Out of Africa: High aerosol concentrations in the upper troposphere over Africa

In the year 2000, six flights (three southbound and three northbound) of the CARIBIC project were conducted between Germany and two destinations in the southern hemisphere (Windhoek, Namibia and Cape Town, South Africa). In the present report, results on particle number concentrations are discus...

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Main Authors: J. Heintzenberg, M. Hermann, D. Theiss
Format: Article
Language:English
Published: Copernicus Publications 2003-01-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/3/1191/2003/acp-3-1191-2003.pdf
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spelling doaj-951191a4782b4044be58f37cb1b3fd122020-11-24T22:17:46ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242003-01-013411911198Out of Africa: High aerosol concentrations in the upper troposphere over AfricaJ. HeintzenbergM. HermannD. TheissIn the year 2000, six flights (three southbound and three northbound) of the CARIBIC project were conducted between Germany and two destinations in the southern hemisphere (Windhoek, Namibia and Cape Town, South Africa). In the present report, results on particle number concentrations are discussed in three size ranges (>4 nm, >12 nm, and >18 nm particle diameter) during the unique transequatorial Africa flights. The flights covered a total of about 80 h in May, July, and December. Thus, no claim can be made for long-term representativeness of the aerosol data. Nevertheless, they are the first upper systematic tropospheric transequatorial aerosol profiles over Africa. The average aerosol results show a broad maximum, roughly symmetrical to the equator, which compares well in latitudinal extent to a maximum of CO concentrations measured on the same flights. This export of continental surface aerosol to the upper troposphere will be dispersed on a global scale both with the easterly flow near the equator and with the westerlies in the adjacent subtropical regions. There was strong evidence of recent new particle formation before aerosol arrival at flight level, in particular during the time periods between 9:00 and 13:00 local time over Africa. Direct and indirect climate effects of the respective particulate matter remain to be investigated by future flights with the ongoing extension of the CARIBIC payload towards size-resolved measurements above 100 nm particle diameter. At the same time global chemical transport models and aerosol dynamics models need to be extended to be able to reproduce the CARIBIC findings over Africa.http://www.atmos-chem-phys.net/3/1191/2003/acp-3-1191-2003.pdf
collection DOAJ
language English
format Article
sources DOAJ
author J. Heintzenberg
M. Hermann
D. Theiss
spellingShingle J. Heintzenberg
M. Hermann
D. Theiss
Out of Africa: High aerosol concentrations in the upper troposphere over Africa
Atmospheric Chemistry and Physics
author_facet J. Heintzenberg
M. Hermann
D. Theiss
author_sort J. Heintzenberg
title Out of Africa: High aerosol concentrations in the upper troposphere over Africa
title_short Out of Africa: High aerosol concentrations in the upper troposphere over Africa
title_full Out of Africa: High aerosol concentrations in the upper troposphere over Africa
title_fullStr Out of Africa: High aerosol concentrations in the upper troposphere over Africa
title_full_unstemmed Out of Africa: High aerosol concentrations in the upper troposphere over Africa
title_sort out of africa: high aerosol concentrations in the upper troposphere over africa
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2003-01-01
description In the year 2000, six flights (three southbound and three northbound) of the CARIBIC project were conducted between Germany and two destinations in the southern hemisphere (Windhoek, Namibia and Cape Town, South Africa). In the present report, results on particle number concentrations are discussed in three size ranges (>4 nm, >12 nm, and >18 nm particle diameter) during the unique transequatorial Africa flights. The flights covered a total of about 80 h in May, July, and December. Thus, no claim can be made for long-term representativeness of the aerosol data. Nevertheless, they are the first upper systematic tropospheric transequatorial aerosol profiles over Africa. The average aerosol results show a broad maximum, roughly symmetrical to the equator, which compares well in latitudinal extent to a maximum of CO concentrations measured on the same flights. This export of continental surface aerosol to the upper troposphere will be dispersed on a global scale both with the easterly flow near the equator and with the westerlies in the adjacent subtropical regions. There was strong evidence of recent new particle formation before aerosol arrival at flight level, in particular during the time periods between 9:00 and 13:00 local time over Africa. Direct and indirect climate effects of the respective particulate matter remain to be investigated by future flights with the ongoing extension of the CARIBIC payload towards size-resolved measurements above 100 nm particle diameter. At the same time global chemical transport models and aerosol dynamics models need to be extended to be able to reproduce the CARIBIC findings over Africa.
url http://www.atmos-chem-phys.net/3/1191/2003/acp-3-1191-2003.pdf
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