2008
DOI: 10.3402/tellusa.v60i2.15182
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ADM-Aeolus retrieval algorithms for aerosol and cloud products

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Cited by 18 publications
(25 citation statements)
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“…ADM-Aeolus will also deliver height profiles of Mie and Rayleigh co-polarized backscatter and extinction coefficients, scattering ratios and lidar ratios [6] along the lidar line-of-sight. From these parameters it is possible to derive cloud and aerosol information such as layer height, multi- layer cloud and aerosol stratification, cloud and aerosol optical depths (integrated light-extinction profiles), and some information on cloud/aerosol type (lidar ratio).…”
Section: Products and Product Requirementsmentioning
confidence: 99%
“…ADM-Aeolus will also deliver height profiles of Mie and Rayleigh co-polarized backscatter and extinction coefficients, scattering ratios and lidar ratios [6] along the lidar line-of-sight. From these parameters it is possible to derive cloud and aerosol information such as layer height, multi- layer cloud and aerosol stratification, cloud and aerosol optical depths (integrated light-extinction profiles), and some information on cloud/aerosol type (lidar ratio).…”
Section: Products and Product Requirementsmentioning
confidence: 99%
“…Thus, L2B products are intermediate between L1B and L2C data. Level-2A products (information on aerosol and cloud layer optical properties) are described by Flamant et al (2008). The operational production of L2B data will be done at ECMWF slightly behind real time, just before the assimilation (and production of L2C) is carried out.…”
Section: The Scope and Purpose Of The Aeolus Wind Retrieval Algorithmsmentioning
confidence: 99%
“…The signal amplitudes also provide product confidence data, including error quantifiers, for the wind and particle information. Although more details on the measurement principles underpinning the instrument are given in other papers from this volume Flamant et al, 2008) and elsewhere , we summarize here the points most relevant for understanding the Level-2B wind retrieval algorithms. The solid curve in fig.…”
Section: The Adm-aeolus Instrumentmentioning
confidence: 99%
“…Airborne HSRLs at 532 nm using iodine vapor filters to reject aerosol scattering have been successfully developed and demonstrated by the NASA Langley Research Center [14,15] and the German Aerospace Center (DLR) [16][17][18][19], respectively. In the near future, the Doppler wind lidar Atmospheric Laser Doppler Instrument (ALADIN) [20,21] of the European Space Agency's (ESA) Atmospheric Dynamics Mission (ADM) [22,23], which uses a Fabry-Perot interferometer and a Fizeau interferometer at 355 nm for Rayleigh and Mie detection, respectively, will be the first HSRL in space [24,25]. As part of ESA's Earth Clouds, Aerosols, and Radiation Explorer (EarthCARE) mission [26], the HSRL Atmospheric Lidar (ATLID) at 355 nm is planned to be employed for direct aerosol extinction measurements with a Fabry-Perot interferometer [27].…”
Section: Introductionmentioning
confidence: 99%
“…The information of molecular scattering can be obtained by using iodine vapor filters [11][12][13] or Fabry-Perot interferometers [24,25,27]. With an iodine vapor filter, the narrowband aerosol Mie scattering can be suppressed by a factor of 10 −6 − 10 −5 [17], while the wings of the molecular scattering can pass through the iodine vapor filter.…”
Section: Introductionmentioning
confidence: 99%