AEROSOL-CLOUD INTERACTION DURING THE TRANSITION TIME PERIOD OF ARCTIC HAZE TO CLEAN SUMMER CONDITIONS
The transition from Arctic haze (a large amount of aerosols coming from Eurasian industrial areas accumulate over the Arctic and cover the Arctic by a layer of this smog-like haze of the size of the continent of Africa) to clean summer conditions is quite sharp due to a radical change in atmospheric
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.543.9552 2023-05-15T14:31:57+02:00 AEROSOL-CLOUD INTERACTION DURING THE TRANSITION TIME PERIOD OF ARCTIC HAZE TO CLEAN SUMMER CONDITIONS A. Schwarzenboeck C. Duroure J. F. Gayet A. Herber R. Krecji R. Lefevre A. Minikin R. Neuber V. Shcherbakov J. Stroem S. Yamagata The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.543.9552 http://elib.dlr.de/10180/1/abstract-727.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.543.9552 http://elib.dlr.de/10180/1/abstract-727.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://elib.dlr.de/10180/1/abstract-727.pdf Arctic aerosol aerosol-cloud interaction arctic mixed phase clouds indirect aerosol effect text ftciteseerx 2016-01-08T11:12:10Z The transition from Arctic haze (a large amount of aerosols coming from Eurasian industrial areas accumulate over the Arctic and cover the Arctic by a layer of this smog-like haze of the size of the continent of Africa) to clean summer conditions is quite sharp due to a radical change in atmospheric Text Arctic Unknown Arctic |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
ftciteseerx |
language |
English |
topic |
Arctic aerosol aerosol-cloud interaction arctic mixed phase clouds indirect aerosol effect |
spellingShingle |
Arctic aerosol aerosol-cloud interaction arctic mixed phase clouds indirect aerosol effect A. Schwarzenboeck C. Duroure J. F. Gayet A. Herber R. Krecji R. Lefevre A. Minikin R. Neuber V. Shcherbakov J. Stroem S. Yamagata AEROSOL-CLOUD INTERACTION DURING THE TRANSITION TIME PERIOD OF ARCTIC HAZE TO CLEAN SUMMER CONDITIONS |
topic_facet |
Arctic aerosol aerosol-cloud interaction arctic mixed phase clouds indirect aerosol effect |
description |
The transition from Arctic haze (a large amount of aerosols coming from Eurasian industrial areas accumulate over the Arctic and cover the Arctic by a layer of this smog-like haze of the size of the continent of Africa) to clean summer conditions is quite sharp due to a radical change in atmospheric |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
A. Schwarzenboeck C. Duroure J. F. Gayet A. Herber R. Krecji R. Lefevre A. Minikin R. Neuber V. Shcherbakov J. Stroem S. Yamagata |
author_facet |
A. Schwarzenboeck C. Duroure J. F. Gayet A. Herber R. Krecji R. Lefevre A. Minikin R. Neuber V. Shcherbakov J. Stroem S. Yamagata |
author_sort |
A. Schwarzenboeck |
title |
AEROSOL-CLOUD INTERACTION DURING THE TRANSITION TIME PERIOD OF ARCTIC HAZE TO CLEAN SUMMER CONDITIONS |
title_short |
AEROSOL-CLOUD INTERACTION DURING THE TRANSITION TIME PERIOD OF ARCTIC HAZE TO CLEAN SUMMER CONDITIONS |
title_full |
AEROSOL-CLOUD INTERACTION DURING THE TRANSITION TIME PERIOD OF ARCTIC HAZE TO CLEAN SUMMER CONDITIONS |
title_fullStr |
AEROSOL-CLOUD INTERACTION DURING THE TRANSITION TIME PERIOD OF ARCTIC HAZE TO CLEAN SUMMER CONDITIONS |
title_full_unstemmed |
AEROSOL-CLOUD INTERACTION DURING THE TRANSITION TIME PERIOD OF ARCTIC HAZE TO CLEAN SUMMER CONDITIONS |
title_sort |
aerosol-cloud interaction during the transition time period of arctic haze to clean summer conditions |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.543.9552 http://elib.dlr.de/10180/1/abstract-727.pdf |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic |
genre_facet |
Arctic |
op_source |
http://elib.dlr.de/10180/1/abstract-727.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.543.9552 http://elib.dlr.de/10180/1/abstract-727.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766305454415151104 |