Publications

EPOC: Project News
Second newsletter of the EPOC project.
Wind forcing controls on Antarctic Bottom Water export from the Weddell Sea via bottom boundary layer processes
The Antarctic Bottom Water (AABW) exported from the Weddell Sea has experienced warming and contraction in the past 30 yrs. Superposed …
EPOC: Project News
First newsletter of the EPOC project.
Climate change impacts on ocean circulation relevant to the UK and Ireland
Ocean circulation, including ocean currents and systems of ocean currents, such as ocean gyres and the meridional overturning …
Climate-Relevant Ocean Transport Measurements in the Atlantic and Arctic Oceans
Mixing and transformation in a deep western boundary current: A case study
Water-mass transformation by turbulent mixing is a key part of the deep-ocean overturning, as it drives the upwelling of dense waters …
Pending recovery in the strength of the meridional overturning circulation at 26°N
The strength of the Atlantic meridional overturning circulation (AMOC) at 26∘ N has now been continuously measured by the RAPID array …
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 …
Model derived uncertainties in deep ocean temperature trends between 1990--2010
In recent decades, deep (below 2,000 m) ocean temperature trends have been measured when scientific research vessels repeat the same …
Structure and variability of the Antilles Current at 26.5°N
Rapid mixing and exchange of deep-ocean waters in an abyssal boundary current
The overturning circulation of the global ocean is regulated by deep-ocean mixing, which transforms cold waters sinking at high …
OceanObs19: OceanGliders: a component of the integrated GOOS
The OceanGliders program started in 2016 to support active coordination and enhancement of global glider activity. OceanGliders …
Loop Current variability as trigger of coherent Gulf Stream transport anomalies
Estimating the Freshwater Flux from the Greenland Ice Sheet Workshop Report, American Geophysical Union, 2018
The Atlantic meridional overturning circulation (AMOC) has been observed continuously at 26° N since April 2004. The AMOC and its …
Variability of the Ross Gyre, Southern Ocean: drivers and responses revealed by satellite altimetry
The Ross Gyre is one of the main current systems of the Southern Ocean and conveys heat toward the cold continental shelves of the …
The North Atlantic Ocean is in a state of reduced overturning
The Atlantic Meridional Overturning Circulation (AMOC) is responsible for a variable and climatically important northward transport of …
The Accuracy of Estimates of the Overturning Circulation from Basin Wide Mooring Arrays
Previous modeling and observational studies have established that it is possible to accurately monitor the Atlantic Meridional …
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 …
Major Variations in Sub-Tropical North Atlantic Heat Transport at Short (5 day) Timescales and their Causes
Variability in the North Atlantic ocean heat transport at 26.5°N on short (5 day) timescales is identified and contrasted with …
Compensation between meridional flow components of the Atlantic MOC at 26°N
From ten years of observations of the Atlantic meridional overturning circulation (MOC) at 26° N (2004–2014), we revisit the question …
Measuring the Atlantic meridional overturning circulation at 26°N
Methodology and error analysis for the RAPID 26°N estimates of the AMOC transport.
A new index for the Atlantic meridional overturning circulation
The Atlantic meridional overturning circulation (AMOC) has received considerable attention, motivated by its major role in the global …
Observed decline of the Atlantic meridional overturning circulation 2004 to 2012
The Atlantic meridional overturning circulation (AMOC) has been observed continuously at 26° N since April 2004. The AMOC and its …
Meridional overturning circulation observations in the North Atlantic Ocean
Atlantic MOC slowdown cooled the subtropical ocean
Observations show that the upper 2 km of the subtropical North Atlantic Ocean cooled throughout 2010 and remained cold until at least …
Atmosphere drives observed interannual variability of the Atlantic meridional overturning circulation at 26.5N
The Atlantic meridional overturning circulation (AMOC) has been observed at 26.5°N since 2004. During 2009/2010, there was a transient …
Meridional overturning circulation and heat transport observations in the Atlantic Ocean
Observed Interannual Variability of the Atlantic MOC at 26.5°N
The Atlantic meridional overturning circulation (MOC) plays a critical role in the climate system and is responsible for much of the …
Meridional overturning circulation observations in the subtropical North Atlantic.
Determining Vertical Velocities from Seaglider
Methodology for estimating vertical seawater velocities from standard Seagliders.
Monitoring the Atlantic meridional overturning circulation
The original RAPID methodology, now updated in McCarthy et al. 2015.
Meridional Overturning Circulation Observations in the Subtropical North Atlantic