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Sensitivity of Neoproterozoic snowball-Earth inceptions to continental configuration, orbital geomet...

Sensitivity of Neoproterozoic snowball-Earth inceptions to continental configuration, orbital geomet...

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_5458acd922d24be4b8ea3686dfcb6be2

Sensitivity of Neoproterozoic snowball-Earth inceptions to continental configuration, orbital geometry, and volcanism

About this item

Full title

Sensitivity of Neoproterozoic snowball-Earth inceptions to continental configuration, orbital geometry, and volcanism

Publisher

Katlenburg-Lindau: Copernicus GmbH

Journal title

Climate of the past, 2023-11, Vol.19 (11), p.2203-2235

Language

English

Formats

Publication information

Publisher

Katlenburg-Lindau: Copernicus GmbH

More information

Scope and Contents

Contents

The Cryogenian period (720–635 million years ago) in the Neoproterozoic era featured two phases of global or near-global ice cover termed “snowball Earth”. Climate models of all kinds indicate that the inception of these phases must have occurred in the course of a self-amplifying ice–albedo feedback that forced the climate from a partially ice-cov...

Alternative Titles

Full title

Sensitivity of Neoproterozoic snowball-Earth inceptions to continental configuration, orbital geometry, and volcanism

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_doaj_primary_oai_doaj_org_article_5458acd922d24be4b8ea3686dfcb6be2

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_5458acd922d24be4b8ea3686dfcb6be2

Other Identifiers

ISSN

1814-9332,1814-9324

E-ISSN

1814-9332

DOI

10.5194/cp-19-2203-2023

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