arc2climate.org

Whole Earth systems and long-term climate evolution

We are a community of scientists and educators interested in what controls long-term climate evolution. For example, why was the Cretaceous and early Paleogene warm and ice-free, and why has the latter half of the Cenozoic been relatively cool and characterized by ice caps covering at least one of the poles? It is generally agreed
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OVERVIEW

The web page arc2climate.org presently has an average traffic classification of zero (the smaller the better). We have downloaded four pages inside the web page arc2climate.org and found zero websites associating themselves with arc2climate.org. There is one contacts and directions for arc2climate.org to help you correspond with them. The web page arc2climate.org has been online for five hundred and ninety-one weeks, one day, three hours, and nine minutes.
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ARC2CLIMATE.ORG HISTORY

The web page arc2climate.org was first filed on January 16, 2013. It is now five hundred and ninety-one weeks, one day, three hours, and nine minutes young.
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January
2013

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11
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CONTACTS

Rice University

Cin-Ty Lee

Dept Earth Science, MS-126

Houston, Texas, 77005

US

1.7133485084
cintylee@gmail.com

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SITE TITLE

Whole Earth systems and long-term climate evolution

DESCRIPTION

We are a community of scientists and educators interested in what controls long-term climate evolution. For example, why was the Cretaceous and early Paleogene warm and ice-free, and why has the latter half of the Cenozoic been relatively cool and characterized by ice caps covering at least one of the poles? It is generally agreed

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The web page states the following, "Whole Earth systems and long-term climate evolution." I saw that the web page also stated " Seminar-Mountains, Climate, Carbon." They also said " Whole Earth systems and long-term climate evolution. Seminar-Mountains, Climate, Carbon. We are a community of scientists and educators interested in what controls long-term climate evolution. For example, why was the Cretaceous and early Paleogene warm and ice-free, and why has the latter half of the Cenozoic been relatively cool and characterized by ice caps covering at least one of the poles? Dasgupta, R."

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