Heat loss from the Atlantic water layer in the northern Kara Sea: causes and consequences

A distinct, subsurface density front along the eastern St. Anna Trough in the northern Kara Sea is inferred from hydrographic observations in 1996 and 2008–2010. Direct velocity measurements show a persistent northward subsurface current (~ 20 cm s -1 ) along the St. Anna Trough eastern flank. This...

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Bibliographic Details
Published in:Ocean Science
Main Authors: Dmitrenko, I.A., Kirillov, S.A., Serra, N., Koldunov, N.V., Ivanov, V.V., Schauer, U., Polyakov, I.V., Barber, D., Janout, M., Lien, V.S., Makhotin, M., Aksenov, Y.
Format: Article in Journal/Newspaper
Language:English
Published: 2014
Subjects:
Online Access:https://eprints.soton.ac.uk/363059/
https://eprints.soton.ac.uk/363059/1/os-10-719-2014.pdf