Our current understanding of ocean–atmosphere–cryosphere interactions at ice-age terminations relies largely on assessments of the most recent (last) glacial–interglacial transition, Termination I (T-I). But the extent to which T-I is representative of previous terminations remains unclear. Testing the consistency of termination processes requires comparison of time series of critical climate parameters with detailed absolute and relative age control.
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Links:
[1] http://admin.indiaenvironmentportal.org.in/feature-article/bipolar-seesaw-control-last-interglacial-sea-level
[2] http://admin.indiaenvironmentportal.org.in/category/author/g-marino
[3] http://admin.indiaenvironmentportal.org.in/category/author/e-j-rohling
[4] http://admin.indiaenvironmentportal.org.in/category/author/l-rodr%C3%ADguez-sanz-et-al
[5] http://admin.indiaenvironmentportal.org.in/category/journal/nature
[6] http://admin.indiaenvironmentportal.org.in/category/thesaurus/climate-change
[7] http://admin.indiaenvironmentportal.org.in/category/thesaurus/climate-science
[8] http://admin.indiaenvironmentportal.org.in/category/thesaurus/oceans-and-seas
[9] http://admin.indiaenvironmentportal.org.in/category/thesaurus/north-atlantic-ocean
[10] http://admin.indiaenvironmentportal.org.in/category/thesaurus/sea-level-rise
[11] http://admin.indiaenvironmentportal.org.in/category/thesaurus/global-warming
