Wind-driven influences on aerosol light scattering in north-east atlantic air

Ten years (2001-2010) of aerosol light-scattering measurements in N.E. Atlantic marine air are analysed to determine wind-speed related influences on scattering properties. The scattering coefficient and the backscattering coefficient dependency on wind speed (U) was determined for the winter (Low B...

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Published in:Geophysical Research Letters
Main Authors: Vaishya, Aditya, Jennings, S. Gerard, O'Dowd, Colin
Format: Article in Journal/Newspaper
Language:unknown
Published: Wiley-Blackwell 2012
Subjects:
Online Access:http://hdl.handle.net/10379/14250
https://doi.org/10.1029/2011gl050556
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spelling ftnuigalway:oai:aran.library.nuigalway.ie/:10379/14250 2023-06-11T04:15:07+02:00 Wind-driven influences on aerosol light scattering in north-east atlantic air Vaishya, Aditya Jennings, S. Gerard O'Dowd, Colin 2012-03-01 http://hdl.handle.net/10379/14250 https://doi.org/10.1029/2011gl050556 unknown Wiley-Blackwell Geophysical Research Letters Vaishya, Aditya; Jennings, S. Gerard; O'Dowd, Colin (2012). Wind-driven influences on aerosol light scattering in north-east atlantic air. Geophysical Research Letters 39 , 0094-8276 http://hdl.handle.net/10379/14250 doi:10.1029/2011gl050556 Attribution-NonCommercial-NoDerivs 3.0 Ireland https://creativecommons.org/licenses/by-nc-nd/3.0/ie/ mace head atmospheric aerosol sea-salt marine nephelometer 3-wavelength submicron particles station coast Article 2012 ftnuigalway https://doi.org/10.1029/2011gl050556 2023-05-28T18:06:03Z Ten years (2001-2010) of aerosol light-scattering measurements in N.E. Atlantic marine air are analysed to determine wind-speed related influences on scattering properties. The scattering coefficient and the backscattering coefficient dependency on wind speed (U) was determined for the winter (Low Biological Activity-LBA) and the summer seasons (High Biological Activity-HBA), and was found to be dependent on similar to U-2. In spite of having a U-2 dependency, scattering properties for the LBA-period are approximately twice those of the HBA-period. 96% of the LBA-HBA scattering difference can be explained by the combined effects of size distribution and refractive index differences while 70% of the scattering difference can be attributed to a difference in refractive index alone resulting from organic-matter enrichment during the HBA period. The 550 nm scattering coefficient was similar to 70 Mm(-1) for similar to 25 ms(-1) wind speeds, which is considerably higher than that encountered under polluted air masses in the same region. Citation: Vaishya, A., S. G. Jennings, and C. O'Dowd (2012), Wind-driven influences on aerosol light scattering in north-east Atlantic air, Geophys. Res. Lett., 39, L05805, doi:10.1029/2011GL050556. Article in Journal/Newspaper North East Atlantic National University of Ireland (NUI), Galway: ARAN Mace ENVELOPE(155.883,155.883,-81.417,-81.417) Jennings ENVELOPE(72.556,72.556,-70.145,-70.145) Geophysical Research Letters 39 5 n/a n/a
institution Open Polar
collection National University of Ireland (NUI), Galway: ARAN
op_collection_id ftnuigalway
language unknown
topic mace head
atmospheric aerosol
sea-salt
marine
nephelometer
3-wavelength
submicron
particles
station
coast
spellingShingle mace head
atmospheric aerosol
sea-salt
marine
nephelometer
3-wavelength
submicron
particles
station
coast
Vaishya, Aditya
Jennings, S. Gerard
O'Dowd, Colin
Wind-driven influences on aerosol light scattering in north-east atlantic air
topic_facet mace head
atmospheric aerosol
sea-salt
marine
nephelometer
3-wavelength
submicron
particles
station
coast
description Ten years (2001-2010) of aerosol light-scattering measurements in N.E. Atlantic marine air are analysed to determine wind-speed related influences on scattering properties. The scattering coefficient and the backscattering coefficient dependency on wind speed (U) was determined for the winter (Low Biological Activity-LBA) and the summer seasons (High Biological Activity-HBA), and was found to be dependent on similar to U-2. In spite of having a U-2 dependency, scattering properties for the LBA-period are approximately twice those of the HBA-period. 96% of the LBA-HBA scattering difference can be explained by the combined effects of size distribution and refractive index differences while 70% of the scattering difference can be attributed to a difference in refractive index alone resulting from organic-matter enrichment during the HBA period. The 550 nm scattering coefficient was similar to 70 Mm(-1) for similar to 25 ms(-1) wind speeds, which is considerably higher than that encountered under polluted air masses in the same region. Citation: Vaishya, A., S. G. Jennings, and C. O'Dowd (2012), Wind-driven influences on aerosol light scattering in north-east Atlantic air, Geophys. Res. Lett., 39, L05805, doi:10.1029/2011GL050556.
format Article in Journal/Newspaper
author Vaishya, Aditya
Jennings, S. Gerard
O'Dowd, Colin
author_facet Vaishya, Aditya
Jennings, S. Gerard
O'Dowd, Colin
author_sort Vaishya, Aditya
title Wind-driven influences on aerosol light scattering in north-east atlantic air
title_short Wind-driven influences on aerosol light scattering in north-east atlantic air
title_full Wind-driven influences on aerosol light scattering in north-east atlantic air
title_fullStr Wind-driven influences on aerosol light scattering in north-east atlantic air
title_full_unstemmed Wind-driven influences on aerosol light scattering in north-east atlantic air
title_sort wind-driven influences on aerosol light scattering in north-east atlantic air
publisher Wiley-Blackwell
publishDate 2012
url http://hdl.handle.net/10379/14250
https://doi.org/10.1029/2011gl050556
long_lat ENVELOPE(155.883,155.883,-81.417,-81.417)
ENVELOPE(72.556,72.556,-70.145,-70.145)
geographic Mace
Jennings
geographic_facet Mace
Jennings
genre North East Atlantic
genre_facet North East Atlantic
op_relation Geophysical Research Letters
Vaishya, Aditya; Jennings, S. Gerard; O'Dowd, Colin (2012). Wind-driven influences on aerosol light scattering in north-east atlantic air. Geophysical Research Letters 39 ,
0094-8276
http://hdl.handle.net/10379/14250
doi:10.1029/2011gl050556
op_rights Attribution-NonCommercial-NoDerivs 3.0 Ireland
https://creativecommons.org/licenses/by-nc-nd/3.0/ie/
op_doi https://doi.org/10.1029/2011gl050556
container_title Geophysical Research Letters
container_volume 39
container_issue 5
container_start_page n/a
op_container_end_page n/a
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