Correction to “Forcing of tropical Atlantic sea surface temperatures during the mid-Pleistocene transition”
Citable URI
https://hdl.handle.net/1912/3438As published
https://doi.org/10.1029/2005PA001134DOI
10.1029/2005PA001134Description
Author Posting. © American Geophysical Union, 2005. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Paleoceanography 20 (2005): PA1019, doi:10.1029/2005PA001134.
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Paleoceanography 20 (2005): PA1019Related items
Showing items related by title, author, creator and subject.
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Forcing of tropical Atlantic sea surface temperatures during the mid-Pleistocene transition
(American Geophysical Union, 2004-12-28)We compare a new mid-Pleistocene sea surface temperature (SST) record from the eastern tropical Atlantic to changes in continental ice volume, orbital insolation, Atlantic deepwater ventilation, and Southern Ocean front ... -
Subsurface heat channel drove sea surface warming in the high-latitude North Atlantic during the Mid-Pleistocene Transition
(American Geophysical Union, 2021-06-01)The Mid-Pleistocene Transition (MPT, 1,200–600 ka) marks the rapid expansion of Northern Hemisphere (NH) continental ice sheets and stronger precession pacing of glacial/interglacial cyclicity. Here, we investigate the ... -
Causes of ice age intensification across the Mid-Pleistocene Transition
(National Academy of Sciences, 2017-11-27)During the Mid-Pleistocene Transition (MPT; 1,200–800 kya), Earth’s orbitally paced ice age cycles intensified, lengthened from ∼40,000 (∼40 ky) to ∼100 ky, and became distinctly asymmetrical. Testing hypotheses that ...
