PA3204 Early Holocene Laurentide Ice Sheet deglaciation causes cooling in the high-latitude Southern Hemisphere through oceanic teleconnection (doi 10.1029/2009PA001854)

Gespeichert in:

Autor*in:	Renssen, H [verfasserIn] Goosse, H Crosta, X Roche, D M

Format:	Artikel

Erschienen:	2010

Übergeordnetes Werk:	Enthalten in: Paleoceanography - Washington, DC : Union, 1986, 25(2010), 3
Übergeordnetes Werk:	volume:25 ; year:2010 ; number:3

Katalog-ID:	OLC1852563680

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