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The North Atlantic Ocean Is in a State of Reduced Overturning

Geophysical research letters, 2018-02, Vol.45 (3), p.1527-1533

2018

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Observed decline of the Atlantic meridional overturning circulation 2004–2012

Ocean science, 2014-02, Vol.10 (1), p.29-38

2014

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Measurement of wind profiles by motion-stabilised ship-borne Doppler lidar

Atmospheric measurement techniques, 2015-11, Vol.8 (11), p.4993-5007

2015

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Motion-correlated flow distortion and wave-induced biases in air–sea flux measurements from ships

Atmospheric chemistry and physics, 2015-09, Vol.15 (18), p.10619-10629

2015

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Compensation between meridional flow components of the Atlantic MOC at 26° N

Ocean science, 2016-04, Vol.12 (2), p.481-493

2016

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Near-surface measurements of sea spray aerosol production over whitecaps in the open ocean

Ocean science, 2013-02, Vol.9 (1), p.133-145

2013

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Linearity of DMS transfer coefficient with both friction velocity and wind speed in the moderate wind speed range

Geophysical research letters, 2010-01, Vol.37 (1), p.n/a

2010

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Seasonal intensification and trends of rogue wave events on the US western seaboard

Scientific reports, 2019-03, Vol.9 (1), p.4461-4461, Article 4461

2019

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Wind stress measurements from the open ocean corrected for airflow distortion by the ship

Journal of physical oceanography, 1998-07, Vol.28 (7), p.1511-1526

1998

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Insights into Decadal North Atlantic Sea Surface Temperature and Ocean Heat Content Variability from an Eddy-Permitting Coupled Climate Model

Journal of climate, 2019-09, Vol.32 (18), p.6137-6161

2019

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Can Rogue Waves Be Predicted Using Characteristic Wave Parameters?

Journal of geophysical research. Oceans, 2018-08, Vol.123 (8), p.5624-5636

2018

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Uncertainties in wind speed dependent CO2 transfer velocities due to airflow distortion at anemometer sites on ships

Atmospheric chemistry and physics, 2010-06, Vol.10 (11), p.5123-5133

2010

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CFD Model Estimates of the Airflow Distortion over Research Ships and the Impact on Momentum Flux Measurements

Journal of atmospheric and oceanic technology, 2002-10, Vol.19 (10), p.1477-1499

2002

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Full-depth temperature trends in the northeastern Atlantic through the early 21st century

Geophysical research letters, 2014-11, Vol.41 (22), p.7971-7979

2014

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Importance of Boundary Processes for Heat Uptake in the Subpolar North Atlantic

Journal of geophysical research. Oceans, 2020-09, Vol.125 (9), p.n/a

2020

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AutoFlux: an autonomous system for the direct measurement of the air-sea fluxes of CO2, heat and momentum

Journal of operational oceanography, 2009, Vol.2 (1), p.15-23

2009

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Major variations in subtropical North Atlantic heat transport at short (5 day) timescales and their causes

Journal of geophysical research. Oceans, 2016-05, Vol.121 (5), p.3237-3249

2016

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The importance of deep, basinwide measurements in optimized Atlantic Meridional Overturning Circulation observing arrays

Journal of geophysical research. Oceans, 2017-03, Vol.122 (3), p.1808-1826

2017

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Measuring the Atlantic Meridional Overturning Circulation at 26°N

Progress in oceanography, 2015-01, Vol.130, p.91-111

2015

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Uncertainties in wind speed dependent CO 2 transfer velocities due to airflow distortion at anemometer sites on ships

Atmospheric chemistry and physics, 2010-06, Vol.10 (11), p.5123-5133

2010

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A 30-year reconstruction of the Atlantic meridional overturning circulation shows no decline

Ocean science, 2021-02, Vol.17 (1), p.285-299

2021

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Sustainable Observations of the AMOC: Methodology and Technology

Reviews of geophysics (1985), 2020-03, Vol.58 (1), p.n/a

2020

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Pending recovery in the strength of the meridional overturning circulation at 26° N

Ocean science, 2020-07, Vol.16 (4), p.863-874

2020

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Ocean Heat Convergence and North Atlantic Multidecadal Heat Content Variability

Journal of climate, 2024-09, Vol.37 (18), p.4723-4742

2024

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Quantifying the Airflow Distortion over Merchant Ships. Part II: Application of the Model Results

Journal of atmospheric and oceanic technology, 2006-03, Vol.23 (3), p.351-360

2006

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The North Atlantic Ocean Is in a State of Reduced Overturning

Observed decline of the Atlantic meridional overturning circulation 2004–2012

Measurement of wind profiles by motion-stabilised ship-borne Doppler lidar

Motion-correlated flow distortion and wave-induced biases in air–sea flux measurements from ships

Compensation between meridional flow components of the Atlantic MOC at 26° N

Near-surface measurements of sea spray aerosol production over whitecaps in the open ocean

Linearity of DMS transfer coefficient with both friction velocity and wind speed in the moderate wind speed range

Seasonal intensification and trends of rogue wave events on the US western seaboard

Wind stress measurements from the open ocean corrected for airflow distortion by the ship

Insights into Decadal North Atlantic Sea Surface Temperature and Ocean Heat Content Variability from an Eddy-Permitting Coupled Climate Model

Can Rogue Waves Be Predicted Using Characteristic Wave Parameters?

Uncertainties in wind speed dependent CO2 transfer velocities due to airflow distortion at anemometer sites on ships

CFD Model Estimates of the Airflow Distortion over Research Ships and the Impact on Momentum Flux Measurements

Full-depth temperature trends in the northeastern Atlantic through the early 21st century

Importance of Boundary Processes for Heat Uptake in the Subpolar North Atlantic

AutoFlux: an autonomous system for the direct measurement of the air-sea fluxes of CO2, heat and momentum

Major variations in subtropical North Atlantic heat transport at short (5 day) timescales and their causes

The importance of deep, basinwide measurements in optimized Atlantic Meridional Overturning Circulation observing arrays

Measuring the Atlantic Meridional Overturning Circulation at 26°N

Uncertainties in wind speed dependent CO 2 transfer velocities due to airflow distortion at anemometer sites on ships

A 30-year reconstruction of the Atlantic meridional overturning circulation shows no decline

Sustainable Observations of the AMOC: Methodology and Technology

Pending recovery in the strength of the meridional overturning circulation at 26° N

Ocean Heat Convergence and North Atlantic Multidecadal Heat Content Variability

Quantifying the Airflow Distortion over Merchant Ships. Part II: Application of the Model Results

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