A Decade of CALIPSO Observations of Asian and Saharan Dust Properties near Source and Transport Regions

The lidar on the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) mission, makes robust measurements of dust and has generated a length of record that is significant both seasonally and inter-annually. We exploit this record to determine a multi-year climatology of the pr...

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Main Author: Omar Ali
Format: Article
Language:English
Published: EDP Sciences 2019-01-01
Series:E3S Web of Conferences
Online Access:https://www.e3s-conferences.org/articles/e3sconf/pdf/2019/25/e3sconf_caduc2019_02008.pdf
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spelling doaj-026fabe17c1c4486b0658d5f164d21ef2021-02-02T07:37:08ZengEDP SciencesE3S Web of Conferences2267-12422019-01-01990200810.1051/e3sconf/20199902008e3sconf_caduc2019_02008A Decade of CALIPSO Observations of Asian and Saharan Dust Properties near Source and Transport RegionsOmar AliThe lidar on the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) mission, makes robust measurements of dust and has generated a length of record that is significant both seasonally and inter-annually. We exploit this record to determine a multi-year climatology of the properties of Asian and Saharan dust, in particular seasonal optical depths, layer frequencies, and layer heights of dust gridded in accordance with the Level 3 data products protocol between 2006 and 2016. The data are screened using standard CALIPSO quality assurance flags, cloud aerosol discrimination (CAD) scores, overlying features and layer properties. To evaluate the effects of transport on small-scale phenomena such as morphology, vertical extent and size of the dust layers, we compare probability distribution functions of the layer integrated volume depolarization ratios, geometric depths and integrated attenuated color ratios near the source to the same distributions in the far field or transport region. To evaluate the uncertainty in the lidar ratios, we compare the values computed from dust layers overlying opaque water clouds, considered accurate, with the constant lidar ratio value used in the CALIOP algorithms for dusthttps://www.e3s-conferences.org/articles/e3sconf/pdf/2019/25/e3sconf_caduc2019_02008.pdf
collection DOAJ
language English
format Article
sources DOAJ
author Omar Ali
spellingShingle Omar Ali
A Decade of CALIPSO Observations of Asian and Saharan Dust Properties near Source and Transport Regions
E3S Web of Conferences
author_facet Omar Ali
author_sort Omar Ali
title A Decade of CALIPSO Observations of Asian and Saharan Dust Properties near Source and Transport Regions
title_short A Decade of CALIPSO Observations of Asian and Saharan Dust Properties near Source and Transport Regions
title_full A Decade of CALIPSO Observations of Asian and Saharan Dust Properties near Source and Transport Regions
title_fullStr A Decade of CALIPSO Observations of Asian and Saharan Dust Properties near Source and Transport Regions
title_full_unstemmed A Decade of CALIPSO Observations of Asian and Saharan Dust Properties near Source and Transport Regions
title_sort decade of calipso observations of asian and saharan dust properties near source and transport regions
publisher EDP Sciences
series E3S Web of Conferences
issn 2267-1242
publishDate 2019-01-01
description The lidar on the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) mission, makes robust measurements of dust and has generated a length of record that is significant both seasonally and inter-annually. We exploit this record to determine a multi-year climatology of the properties of Asian and Saharan dust, in particular seasonal optical depths, layer frequencies, and layer heights of dust gridded in accordance with the Level 3 data products protocol between 2006 and 2016. The data are screened using standard CALIPSO quality assurance flags, cloud aerosol discrimination (CAD) scores, overlying features and layer properties. To evaluate the effects of transport on small-scale phenomena such as morphology, vertical extent and size of the dust layers, we compare probability distribution functions of the layer integrated volume depolarization ratios, geometric depths and integrated attenuated color ratios near the source to the same distributions in the far field or transport region. To evaluate the uncertainty in the lidar ratios, we compare the values computed from dust layers overlying opaque water clouds, considered accurate, with the constant lidar ratio value used in the CALIOP algorithms for dust
url https://www.e3s-conferences.org/articles/e3sconf/pdf/2019/25/e3sconf_caduc2019_02008.pdf
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