We show how the prototypical models governing the unforced components of the variability can be deduced from a more general three-variable model involving an additional variable that is a measure of the underside, near-ice edge ocean temperature, and how this three-variable model can itself plausibly exhibit long term oscillations of about 100 000 years even though the time constants involved are only of the order of 10 000 years.-from Authors
Long period free oscillations in a three-component climate model / Saltzman, B.; Sutera, Alfonso; Hansen, A. R.. - STAMPA. - (1984), pp. 289-298.
Long period free oscillations in a three-component climate model.
SUTERA, Alfonso;
1984
Abstract
We show how the prototypical models governing the unforced components of the variability can be deduced from a more general three-variable model involving an additional variable that is a measure of the underside, near-ice edge ocean temperature, and how this three-variable model can itself plausibly exhibit long term oscillations of about 100 000 years even though the time constants involved are only of the order of 10 000 years.-from AuthorsFile allegati a questo prodotto
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