Please use this identifier to cite or link to this item:
https://hdl.handle.net/2440/12557
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Full metadata record
DC Field | Value | Language |
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dc.contributor.author | Lawrence, B. | - |
dc.contributor.author | Fraser, G. | - |
dc.contributor.author | Vincent, R. | - |
dc.contributor.author | Phillips, A. | - |
dc.date.issued | 1995 | - |
dc.identifier.citation | Journal of Geophysical Research, 1995; 100(D9):18899-18908 | - |
dc.identifier.issn | 0148-0227 | - |
dc.identifier.uri | http://hdl.handle.net/2440/12557 | - |
dc.description.abstract | A zonal wave number one eastward propagating planetary wave observed in the high latitude winter stratosphere with a period near 4 days has been studied by a number of previous authors. Radar observations coupled with stratospheric analyses are here used to demonstrate that this wave, known as the 4-day wave, extends into the Antarctic upper mesosphere. Previous workers have asserted that the wave is a manifestation of the observation of warm pools rotating in the polar vortex, and that the pool seems to behave in a quasi-nondispersive manner. The observation of the 4-day wave in the upper mesosophere presented here appears to validate previous claims that the warm pools are being maintained by wavelike dynamics, rather than simple advection. | - |
dc.description.statementofresponsibility | Bryan N. Lawrence, Grahame J. Fraser, Robert A. Vincent and Andre Phillips | - |
dc.language.iso | en | - |
dc.publisher | American Geophysical Union | - |
dc.rights | Copyright 1995 by the American Geophysical Union | - |
dc.source.uri | http://dx.doi.org/10.1029/95jd01168 | - |
dc.title | The 4-day wave in the Antarctic mesosphere | - |
dc.type | Journal article | - |
dc.identifier.doi | 10.1029/95JD01168 | - |
pubs.publication-status | Published | - |
dc.identifier.orcid | Vincent, R. [0000-0001-6559-6544] | - |
Appears in Collections: | Aurora harvest 2 Physics publications |
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hdl_12557.pdf | Published version | 914.33 kB | Adobe PDF | View/Open |
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