On the maintenance of the axisymmetric part of the flow in the atmosphere
dc.contributor.author | Derome, Jacques F. (Jacques Florian) | en_US |
dc.contributor.author | Wiin-Nielsen, Aksel C. | en_US |
dc.date.accessioned | 2006-09-08T21:14:05Z | |
dc.date.available | 2006-09-08T21:14:05Z | |
dc.date.issued | 1972-12 | en_US |
dc.identifier.citation | Derome, Jacques; Wiin-Nielsen, A.; (1972). "On the maintenance of the axisymmetric part of the flow in the atmosphere." Pure and Applied Geophysics PAGEOPH 95(1): 163-185. <http://hdl.handle.net/2027.42/43251> | en_US |
dc.identifier.issn | 0033-4553 | en_US |
dc.identifier.issn | 1420-9136 | en_US |
dc.identifier.uri | https://hdl.handle.net/2027.42/43251 | |
dc.description.abstract | The maintenance of the axisymmetric component of the flow in the atmosphere is investigated by means of a steady-state, quasi-geostrophic formulation of the meteorological equations. It is shown that the meridional variations in the time-averaged axisymmetric variables can be expressed as the sum of three contributions, one being due to the eddy heat transport, another to the eddy momentum transport, and a third to the convective-radiative equilibrium temperature which enters the problem through the specification of a Newtonian form of diabatic heating. The contributions by the large scale eddies are evaluated through the use of observed values for the eddy heat and momentum transports. | en_US |
dc.format.extent | 1192749 bytes | |
dc.format.extent | 3115 bytes | |
dc.format.mimetype | application/pdf | |
dc.format.mimetype | text/plain | |
dc.language.iso | en_US | |
dc.publisher | Birkhäuser-Verlag; Springer Science+Business Media | en_US |
dc.subject.other | Geosciences | en_US |
dc.subject.other | Geophysics/Geodesy | en_US |
dc.title | On the maintenance of the axisymmetric part of the flow in the atmosphere | en_US |
dc.type | Article | en_US |
dc.subject.hlbsecondlevel | Physics | en_US |
dc.subject.hlbsecondlevel | Atmospheric, Oceanic and Space Sciences | en_US |
dc.subject.hlbtoplevel | Science | en_US |
dc.description.peerreviewed | Peer Reviewed | en_US |
dc.contributor.affiliationum | Department of Meteorology and Oceanography, The University of Michigan, Ann Arbor, Michigan, U.S.A. | en_US |
dc.contributor.affiliationother | Meteorological Service of Canada, Montreal, Quebec, Canada | en_US |
dc.contributor.affiliationumcampus | Ann Arbor | en_US |
dc.description.bitstreamurl | http://deepblue.lib.umich.edu/bitstream/2027.42/43251/1/24_2004_Article_BF00878865.pdf | en_US |
dc.identifier.doi | http://dx.doi.org/10.1007/BF00878865 | en_US |
dc.identifier.source | Pure and Applied Geophysics PAGEOPH | en_US |
dc.owningcollname | Interdisciplinary and Peer-Reviewed |
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