Comparison of satellite microwave backscattering (ASCAT) and visible/near-infrared reflectances (PARASOL) for the estimation of aeolian aerodynamic roughness length in arid and semi-arid regions

Previous studies examined the possibility to estimate the aeolian aerodynamic roughness length from satellites, either from visible/near-infrared observations or from microwave backscattering measurements. Here we compare the potential of the two approaches and propose to merge the two sources of in...

Full description

Bibliographic Details
Main Authors: C. Prigent, C. Jiménez, J. Catherinot
Format: Article
Language:English
Published: Copernicus Publications 2012-11-01
Series:Atmospheric Measurement Techniques
Online Access:http://www.atmos-meas-tech.net/5/2703/2012/amt-5-2703-2012.pdf
id doaj-c1ceb1623e2e41f38c515267b4be0a06
record_format Article
spelling doaj-c1ceb1623e2e41f38c515267b4be0a062020-11-24T23:08:59ZengCopernicus PublicationsAtmospheric Measurement Techniques1867-13811867-85482012-11-015112703271210.5194/amt-5-2703-2012Comparison of satellite microwave backscattering (ASCAT) and visible/near-infrared reflectances (PARASOL) for the estimation of aeolian aerodynamic roughness length in arid and semi-arid regionsC. PrigentC. JiménezJ. CatherinotPrevious studies examined the possibility to estimate the aeolian aerodynamic roughness length from satellites, either from visible/near-infrared observations or from microwave backscattering measurements. Here we compare the potential of the two approaches and propose to merge the two sources of information to benefit from their complementary aspects, i.e. the high spatial resolution of the visible/near-infrared (6 km for PARASOL that is part of the A-Train) and the independence from atmospheric contamination of the active microwaves (ASCAT on board MetOp with a lower spatial resolution of 25 km). A global map of the aeolian aerodynamic roughness length at 6 km resolution is derived, for arid and semi-arid regions. It shows very good consistency with the existing information on the properties of these surfaces. The dataset is available to the community, for use in atmospheric dust transport models.http://www.atmos-meas-tech.net/5/2703/2012/amt-5-2703-2012.pdf
collection DOAJ
language English
format Article
sources DOAJ
author C. Prigent
C. Jiménez
J. Catherinot
spellingShingle C. Prigent
C. Jiménez
J. Catherinot
Comparison of satellite microwave backscattering (ASCAT) and visible/near-infrared reflectances (PARASOL) for the estimation of aeolian aerodynamic roughness length in arid and semi-arid regions
Atmospheric Measurement Techniques
author_facet C. Prigent
C. Jiménez
J. Catherinot
author_sort C. Prigent
title Comparison of satellite microwave backscattering (ASCAT) and visible/near-infrared reflectances (PARASOL) for the estimation of aeolian aerodynamic roughness length in arid and semi-arid regions
title_short Comparison of satellite microwave backscattering (ASCAT) and visible/near-infrared reflectances (PARASOL) for the estimation of aeolian aerodynamic roughness length in arid and semi-arid regions
title_full Comparison of satellite microwave backscattering (ASCAT) and visible/near-infrared reflectances (PARASOL) for the estimation of aeolian aerodynamic roughness length in arid and semi-arid regions
title_fullStr Comparison of satellite microwave backscattering (ASCAT) and visible/near-infrared reflectances (PARASOL) for the estimation of aeolian aerodynamic roughness length in arid and semi-arid regions
title_full_unstemmed Comparison of satellite microwave backscattering (ASCAT) and visible/near-infrared reflectances (PARASOL) for the estimation of aeolian aerodynamic roughness length in arid and semi-arid regions
title_sort comparison of satellite microwave backscattering (ascat) and visible/near-infrared reflectances (parasol) for the estimation of aeolian aerodynamic roughness length in arid and semi-arid regions
publisher Copernicus Publications
series Atmospheric Measurement Techniques
issn 1867-1381
1867-8548
publishDate 2012-11-01
description Previous studies examined the possibility to estimate the aeolian aerodynamic roughness length from satellites, either from visible/near-infrared observations or from microwave backscattering measurements. Here we compare the potential of the two approaches and propose to merge the two sources of information to benefit from their complementary aspects, i.e. the high spatial resolution of the visible/near-infrared (6 km for PARASOL that is part of the A-Train) and the independence from atmospheric contamination of the active microwaves (ASCAT on board MetOp with a lower spatial resolution of 25 km). A global map of the aeolian aerodynamic roughness length at 6 km resolution is derived, for arid and semi-arid regions. It shows very good consistency with the existing information on the properties of these surfaces. The dataset is available to the community, for use in atmospheric dust transport models.
url http://www.atmos-meas-tech.net/5/2703/2012/amt-5-2703-2012.pdf
work_keys_str_mv AT cprigent comparisonofsatellitemicrowavebackscatteringascatandvisiblenearinfraredreflectancesparasolfortheestimationofaeolianaerodynamicroughnesslengthinaridandsemiaridregions
AT cjimenez comparisonofsatellitemicrowavebackscatteringascatandvisiblenearinfraredreflectancesparasolfortheestimationofaeolianaerodynamicroughnesslengthinaridandsemiaridregions
AT jcatherinot comparisonofsatellitemicrowavebackscatteringascatandvisiblenearinfraredreflectancesparasolfortheestimationofaeolianaerodynamicroughnesslengthinaridandsemiaridregions
_version_ 1725612145958191104