Interpretation of FRESCO cloud retrievals in case of absorbing aerosol events

Cloud and aerosol information is needed in trace gas retrievals from satellite measurements. The Fast REtrieval Scheme for Clouds from the Oxygen A band (FRESCO) cloud algorithm employs reflectance spectra of the O<sub>2</sub> A band around 760 nm to derive cloud pressure...

Full description

Bibliographic Details
Main Authors: P. Wang, O. N. E. Tuinder, L. G. Tilstra, M. de Graaf, P. Stammes
Format: Article
Language:English
Published: Copernicus Publications 2012-10-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/12/9057/2012/acp-12-9057-2012.pdf
_version_ 1818499888380379136
author P. Wang
O. N. E. Tuinder
L. G. Tilstra
M. de Graaf
P. Stammes
author_facet P. Wang
O. N. E. Tuinder
L. G. Tilstra
M. de Graaf
P. Stammes
author_sort P. Wang
collection DOAJ
description Cloud and aerosol information is needed in trace gas retrievals from satellite measurements. The Fast REtrieval Scheme for Clouds from the Oxygen A band (FRESCO) cloud algorithm employs reflectance spectra of the O<sub>2</sub> A band around 760 nm to derive cloud pressure and effective cloud fraction. In general, clouds contribute more to the O<sub>2</sub> A band reflectance than aerosols. Therefore, the FRESCO algorithm does not correct for aerosol effects in the retrievals and attributes the retrieved cloud information entirely to the presence of clouds, and not to aerosols. For events with high aerosol loading, aerosols may have a dominant effect, especially for almost cloud free scenes. We have analysed FRESCO cloud data and Absorbing Aerosol Index (AAI) data from the Global Ozone Monitoring Experiment (GOME-2) instrument on the Metop-A satellite for events with typical absorbing aerosol types, such as volcanic ash, desert dust and smoke. We find that the FRESCO effective cloud fractions are correlated with the AAI data for these absorbing aerosol events and that the FRESCO cloud pressure contains information on aerosol layer pressure. For cloud free scenes, the derived FRESCO cloud pressure is close to the aerosol layer pressure, especially for optically thick aerosol layers. For cloudy scenes, if the strongly absorbing aerosols are located above the clouds, then the retrieved FRESCO cloud pressure may represent the height of the aerosol layer rather than the height of the clouds. Combining FRESCO and AAI data, an estimate for the aerosol layer pressure can be given.
first_indexed 2024-12-10T20:35:43Z
format Article
id doaj.art-d34905331c3a443783f4f6410cd79e7c
institution Directory Open Access Journal
issn 1680-7316
1680-7324
language English
last_indexed 2024-12-10T20:35:43Z
publishDate 2012-10-01
publisher Copernicus Publications
record_format Article
series Atmospheric Chemistry and Physics
spelling doaj.art-d34905331c3a443783f4f6410cd79e7c2022-12-22T01:34:32ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242012-10-0112199057907710.5194/acp-12-9057-2012Interpretation of FRESCO cloud retrievals in case of absorbing aerosol eventsP. WangO. N. E. TuinderL. G. TilstraM. de GraafP. StammesCloud and aerosol information is needed in trace gas retrievals from satellite measurements. The Fast REtrieval Scheme for Clouds from the Oxygen A band (FRESCO) cloud algorithm employs reflectance spectra of the O<sub>2</sub> A band around 760 nm to derive cloud pressure and effective cloud fraction. In general, clouds contribute more to the O<sub>2</sub> A band reflectance than aerosols. Therefore, the FRESCO algorithm does not correct for aerosol effects in the retrievals and attributes the retrieved cloud information entirely to the presence of clouds, and not to aerosols. For events with high aerosol loading, aerosols may have a dominant effect, especially for almost cloud free scenes. We have analysed FRESCO cloud data and Absorbing Aerosol Index (AAI) data from the Global Ozone Monitoring Experiment (GOME-2) instrument on the Metop-A satellite for events with typical absorbing aerosol types, such as volcanic ash, desert dust and smoke. We find that the FRESCO effective cloud fractions are correlated with the AAI data for these absorbing aerosol events and that the FRESCO cloud pressure contains information on aerosol layer pressure. For cloud free scenes, the derived FRESCO cloud pressure is close to the aerosol layer pressure, especially for optically thick aerosol layers. For cloudy scenes, if the strongly absorbing aerosols are located above the clouds, then the retrieved FRESCO cloud pressure may represent the height of the aerosol layer rather than the height of the clouds. Combining FRESCO and AAI data, an estimate for the aerosol layer pressure can be given.http://www.atmos-chem-phys.net/12/9057/2012/acp-12-9057-2012.pdf
spellingShingle P. Wang
O. N. E. Tuinder
L. G. Tilstra
M. de Graaf
P. Stammes
Interpretation of FRESCO cloud retrievals in case of absorbing aerosol events
Atmospheric Chemistry and Physics
title Interpretation of FRESCO cloud retrievals in case of absorbing aerosol events
title_full Interpretation of FRESCO cloud retrievals in case of absorbing aerosol events
title_fullStr Interpretation of FRESCO cloud retrievals in case of absorbing aerosol events
title_full_unstemmed Interpretation of FRESCO cloud retrievals in case of absorbing aerosol events
title_short Interpretation of FRESCO cloud retrievals in case of absorbing aerosol events
title_sort interpretation of fresco cloud retrievals in case of absorbing aerosol events
url http://www.atmos-chem-phys.net/12/9057/2012/acp-12-9057-2012.pdf
work_keys_str_mv AT pwang interpretationoffrescocloudretrievalsincaseofabsorbingaerosolevents
AT onetuinder interpretationoffrescocloudretrievalsincaseofabsorbingaerosolevents
AT lgtilstra interpretationoffrescocloudretrievalsincaseofabsorbingaerosolevents
AT mdegraaf interpretationoffrescocloudretrievalsincaseofabsorbingaerosolevents
AT pstammes interpretationoffrescocloudretrievalsincaseofabsorbingaerosolevents