Lidar observations of the Fe layer and temperatures in the polar mesopause region
Lidar observations of the mesospheric Fe layer and temperatures have been performed at Davis, Antarctica and ALOMAR, Norway. Large-scale transport is the primary cause of the seasonal variation of the Fe layer. An uptake of metal atoms on ice particles, as well as temperature-dependent chemistry, pl...
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Universität Rostock
2017
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ftdatacite:10.18453/rosdok_id00001910 2023-05-15T13:32:01+02:00 Lidar observations of the Fe layer and temperatures in the polar mesopause region Viehl, Timo Pascal 2017 https://dx.doi.org/10.18453/rosdok_id00001910 http://rosdok.uni-rostock.de/resolve/id/rosdok_disshab_0000001732 en eng Universität Rostock 550 Earth sciences Text article-journal ScholarlyArticle 2017 ftdatacite https://doi.org/10.18453/rosdok_id00001910 2021-11-05T12:55:41Z Lidar observations of the mesospheric Fe layer and temperatures have been performed at Davis, Antarctica and ALOMAR, Norway. Large-scale transport is the primary cause of the seasonal variation of the Fe layer. An uptake of metal atoms on ice particles, as well as temperature-dependent chemistry, play secondary roles for the seasonal variation. The regular bottomside extension of the Fe layer in the upper mesosphere and lower thermosphere (MLT) is caused by the direct photolysis of FeOH. Temperature and Fe density observations reveal unexpectedly strong tidal modulations in the polar MLT. Text Antarc* Antarctica DataCite Metadata Store (German National Library of Science and Technology) Alomar ENVELOPE(-67.083,-67.083,-68.133,-68.133) Norway |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
550 Earth sciences |
spellingShingle |
550 Earth sciences Viehl, Timo Pascal Lidar observations of the Fe layer and temperatures in the polar mesopause region |
topic_facet |
550 Earth sciences |
description |
Lidar observations of the mesospheric Fe layer and temperatures have been performed at Davis, Antarctica and ALOMAR, Norway. Large-scale transport is the primary cause of the seasonal variation of the Fe layer. An uptake of metal atoms on ice particles, as well as temperature-dependent chemistry, play secondary roles for the seasonal variation. The regular bottomside extension of the Fe layer in the upper mesosphere and lower thermosphere (MLT) is caused by the direct photolysis of FeOH. Temperature and Fe density observations reveal unexpectedly strong tidal modulations in the polar MLT. |
format |
Text |
author |
Viehl, Timo Pascal |
author_facet |
Viehl, Timo Pascal |
author_sort |
Viehl, Timo Pascal |
title |
Lidar observations of the Fe layer and temperatures in the polar mesopause region |
title_short |
Lidar observations of the Fe layer and temperatures in the polar mesopause region |
title_full |
Lidar observations of the Fe layer and temperatures in the polar mesopause region |
title_fullStr |
Lidar observations of the Fe layer and temperatures in the polar mesopause region |
title_full_unstemmed |
Lidar observations of the Fe layer and temperatures in the polar mesopause region |
title_sort |
lidar observations of the fe layer and temperatures in the polar mesopause region |
publisher |
Universität Rostock |
publishDate |
2017 |
url |
https://dx.doi.org/10.18453/rosdok_id00001910 http://rosdok.uni-rostock.de/resolve/id/rosdok_disshab_0000001732 |
long_lat |
ENVELOPE(-67.083,-67.083,-68.133,-68.133) |
geographic |
Alomar Norway |
geographic_facet |
Alomar Norway |
genre |
Antarc* Antarctica |
genre_facet |
Antarc* Antarctica |
op_doi |
https://doi.org/10.18453/rosdok_id00001910 |
_version_ |
1766023536293445632 |