Extremal climatic states simulated by a 2-dimensional model Part II: Different climatic scenarios
dc.contributor.author
dc.date.accessioned
2013-04-12T09:51:20Z
dc.date.available
2013-04-12T09:51:20Z
dc.date.issued
2000
dc.identifier.issn
0280-6495
dc.identifier.uri
dc.description.abstract
Different climatic simulations have been obtained by using a 2-Dim horizontal energy balancemodel (EBM), which has been constrained to satisfy several extremal principles on dissipationand convection. Moreover, 2 different versions of the model with fixed and variable cloud-coverhave been used. The assumption of an extremal type of behaviour for the climatic system canacquire additional support depending on the similarities found with measured data for pastconditions as well as with usual projections for possible future scenarios
dc.format.mimetype
application/pdf
dc.language.iso
eng
dc.publisher
International Meteorological Institute in Stockholm
dc.relation.isformatof
Reproducció digital del document publicat a: http://dx.doi.org/10.1034/j.1600-0870.2000.00193.x
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© Tellus Series A-Dynamic Meteorology and Oceanography, 2000, vol. 52, núm. 4, p.440-454
dc.relation.ispartofseries
Articles publicats (D-F)
dc.rights
Attribution-NonCommercial 3.0 Spain
dc.rights.uri
dc.title
Extremal climatic states simulated by a 2-dimensional model Part II: Different climatic scenarios
dc.type
info:eu-repo/semantics/article
dc.rights.accessRights
info:eu-repo/semantics/openAccess
dc.embargo.terms
Cap
dc.type.version
info:eu-repo/semantics/publishedVersion
dc.identifier.doi
dc.identifier.idgrec
007934
dc.identifier.eissn
1600-0870