Impacts of water vapor on Saharan air layer radiative heating

Abstract Airborne lidar observations of long-range transported Saharan air layers in the western North Atlantic trades indicate increased amounts of water vapor within the dust layers compared to the surrounding dry free atmosphere. This study investigates the impact of such enhanced water vapor con...

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Published in:Geophysical Research Letters
Main Authors: Gutleben, Manuel, Groß, Silke, Wirth, Martin, Emde, Claudia, Mayer, Bernhard
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2019
Subjects:
Online Access:https://elib.dlr.de/134038/
https://elib.dlr.de/134038/1/Gutleben_et_al-2019-Geophysical_Research_Letters.pdf
https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/2019GL085344
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spelling ftdlr:oai:elib.dlr.de:134038 2023-12-03T10:26:52+01:00 Impacts of water vapor on Saharan air layer radiative heating Gutleben, Manuel Groß, Silke Wirth, Martin Emde, Claudia Mayer, Bernhard 2019-12-23 application/pdf https://elib.dlr.de/134038/ https://elib.dlr.de/134038/1/Gutleben_et_al-2019-Geophysical_Research_Letters.pdf https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/2019GL085344 en eng Wiley https://elib.dlr.de/134038/1/Gutleben_et_al-2019-Geophysical_Research_Letters.pdf Gutleben, Manuel und Groß, Silke und Wirth, Martin und Emde, Claudia und Mayer, Bernhard (2019) Impacts of water vapor on Saharan air layer radiative heating. Geophysical Research Letters, 46 (24), Seiten 14854-14862. Wiley. doi:10.1029/2019GL085344 <https://doi.org/10.1029/2019GL085344>. ISSN 0094-8276. cc_by Institut für Physik der Atmosphäre Zeitschriftenbeitrag PeerReviewed 2019 ftdlr https://doi.org/10.1029/2019GL085344 2023-11-06T00:24:18Z Abstract Airborne lidar observations of long-range transported Saharan air layers in the western North Atlantic trades indicate increased amounts of water vapor within the dust layers compared to the surrounding dry free atmosphere. This study investigates the impact of such enhanced water vapor concentrations on radiative heating. Therefore, spatially high resolved airborne high spectral resolution and differential absorption lidar measurements are used for the parametrization of aerosol optical properties and water vapor concentrations in radiative transfer calculations. Heating rates that are calculated under consideration of the measured water vapor distribution strongly differ from heating rates that are derived under assumption of an atmospheric reference water vapor profile which is steadily decreasing with altitude. Results highlight that water vapor represents a major radiative driver for dust layer vertical mixing and the maintenance of bounding inversions at the top and bottom of the dust layer. Article in Journal/Newspaper North Atlantic German Aerospace Center: elib - DLR electronic library Geophysical Research Letters 46 24 14854 14862
institution Open Polar
collection German Aerospace Center: elib - DLR electronic library
op_collection_id ftdlr
language English
topic Institut für Physik der Atmosphäre
spellingShingle Institut für Physik der Atmosphäre
Gutleben, Manuel
Groß, Silke
Wirth, Martin
Emde, Claudia
Mayer, Bernhard
Impacts of water vapor on Saharan air layer radiative heating
topic_facet Institut für Physik der Atmosphäre
description Abstract Airborne lidar observations of long-range transported Saharan air layers in the western North Atlantic trades indicate increased amounts of water vapor within the dust layers compared to the surrounding dry free atmosphere. This study investigates the impact of such enhanced water vapor concentrations on radiative heating. Therefore, spatially high resolved airborne high spectral resolution and differential absorption lidar measurements are used for the parametrization of aerosol optical properties and water vapor concentrations in radiative transfer calculations. Heating rates that are calculated under consideration of the measured water vapor distribution strongly differ from heating rates that are derived under assumption of an atmospheric reference water vapor profile which is steadily decreasing with altitude. Results highlight that water vapor represents a major radiative driver for dust layer vertical mixing and the maintenance of bounding inversions at the top and bottom of the dust layer.
format Article in Journal/Newspaper
author Gutleben, Manuel
Groß, Silke
Wirth, Martin
Emde, Claudia
Mayer, Bernhard
author_facet Gutleben, Manuel
Groß, Silke
Wirth, Martin
Emde, Claudia
Mayer, Bernhard
author_sort Gutleben, Manuel
title Impacts of water vapor on Saharan air layer radiative heating
title_short Impacts of water vapor on Saharan air layer radiative heating
title_full Impacts of water vapor on Saharan air layer radiative heating
title_fullStr Impacts of water vapor on Saharan air layer radiative heating
title_full_unstemmed Impacts of water vapor on Saharan air layer radiative heating
title_sort impacts of water vapor on saharan air layer radiative heating
publisher Wiley
publishDate 2019
url https://elib.dlr.de/134038/
https://elib.dlr.de/134038/1/Gutleben_et_al-2019-Geophysical_Research_Letters.pdf
https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/2019GL085344
genre North Atlantic
genre_facet North Atlantic
op_relation https://elib.dlr.de/134038/1/Gutleben_et_al-2019-Geophysical_Research_Letters.pdf
Gutleben, Manuel und Groß, Silke und Wirth, Martin und Emde, Claudia und Mayer, Bernhard (2019) Impacts of water vapor on Saharan air layer radiative heating. Geophysical Research Letters, 46 (24), Seiten 14854-14862. Wiley. doi:10.1029/2019GL085344 <https://doi.org/10.1029/2019GL085344>. ISSN 0094-8276.
op_rights cc_by
op_doi https://doi.org/10.1029/2019GL085344
container_title Geophysical Research Letters
container_volume 46
container_issue 24
container_start_page 14854
op_container_end_page 14862
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