AMPLITUDE AND PHASE OF GLACIAL CYCLES FROM A CONCEPTUAL MODEL

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dc.contributor.author Parrenin F.
dc.contributor.author Paillard D.
dc.date.accessioned 2021-11-27T03:01:35Z
dc.date.available 2021-11-27T03:01:35Z
dc.date.issued 2003
dc.identifier https://www.elibrary.ru/item.asp?id=14096116
dc.identifier.citation Earth and Planetary Science Letters, 2003, 214, 1-2, 243-250
dc.identifier.issn 0012-821X
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/32524
dc.description.abstract The astronomical theory of climate, in which the orbital variations of the Earth are taken to drive the climate changes, explains many features of the paleoclimatic records. Nevertheless, the precise link between insolation variations and climatic changes during the Quaternary remains mysterious in several aspects. In particular, the largest sea level changes of the past million years occurred when insolation variations were minimal, like during stage 11, and vice versa like during stage 7. Moreover, recent data from terminations II and III show surprising phase lead and lag between insolation and sea level variations. To explain these paradoxical amplitude and phase modulations, we suggest here that deglaciations started when a combination of insolation and ice volume was large enough. To illustrate this new idea, we present a simple conceptual model that simulates the sea level curve of the past million years with very realistic amplitude modulations, and with good phase modulations.
dc.title AMPLITUDE AND PHASE OF GLACIAL CYCLES FROM A CONCEPTUAL MODEL
dc.type Статья


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