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contributor authorCushman-Roisin, Benoit
date accessioned2017-06-09T14:49:08Z
date available2017-06-09T14:49:08Z
date copyright1989/02/01
date issued1989
identifier issn0022-3670
identifier otherams-27469.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4164477
description abstractIt has been previously noted that, if two warm-core rings were to merge to form a single new eddy, there would be more energy in the final state than in the initial, premerging state, and that therefore, merging is energetically prohibited. However, field and laboratory observations reveal spontaneous merging occurrences and thus challenge this energy argument. The paradox is resolved here by noting that the merging need not be complete; specifically, that the final state in fact consists of a center eddy containing almost all the energy but only a fraction of the mass, surrounded by a pair of thin filaments holding the mass difference, a residual of energy and most of the angular momentum. Existing numerical and experimental results point to the likelihood of such a composite state as the outcome of the merging of two warm-core rings.
publisherAmerican Meteorological Society
titleOn the Role of Filamentation in the Merging of Anticyclonic Lenses
typeJournal Paper
journal volume19
journal issue2
journal titleJournal of Physical Oceanography
identifier doi10.1175/1520-0485(1989)019<0253:OTROFI>2.0.CO;2
journal fristpage253
journal lastpage258
treeJournal of Physical Oceanography:;1989:;Volume( 019 ):;issue: 002
contenttypeFulltext


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