 4, FranceGeosciences Environnement Toulouse (GET), UMR 5563, CNRS/IRD/UPS, Observatoire Midi-Pyrenees 8 (OMP), 14 Avenue Edouard Belin, 31400 Toulouse, FranceGeosciences Environnement Toulouse (GET), UMR 5563, CNRS/IRD/UPS, Observatoire Midi-Pyrenees 8 (OMP), 14 Avenue Edouard Belin, 31400 Toulouse, FranceLaboratoire d’Etudes en Geophysique et Oceanographie Spatiales (LEGOS), UMR 5566, CNRS/IRD/UPS, Observatoire Midi-Pyrenees 8 (OMP), 14 Avenue Edouard Belin, 31400 Toulouse, FranceLaboratoire d’Etudes en Geophysique et Oceanographie Spatiales (LEGOS), UMR 5566, CNRS/IRD/UPS, Observatoire Midi-Pyrenees 8 (OMP), 14 Avenue Edouard Belin, 31400 Toulouse, FranceRadar altimetry provides information on the topography of the Earth surface. It is commonly used for the monitoring not only sea surface height but also ice sheets topography and inland water levels. The radar altimetry backscattering coefficient, which depends on surface roughness and water content, can be related to surface properties such as surface soil moisture content. In this study, the influence of surface soil moisture on the radar altimetry echo and backscattering coefficient is analyzed over semi-arid areas. A semi-empirical model of the soil’s complex dielectric permittivity that takes into account that small-scale roughness and large-scale topography was developed to simulate the radar echoes. It was validated using waveforms acquired at Ku and Ka-bands by ENVISAT RA-2 and SARAL AltiKa respectively over several sites in Mali. Correlation coefficients ranging from 0.66 to 0.94 at Ku-band and from 0.27 to 0.96 at Ka-band were found. The increase in surface soil moisture from 0.02 to 0.4 (i.e., the typical range of variations in semi-arid areas) increase the backscattering from 10 to 15 dB between the core of the dry and the maximum of the rainy seasons.http://www.mdpi.com/2072-4292/10/4/582radar altimetrywaveformdielectric permittivitysoil moisture
spellingShingle Christophe Fatras
Pierre Borderies
Frédéric Frappart
Eric Mougin
Denis Blumstein
Fernando Niño
Impact of Surface Soil Moisture Variations on Radar Altimetry Echoes at Ku and Ka Bands in Semi-Arid Areas
Remote Sensing
radar altimetry
waveform
dielectric permittivity
soil moisture
title Impact of Surface Soil Moisture Variations on Radar Altimetry Echoes at Ku and Ka Bands in Semi-Arid Areas
title_full Impact of Surface Soil Moisture Variations on Radar Altimetry Echoes at Ku and Ka Bands in Semi-Arid Areas
title_fullStr Impact of Surface Soil Moisture Variations on Radar Altimetry Echoes at Ku and Ka Bands in Semi-Arid Areas
title_full_unstemmed Impact of Surface Soil Moisture Variations on Radar Altimetry Echoes at Ku and Ka Bands in Semi-Arid Areas
title_short Impact of Surface Soil Moisture Variations on Radar Altimetry Echoes at Ku and Ka Bands in Semi-Arid Areas
title_sort impact of surface soil moisture variations on radar altimetry echoes at ku and ka bands in semi arid areas
topic radar altimetry
waveform
dielectric permittivity
soil moisture
url http://www.mdpi.com/2072-4292/10/4/582
work_keys_str_mv AT christophefatras impactofsurfacesoilmoisturevariationsonradaraltimetryechoesatkuandkabandsinsemiaridareas
AT pierreborderies impactofsurfacesoilmoisturevariationsonradaraltimetryechoesatkuandkabandsinsemiaridareas
AT fredericfrappart impactofsurfacesoilmoisturevariationsonradaraltimetryechoesatkuandkabandsinsemiaridareas
AT ericmougin impactofsurfacesoilmoisturevariationsonradaraltimetryechoesatkuandkabandsinsemiaridareas
AT denisblumstein impactofsurfacesoilmoisturevariationsonradaraltimetryechoesatkuandkabandsinsemiaridareas
AT fernandonino impactofsurfacesoilmoisturevariationsonradaraltimetryechoesatkuandkabandsinsemiaridareas