Thermal Convection and the Origin of Ice Streams


Autoria(s): Hughes, Terence J.
Data(s)

01/01/2009

Resumo

Ice streams are a fact of ice-sheet dynamics, draining up to 90% of the ice. Thermal convection in ice below the density inversion is a speculation. An attempt is made to meld the two in such a way that the speculation becomes an explanation for the fact.

Formato

application/pdf

Identificador

http://digitalcommons.library.umaine.edu/ers_facpub/109

http://digitalcommons.library.umaine.edu/cgi/viewcontent.cgi?article=1108&context=ers_facpub

Publicador

DigitalCommons@UMaine

Fonte

Earth Science Faculty Scholarship

Palavras-Chave #Earth Sciences
Tipo

text