A plausible model for the synchroneity or the phase shift between climatic transitions

dc.contributor.author	Nicolis, C.
dc.date	1984
dc.date.accessioned	2017-06-28T09:19:13Z
dc.date.available	2017-06-28T09:19:13Z
dc.identifier.uri	https://orfeo.belnet.be/handle/internal/5882
dc.description	A class of climate models describing the dynamics of the sea ice‐ocean surface temperature interactions is considered. The coupling mechanism between different spatial regions is analyzed, and the possibility of inhomogeneous phase shifted states is established. It is concluded that many major climatic transitions should occur in an asynchronous fashion. A new examination of the climatic record seems therefore to be necessary, in the light of this possibility.
dc.language	eng
dc.title	A plausible model for the synchroneity or the phase shift between climatic transitions
dc.type	Article
dc.subject.frascati	Earth and related Environmental sciences
dc.audience	Scientific
dc.source.title	Geophysical Research Letters
dc.source.volume	11
dc.source.issue	6
dc.source.page	587-590
Orfeo.peerreviewed	Yes
dc.identifier.doi	10.1029/GL011i006p00587
dc.identifier.scopus	2-s2.0-0021443568