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Satellite
Project - UHEAT
Understanding Ocean Heat Content and Its Role in Driving Marine Heatwaves and Ecosystem Responses
Eleanor Frajka-Williams
Estimates of Atlantic meridional heat transport from spatiotemporal fusion of Argo, altimetry and gravimetry data
Understanding how changes in Atlantic meridional heat transport (MHT) and the Earth’s climate relate to one another is crucial to our …
F. M. Calafat
,
P. Vallivattathillam
,
Eleanor Frajka-Williams
March 2025
Ocean Science
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Dissipation of mesoscale eddies at a western boundary via a direct energy cascade
The fate of mesoscale eddy kinetic energy represents a large source of uncertainty in the global ocean energy budget. Satellite …
D. Gwyn Evans
,
Eleanor Frajka-Williams
,
Alberto C. Naveira Garabato
January 2022
Scientific Reports
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A dynamically based method for estimating the Atlantic meridional overturning circulation at 26°N from satellite altimetry
A method for estimating 26°N overturning from time-varying satellite altimetry and time-averaged boundary profiles of dynamic height.
Alejandra Sanchez-Franks
,
Eleanor Frajka-Williams
,
Ben I. Moat
,
David A. Smeed
January 2021
Oc. Sci.
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Breaking of internal waves and turbulent dissipation in an anticyclonic mode water eddy
A 4-month glider mission was analyzed to assess turbulent dissipation in an anticyclonic eddy at the western boundary of the …
Bieito Fernandez-Castro
,
D. Gwyn Evans
,
Eleanor Frajka-Williams
,
Clement Vic
,
Alberto C. Naveira Garabato
July 2020
J. Phys. Ocean.
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Phased response of the subpolar Southern Ocean to changes in circumpolar winds
The response of the subpolar Southern Ocean (sSO) to wind forcing is assessed using satellite radar altimetry. sSO sea level exhibits a …
Alberto C. Naveira Garabato
,
Jack Hooley
,
Tiago S. Dotto
,
Sheldon Bacon
,
M. Tsamados
,
A. Ridout
,
Eleanor Frajka-Williams
,
L. Herraiz-Borreguero
,
Paul R. Holland
,
H. D. B. S. Heorton
,
Mike P. Meredith
May 2019
Geophys. Res. Lett.
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Using GRACE and in situ bottom pressure recorders to evaluate external transports at 26°N
A demonstration of how GRACE-satellite estimates of ocean bottom pressure can be used to stitch together
in situ
bottom pressure records at 26°N, alleviating the need to detrend the observed bottom pressure. However, the method does not allow determination of the trend over the full period; if the GRACE trend over the full period (2004-2016) is applied, then it implies a trend in the compensation transports from 26°N which has the opposite sign as the compensation transport derived from the RAPID 26°N mooring array.
Emma Worthington
,
Eleanor Frajka-Williams
,
G. D. McCarthy
January 2019
J. Geophys. Res.
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Loop Current variability as trigger of coherent Gulf Stream transport anomalies
Joel J.-M. Hirschi
,
Eleanor Frajka-Williams
,
Adam T. Blaker
,
Bablu Sinha
,
P. Hyder
,
Andrew Coward
,
Others
January 2019
J. Phys. Ocean.
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PDF (accepted)
Monthly SSS in the Labrador Sea from SMOS
1 Jan 2019
0 min read
Project
Coherent modulation of the sea-level annual cycle in the United States by Atlantic Rossby waves
Changes in the sea-level annual cycle (SLAC) can have profound impacts on coastal areas, including increased flooding risk and …
Francisco M. Calafat
,
Thomas Wahl
,
Fredrik Lindsten
,
Joanne Williams
,
Eleanor Frajka-Williams
December 2018
Nature Comm.
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