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Quaternary Climate Change
Top > Geography > Paleontology > Quaternary Studies > Quaternary Climate Change
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University of California Santa Cruz. Research areas include climate variability, warm climate transitions, Milankovitch forcing of early Cenozoic climates.
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Google PR: A central location for paleoclimate data, research, and education.
Details Hits: 1 Votes: 0 Ratings: Reviews: Google PR: Atlantic Monthly article reviews the abrupt (less than a decade transition) climate changes of the past, analyzes the role of the Gulf Stream's thermohaline circulation switching modes of operation, and presents three scenarios for the future, including potential methods for stabilizing the flip-flop tendencies.
Details Hits: 0 Votes: 0 Ratings: Reviews: Google PR: Article about research suggesting that cyclical changes in the location of the Earth's orbit causing differing amounts of extraterrestrial debris to come into the atmosphere, and not the Milankovitch theory, explain cycles of glaciation in the last million years.
Details Hits: 0 Votes: 0 Ratings: Reviews: Google PR: Article about the potential climatic impacts of disruptions in the thermohaline circulation system in the North Atlantic.
Details Hits: 0 Votes: 0 Ratings: Reviews: Google PR: articles from American Geophysical Union publications, primarily for a general audience.
Details Hits: 0 Votes: 0 Ratings: Reviews: Google PR: NOAA Paleoclimatology Program educational material concerning the Milankovitch theory, which explains changes in the seasons as a result of changes in the earth's orbit around the sun.
Details Hits: 0 Votes: 0 Ratings: Reviews: Google PR: Examines the climate variation in the pas, and the link with changes in atmospheric carbon dioxide.
Details Hits: 0 Votes: 0 Ratings: Reviews: Google PR: 100 million years to recent ice age, by Thomas J. Crowley, a marine geologist and climatogist.
Details Hits: 0 Votes: 0 Ratings: Reviews: Google PR: Description, publications, and other scientific contributions from investigations to reconstruct 200 - 2000 years of past climatic and environmental changes in Antarctica, using remote sensing, ice cores, geophysics, and other methods.
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