The Plymouth Student Scientist
Document Type
Project Article
Abstract
Historical temperature and salinity data from the Irminger basin were analysed to determine if Labrador Sea Water forms in the Irminger Basin and if deep convection in the region is dependent on the North Atlantic Oscillation. This was undertaken by analysing the Surface Mixed Layer depth during the Boreal winter (December-March) and comparing it to the North Atlantic Oscillation Index. We find there is evidence of LSW formation in the region and there is a weak to moderate correlation with the North Atlantic Oscillation Index.
Publication Date
2009-12-01
Publication Title
The Plymouth Student Scientist
Volume
2
Issue
2
First Page
199
Last Page
217
ISSN
1754-2383
Deposit Date
May 2019
Embargo Period
2024-07-03
URI
http://hdl.handle.net/10026.1/13878
Creative Commons License
This work is licensed under a Creative Commons Attribution 4.0 International License.
Recommended Citation
Garner, Philip
(2009)
"Labrador Sea Water formation in the Irminger Basin and its dependence on the North Atlantic Oscillation,"
The Plymouth Student Scientist: Vol. 2:
Iss.
2, Article 14.
Available at:
https://pearl.plymouth.ac.uk/tpss/vol2/iss2/14
