Ocean Circulation under Globally Glaciated Snowball Earth Conditions: Steady-State Solutions
Ocean Circulation under Globally Glaciated Snowball Earth Conditions: Steady-State Solutions
About this item
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Author / Creator
Publisher
Boston, MA: American Meteorological Society
Journal title
Language
English
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Publication information
Publisher
Boston, MA: American Meteorological Society
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Scope and Contents
Contents
Between ~750 and 635 million years ago, during the Neoproterozoic era, the earth experienced at least two significant, possibly global, glaciations, termed “Snowball Earth.” While many studies have focused on the dynamics and the role of the atmosphere and ice flow over the ocean in these events, only a few have investigated the related associated...
Alternative Titles
Full title
Ocean Circulation under Globally Glaciated Snowball Earth Conditions: Steady-State Solutions
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Record Identifier
TN_cdi_proquest_miscellaneous_1496898678
Permalink
https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_1496898678
Other Identifiers
ISSN
0022-3670
E-ISSN
1520-0485
DOI
10.1175/JPO-D-13-086.1
