Spectral characteristics of spring arctic mesosphere dynamics
Abstract. The spring of 1997 has represented a stable period of operation for the joint University of Tromsù / University of Saskatchewan MF radar, being between refurbishment and upgrades. We examine the horizontal winds from the February to June inclusive and also include estimates of energy dissi...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.371.4609 2023-05-15T15:01:09+02:00 Spectral characteristics of spring arctic mesosphere dynamics C. M. Hall A. H. Manson C. E. Meek The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.371.4609 http://hal.archives-ouvertes.fr/docs/00/31/64/87/PDF/angeo-16-1607-1998.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.371.4609 http://hal.archives-ouvertes.fr/docs/00/31/64/87/PDF/angeo-16-1607-1998.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://hal.archives-ouvertes.fr/docs/00/31/64/87/PDF/angeo-16-1607-1998.pdf text ftciteseerx 2016-01-08T01:19:41Z Abstract. The spring of 1997 has represented a stable period of operation for the joint University of Tromsù / University of Saskatchewan MF radar, being between refurbishment and upgrades. We examine the horizontal winds from the February to June inclusive and also include estimates of energy dissipation rates derived from signal fading times and presented as upper limits on the turbulent energy dissipation rate, e. Here we address the periodicity in the dynamics of the upper mesosphere for time scales from hours to one month. Thus, we are able to examine the changes in the spectral signature of the mesospheric dynamics during the transition from winter to summer states. Key words. Meteorology and atmospheric dynamics (middle atmosphere dynamics; turbulence; waves and tides). Text Arctic Unknown Arctic |
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English |
description |
Abstract. The spring of 1997 has represented a stable period of operation for the joint University of Tromsù / University of Saskatchewan MF radar, being between refurbishment and upgrades. We examine the horizontal winds from the February to June inclusive and also include estimates of energy dissipation rates derived from signal fading times and presented as upper limits on the turbulent energy dissipation rate, e. Here we address the periodicity in the dynamics of the upper mesosphere for time scales from hours to one month. Thus, we are able to examine the changes in the spectral signature of the mesospheric dynamics during the transition from winter to summer states. Key words. Meteorology and atmospheric dynamics (middle atmosphere dynamics; turbulence; waves and tides). |
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The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
C. M. Hall A. H. Manson C. E. Meek |
spellingShingle |
C. M. Hall A. H. Manson C. E. Meek Spectral characteristics of spring arctic mesosphere dynamics |
author_facet |
C. M. Hall A. H. Manson C. E. Meek |
author_sort |
C. M. Hall |
title |
Spectral characteristics of spring arctic mesosphere dynamics |
title_short |
Spectral characteristics of spring arctic mesosphere dynamics |
title_full |
Spectral characteristics of spring arctic mesosphere dynamics |
title_fullStr |
Spectral characteristics of spring arctic mesosphere dynamics |
title_full_unstemmed |
Spectral characteristics of spring arctic mesosphere dynamics |
title_sort |
spectral characteristics of spring arctic mesosphere dynamics |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.371.4609 http://hal.archives-ouvertes.fr/docs/00/31/64/87/PDF/angeo-16-1607-1998.pdf |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic |
genre_facet |
Arctic |
op_source |
http://hal.archives-ouvertes.fr/docs/00/31/64/87/PDF/angeo-16-1607-1998.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.371.4609 http://hal.archives-ouvertes.fr/docs/00/31/64/87/PDF/angeo-16-1607-1998.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766333192085700608 |