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Variability and Transport Methodology of the Atlantic Meridional Overturning Circulation at 26°N
The importance of The Atlantic Meridional Overturning Circulation (AMOC) resides in its associated poleward movement of heat (Bryden et …
Neela Morarji
December 2017
University of Southampton, Ocean and Earth Science
PhD theses
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Emerging negative Atlantic Multidecadal Oscillation index in spite of warm subtropics
Sea surface temperatures in the northern North Atlantic have shown a marked decrease over the past several years. The sea surface in …
Eleanor Frajka-Williams
,
Claudie Beaulieu
,
Aurelie D. Duchez
September 2017
Scientific Reports
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Primary production and nitrate budgets in the temperate North Atlantic estimated from ocean gliders
Phytoplankton in the ocean are a key component of the global carbon cycle and the base of most marine food webs. They contribute …
Victoria S. Hemsley
November 2016
University of Southampton, Ocean and Earth Science
PhD theses
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Drivers of exceptionally cold North Atlantic Ocean temperatures and their link to the 2015 European heat wave
The North Atlantic and Europe experienced two extreme climate events in 2015: exceptionally cold ocean surface temperatures and a …
Aurelie D. Duchez
,
Eleanor Frajka-Williams
,
Simon A. Josey
,
D. Gwyn Evans
,
Jeremy P. Grist
,
R. Marsh
,
Gerard D. McCarthy
,
Bablu Sinha
,
David I. Berry
,
Joel J.-M. Hirschi
July 2016
Env. Res. Lett.
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Generation of Internal Waves by Eddies Impinging on the Western Boundary of the North Atlantic
Despite the major role played by mesoscale eddies in redistributing the energy of the large-scale circulation, our understanding of …
Louis Clement
,
Eleanor Frajka-Williams
,
Katy L. Sheen
,
J. Alex Brearley
,
Alberto C. Naveira Garabato
April 2016
J. Phys. Ocean.
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Estimating the Atlantic MOC at 26°N using satellite altimetry and cable measurements
A statistical relationship between satellite sea surface height (SSH) and observed transports at 26°N is used to build a proxy for the AMOC transport since 1992. The method relies on a strong relationship between (1) the interannual variability of spatially-smoothed SSH at the western boundary of the Atlantic and (2) the RAPID 26°N estimate of upper mid-ocean transport (UMO, top ~1100m) across the Atlantic. Explained variance is very high, but the method assumes stationarity in the relationship between SSH and UMO, which would likely be violated on longer timescales associated with e.g., deep watermass change.
Eleanor Frajka-Williams
April 2015
Geophys. Res. Lett.
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Vertical structure of eddies and Rossby waves and their effect on the Atlantic MOC at 26.5°N
The meridional overturning circulation (MOC) at inline image in the Atlantic has a standard deviation of 4.9 Sv and contains large …
Louis Clement
,
Eleanor Frajka-Williams
,
Zoltan B. Szuts
,
Stuart A. Cunningham
September 2014
J. Geophys. Res.
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Eddy impacts on the Florida Current
The Gulf Stream in the Atlantic carries warm water northwards and forms both the return closure of the subtropical gyre as well as the …
Eleanor Frajka-Williams
,
William E. Johns
,
Chris S. Meinen
,
Lisa M. Beal
,
Stuart A. Cunningham
January 2013
Geophys. Res. Lett.
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Physical controls and interannual variability of the Labrador Sea spring phytoplankton bloom in distinct regions
We investigated the variability of the spring phytoplankton bloom in the Labrador Sea, dividing into distinct biogeographical zones, …
Eleanor Frajka-Williams
,
Peter B. Rhines
January 2010
Deep Sea Res. I
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Physical controls and mesoscale variability in the Labrador Sea spring phytoplankton bloom observed by Seaglider
We investigated the 2005 spring phytoplankton bloom in the Labrador Sea using Seaglider, an autonomous underwater vehicle equipped with …
Eleanor Frajka-Williams
,
Peter B. Rhines
,
Charles C. Eriksen
August 2009
Deep Sea Res. I
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