Dynamical Meteorology of the Equatorial and Extratropical Stratosphere
Observational studies were performed of westward propagating synoptic scale waves in the tropical troposphere, the structure of monsoon circulations in the upper troposphere and lower stratosphere, and zonally propagating features in deep tropical convection. The effect of the quasi-biennial oscilla...
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ftnasantrs:oai:casi.ntrs.nasa.gov:19990116841 2023-05-15T14:59:32+02:00 Dynamical Meteorology of the Equatorial and Extratropical Stratosphere Dunkerton, Tomothy Unclassified, Unlimited, Publicly available Oct. 06, 1999 application/pdf http://hdl.handle.net/2060/19990116841 unknown Document ID: 19990116841 http://hdl.handle.net/2060/19990116841 No Copyright CASI Geophysics NWRA-CR-99-R203 1999 ftnasantrs 2019-08-31T23:03:23Z Observational studies were performed of westward propagating synoptic scale waves in the tropical troposphere, the structure of monsoon circulations in the upper troposphere and lower stratosphere, and zonally propagating features in deep tropical convection. The effect of the quasi-biennial oscillation (QBO) were investigated, and a numerical study of the QBO was performed using a two-dimensional model, highlighting the role of gravity waves in the momentum balance of the QBO. Vertical coupling of the troposphere and stratosphere was examined in polar regions on intraseasonal and interannual timescales. A deep circumpolar mode was discovered, now known as the Arctic Oscillation. Other/Unknown Material Arctic NASA Technical Reports Server (NTRS) Arctic |
institution |
Open Polar |
collection |
NASA Technical Reports Server (NTRS) |
op_collection_id |
ftnasantrs |
language |
unknown |
topic |
Geophysics |
spellingShingle |
Geophysics Dunkerton, Tomothy Dynamical Meteorology of the Equatorial and Extratropical Stratosphere |
topic_facet |
Geophysics |
description |
Observational studies were performed of westward propagating synoptic scale waves in the tropical troposphere, the structure of monsoon circulations in the upper troposphere and lower stratosphere, and zonally propagating features in deep tropical convection. The effect of the quasi-biennial oscillation (QBO) were investigated, and a numerical study of the QBO was performed using a two-dimensional model, highlighting the role of gravity waves in the momentum balance of the QBO. Vertical coupling of the troposphere and stratosphere was examined in polar regions on intraseasonal and interannual timescales. A deep circumpolar mode was discovered, now known as the Arctic Oscillation. |
format |
Other/Unknown Material |
author |
Dunkerton, Tomothy |
author_facet |
Dunkerton, Tomothy |
author_sort |
Dunkerton, Tomothy |
title |
Dynamical Meteorology of the Equatorial and Extratropical Stratosphere |
title_short |
Dynamical Meteorology of the Equatorial and Extratropical Stratosphere |
title_full |
Dynamical Meteorology of the Equatorial and Extratropical Stratosphere |
title_fullStr |
Dynamical Meteorology of the Equatorial and Extratropical Stratosphere |
title_full_unstemmed |
Dynamical Meteorology of the Equatorial and Extratropical Stratosphere |
title_sort |
dynamical meteorology of the equatorial and extratropical stratosphere |
publishDate |
1999 |
url |
http://hdl.handle.net/2060/19990116841 |
op_coverage |
Unclassified, Unlimited, Publicly available |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic |
genre_facet |
Arctic |
op_source |
CASI |
op_relation |
Document ID: 19990116841 http://hdl.handle.net/2060/19990116841 |
op_rights |
No Copyright |
_version_ |
1766331640898912256 |