Preliminary results of lidar based studies of the aerosol vertical distribution in the lower troposphere over urban coastal areas

The paper reports the results of lidar measurements performed in the lower troposphere during several measurement sessions in Athens (Greece) in 2000. For the sake of comparison, results of a similar study performed in Kołobrzeg (Poland) in 2001 are also given. These data indicate that t...

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Main Authors: Marek Ha³as, Zdzis³aw B³aszczak, Józef Grabowski, Alexandros Papayannis, Tymon Zieliñski
Format: Article
Language:English
Published: Elsevier 2004-09-01
Series:Oceanologia
Subjects:
Online Access:http://www.iopan.gda.pl/oceanologia/46_3.html#A2
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spelling doaj-d031e6ac68b241ebba0a02d423d5c3a72020-11-24T23:25:44ZengElsevierOceanologia0078-32342004-09-01463347364Preliminary results of lidar based studies of the aerosol vertical distribution in the lower troposphere over urban coastal areasMarek Ha³asZdzis³aw B³aszczakJózef GrabowskiAlexandros PapayannisTymon ZieliñskiThe paper reports the results of lidar measurements performed in the lower troposphere during several measurement sessions in Athens (Greece) in 2000. For the sake of comparison, results of a similar study performed in Kołobrzeg (Poland) in 2001 are also given. These data indicate that the exhaust gases produced by motor transportation in the cities resulted in the formation of an inversion layer. The rate of convection of the inversion layer depends on the intensity of sunlight, the strength of winds and the morphology of the land. The inversion layer reaches the highest altitudes in the middle of summer, lower in early and late summer and the lowest in autumn. Over the sea the inversion layer altitude extends to several meters, but on moving inland it rises to a few hundred meters.http://www.iopan.gda.pl/oceanologia/46_3.html#A2AerosolVertical profileUrban areaLidar
collection DOAJ
language English
format Article
sources DOAJ
author Marek Ha³as
Zdzis³aw B³aszczak
Józef Grabowski
Alexandros Papayannis
Tymon Zieliñski
spellingShingle Marek Ha³as
Zdzis³aw B³aszczak
Józef Grabowski
Alexandros Papayannis
Tymon Zieliñski
Preliminary results of lidar based studies of the aerosol vertical distribution in the lower troposphere over urban coastal areas
Oceanologia
Aerosol
Vertical profile
Urban area
Lidar
author_facet Marek Ha³as
Zdzis³aw B³aszczak
Józef Grabowski
Alexandros Papayannis
Tymon Zieliñski
author_sort Marek Ha³as
title Preliminary results of lidar based studies of the aerosol vertical distribution in the lower troposphere over urban coastal areas
title_short Preliminary results of lidar based studies of the aerosol vertical distribution in the lower troposphere over urban coastal areas
title_full Preliminary results of lidar based studies of the aerosol vertical distribution in the lower troposphere over urban coastal areas
title_fullStr Preliminary results of lidar based studies of the aerosol vertical distribution in the lower troposphere over urban coastal areas
title_full_unstemmed Preliminary results of lidar based studies of the aerosol vertical distribution in the lower troposphere over urban coastal areas
title_sort preliminary results of lidar based studies of the aerosol vertical distribution in the lower troposphere over urban coastal areas
publisher Elsevier
series Oceanologia
issn 0078-3234
publishDate 2004-09-01
description The paper reports the results of lidar measurements performed in the lower troposphere during several measurement sessions in Athens (Greece) in 2000. For the sake of comparison, results of a similar study performed in Kołobrzeg (Poland) in 2001 are also given. These data indicate that the exhaust gases produced by motor transportation in the cities resulted in the formation of an inversion layer. The rate of convection of the inversion layer depends on the intensity of sunlight, the strength of winds and the morphology of the land. The inversion layer reaches the highest altitudes in the middle of summer, lower in early and late summer and the lowest in autumn. Over the sea the inversion layer altitude extends to several meters, but on moving inland it rises to a few hundred meters.
topic Aerosol
Vertical profile
Urban area
Lidar
url http://www.iopan.gda.pl/oceanologia/46_3.html#A2
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