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John Imbrie

Researcher at Brown University

Publications -  50
Citations -  15243

John Imbrie is an academic researcher from Brown University. The author has contributed to research in topics: Milankovitch cycles & Ice age. The author has an hindex of 29, co-authored 50 publications receiving 14815 citations. Previous affiliations of John Imbrie include Columbia University.

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Variations in the Earth's Orbit: Pacemaker of the Ice Ages

TL;DR: It is concluded that changes in the earth's orbital geometry are the fundamental cause of the succession of Quaternary ice ages and a model of future climate based on the observed orbital-climate relationships, but ignoring anthropogenic effects, predicts that the long-term trend over the next sevem thousand years is toward extensive Northern Hemisphere glaciation.
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Age dating and the orbital theory of the ice ages: Development of a high-resolution 0 to 300,000-year chronostratigraphy

TL;DR: Using the concept of "orbital tuning", a continuous, high-resolution deep-sea chronostratigraphy has been developed spanning the last 300,000 yr as mentioned in this paper.
BookDOI

Milankovitch and Climate

TL;DR: Adem et al. as discussed by the authors simulate the equilibrium climate at five different stages of the last deglaciation, in order to assess the respective role of different forcings: insolation, ice boundaries and sea surface temperature.
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On the Structure and Origin of Major Glaciation Cycles 1. Linear Responses to Milankovitch Forcing

TL;DR: Starr et al. as mentioned in this paper showed that the 23,000 and 41,000-year cycles of glaciation are continuous, linear responses to orbitally driven changes in the Arctic radiation budget, and used the phase progression in each climatic cycle to identify the main pathways along which the initial, local responses to radiation are propagated by the atmosphere and ocean.
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Modeling the Climatic Response to Orbital Variations

TL;DR: This article summarizes how the theory has evolved since the pioneer studies of James Croll and Milutin Milankovitch, reviews recent evidence that supports the theory, and argues that a major opportunity is at hand to investigate the physical mechanisms by which the climate system responds to orbital forcing.