Upper atmosphere circulation and wave motion

A fully automated partial-reflection, spaced antema, winds system has been developed at Birdlings Flat (44°S), using real-time data processing on a miniconputer. This enables almost continuous measurement of the winds between 65km and l00km to be made. Optimal data selection criteria for this locat...

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Main Author: Smith, M. J.
Language:en
Published: University of Canterbury. Physics 2011
Online Access:http://hdl.handle.net/10092/6101
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spelling ndltd-canterbury.ac.nz-oai-ir.canterbury.ac.nz-10092-61012015-03-30T15:30:47ZUpper atmosphere circulation and wave motionSmith, M. J.A fully automated partial-reflection, spaced antema, winds system has been developed at Birdlings Flat (44°S), using real-time data processing on a miniconputer. This enables almost continuous measurement of the winds between 65km and l00km to be made. Optimal data selection criteria for this location, and the value of simplifications in the data analysis and collection, are examined. The seasonal variation of the prevailing wind is studied in detail. The circulation in the mesosphere is characterized by strong westward winds in summer, and more variable eastward winds in winter. The circulation in the lower thermosphere is in the opposite direction. Long-period wind oscillations are observed throughout the year, and an identification of some of these with atmospheric normal modes, is strongly suggested in summer. Baroclinic instability may also occur in the summer mesosphere. Stratospheric disturbances are found to have significant effects in the 65 - 100 km region. The variation of atmospheric tides with height end season is also examined.University of Canterbury. Physics2011-12-14T23:02:06Z2011-12-14T23:02:06Z1981Electronic thesis or dissertationTexthttp://hdl.handle.net/10092/6101enNZCUCopyright M. J. Smithhttp://library.canterbury.ac.nz/thesis/etheses_copyright.shtml
collection NDLTD
language en
sources NDLTD
description A fully automated partial-reflection, spaced antema, winds system has been developed at Birdlings Flat (44°S), using real-time data processing on a miniconputer. This enables almost continuous measurement of the winds between 65km and l00km to be made. Optimal data selection criteria for this location, and the value of simplifications in the data analysis and collection, are examined. The seasonal variation of the prevailing wind is studied in detail. The circulation in the mesosphere is characterized by strong westward winds in summer, and more variable eastward winds in winter. The circulation in the lower thermosphere is in the opposite direction. Long-period wind oscillations are observed throughout the year, and an identification of some of these with atmospheric normal modes, is strongly suggested in summer. Baroclinic instability may also occur in the summer mesosphere. Stratospheric disturbances are found to have significant effects in the 65 - 100 km region. The variation of atmospheric tides with height end season is also examined.
author Smith, M. J.
spellingShingle Smith, M. J.
Upper atmosphere circulation and wave motion
author_facet Smith, M. J.
author_sort Smith, M. J.
title Upper atmosphere circulation and wave motion
title_short Upper atmosphere circulation and wave motion
title_full Upper atmosphere circulation and wave motion
title_fullStr Upper atmosphere circulation and wave motion
title_full_unstemmed Upper atmosphere circulation and wave motion
title_sort upper atmosphere circulation and wave motion
publisher University of Canterbury. Physics
publishDate 2011
url http://hdl.handle.net/10092/6101
work_keys_str_mv AT smithmj upperatmospherecirculationandwavemotion
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