Derivation of Zero-Dimensional from One-Dimensional Climate Models

dc.contributor.author	Nicolis, C.
dc.date	1980
dc.date.accessioned	2017-09-08T13:21:08Z
dc.date.available	2017-09-08T13:21:08Z
dc.identifier.uri	https://orfeo.belnet.be/handle/internal/6234
dc.description	A ‘one-dmensional energy-balance equation involving diffusive energy transport and taking into account the ice-albedo feedback is considered. A systematic elimination of the spatial degrecs of freedom is performed. This gives rise to a zero-dimensional climate model displaying the explicit dependence of planetary albedo on plarietary temperature and on some model parameters. In the general case, the zero-dimensional model involves memory effects as well as two characteristic relaxation rates.
dc.language	eng
dc.title	Derivation of Zero-Dimensional from One-Dimensional Climate Models
dc.type	Article
dc.subject.frascati	Physical sciences
dc.audience	Scientific
dc.source.title	Geophysical & Astrophysical Fluid Dynamics
dc.source.volume	15
dc.source.issue	1
dc.source.page	91-103
Orfeo.peerreviewed	Yes
dc.identifier.doi	10.1080/03091928008241172
dc.identifier.scopus	2-s2.0-77955135155