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...
Published in: | Geophysical Research Letters |
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Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Wiley
2019
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Subjects: | |
Online Access: | https://elib.dlr.de/134038/ https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/2019GL085344 |
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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 |
collection | Unknown |
container_issue | 24 |
container_start_page | 14854 |
container_title | Geophysical Research Letters |
container_volume | 46 |
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 |
genre | North Atlantic |
genre_facet | North Atlantic |
id | ftdlr:oai:elib.dlr.de:134038 |
institution | Open Polar |
language | English |
op_collection_id | ftdlr |
op_container_end_page | 14862 |
op_doi | https://doi.org/10.1029/2019GL085344 |
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 |
publishDate | 2019 |
publisher | Wiley |
record_format | openpolar |
spelling | ftdlr:oai:elib.dlr.de:134038 2025-06-15T14:43:04+00:00 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://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 2025-06-04T04:58:07Z 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 Unknown Geophysical Research Letters 46 24 14854 14862 |
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 |
title | 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_short | Impacts of water vapor on Saharan air layer radiative heating |
title_sort | impacts of water vapor on saharan air layer radiative heating |
topic | Institut für Physik der Atmosphäre |
topic_facet | Institut für Physik der Atmosphäre |
url | https://elib.dlr.de/134038/ https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/2019GL085344 |