Arc-continent collisions in the tropics set Earth’s climate state-Reference-Cited by-同舟云学术

Arc-continent collisions in the tropics set Earth’s climate state

Published:2019-04-12 Issue:6436 Volume:364 Page:181-184
ISSN:0036-8075
Container-title:Science
language:en
Short-container-title:Science

Author:

Macdonald Francis A.¹^ORCID,Swanson-Hysell Nicholas L.²^ORCID,Park Yuem²^ORCID,Lisiecki Lorraine¹^ORCID,Jagoutz Oliver³^ORCID

Affiliation:

1. Department of Earth Science, University of California, Santa Barbara, CA 93106, USA.

2. Department of Earth and Planetary Science, University of California, Berkeley, CA 94720, USA.

3. Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139, USA.

Abstract

Controlling cooling On million-year time scales, Earth's climate state is determined by sources and sinks of carbon to the ocean-atmosphere system. But which specific mechanisms are important in controlling the timing of glacial intervals? Macdonald et al. identify arc-continent collisions in the tropics as a primary control (see the Perspective by Hartmann). They compiled a database of Phanerozoic arc-continent collisions and the latitudinal distribution of ice sheets, showing that ice coverage was greatest when those collisions were most widespread, maximizing global weatherability. Science , this issue p. 181 ; see also p. 126

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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