The influence of double-diffusive processes on the melting of ice in the Arctic Ocean: laboratory analogue experiments and their interpretation

This study has been motivated by two oceanographic observations: an increased rate of melting of sea ice in the Arctic Ocean, and the advance of an anomalously warm tongue of Atlantic water across the Arctic below the halocline over the last few decades.

Bibliographic Details
Published in:Journal of Marine Systems
Main Authors: Turner, J, Veronis, G
Format: Article in Journal/Newspaper
Language:unknown
Published: Elsevier
Subjects:
Ice
Online Access:http://hdl.handle.net/1885/85507
https://doi.org/10.1016/j.jmarsys.2003.06.002
Description
Summary:This study has been motivated by two oceanographic observations: an increased rate of melting of sea ice in the Arctic Ocean, and the advance of an anomalously warm tongue of Atlantic water across the Arctic below the halocline over the last few decades.