By reinterpreting the 'sea-ice extent' discussed in a recently proposed model of auto-oscillatory climatic change to represent high-inertia grounded and shelf sea ice forms, instead of thinner marine ice forms, it is possible for the model to yield a much longer period of auto-oscillation, perhaps as much as 100 000yr (the dominant period of ice volume variations revealed by deep-sea ocean cores).
A possible marine mechanism for internally generated long-period climate cycles / Saltzman, B.; Sutera, Alfonso; Hansen, A. R.. - In: JOURNAL OF THE ATMOSPHERIC SCIENCES. - ISSN 0022-4928. - STAMPA. - 39:11(1982), pp. 2634-2637. [10.1175/1520-0469(1982)039<2634:APMMFI>2.0.CO;2]
A possible marine mechanism for internally generated long-period climate cycles.
SUTERA, Alfonso;
1982
Abstract
By reinterpreting the 'sea-ice extent' discussed in a recently proposed model of auto-oscillatory climatic change to represent high-inertia grounded and shelf sea ice forms, instead of thinner marine ice forms, it is possible for the model to yield a much longer period of auto-oscillation, perhaps as much as 100 000yr (the dominant period of ice volume variations revealed by deep-sea ocean cores).I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
