Relevant bibliographies by topics / Meridional overturning

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Meridional overturning'

Author: Grafiati
Published: 2 June 2025
Last updated: 31 July 2025

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Journal articles on the topic "Meridional overturning"

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Lumpkin, Rick, and Kevin Speer. "Global Ocean Meridional Overturning." Journal of Physical Oceanography 37, no. 10 (2007): 2550–62. http://dx.doi.org/10.1175/jpo3130.1.

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Abstract A decade-mean global ocean circulation is estimated using inverse techniques, incorporating air–sea fluxes of heat and freshwater, recent hydrographic sections, and direct current measurements. This information is used to determine mass, heat, freshwater, and other chemical transports, and to constrain boundary currents and dense overflows. The 18 boxes defined by these sections are divided into 45 isopycnal (neutral density) layers. Diapycnal transfers within the boxes are allowed, representing advective fluxes and mixing processes. Air–sea fluxes at the surface produce transfers bet
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Back, Amanda, and Joseph A. Biello. "Effect of Overturning Circulation on Long Equatorial Waves: A Low-Frequency Cutoff." Journal of the Atmospheric Sciences 75, no. 5 (2018): 1721–39. http://dx.doi.org/10.1175/jas-d-17-0173.1.

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Zonally long tropical waves in the presence of a large-scale meridional and vertical overturning circulation are studied in an idealized model based on the intraseasonal multiscale moist dynamics (IMMD) theory. The model consists of a system of shallow-water equations describing barotropic and first baroclinic vertical modes coupled to one another by the zonally symmetric, time-independent background circulation. To isolate the effects of the meridional circulation alone, an idealized background flow is chosen to mimic the meridional and vertical components of the flow of the Hadley cell; the
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Bingham, Rory J., Chris W. Hughes, Vassil Roussenov, and Richard G. Williams. "Meridional coherence of the North Atlantic meridional overturning circulation." Geophysical Research Letters 34, no. 23 (2007): n/a. http://dx.doi.org/10.1029/2007gl031731.

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Pinardi, Nadia, Paola Cessi, Federica Borile, and Christopher L. P. Wolfe. "The Mediterranean Sea Overturning Circulation." Journal of Physical Oceanography 49, no. 7 (2019): 1699–721. http://dx.doi.org/10.1175/jpo-d-18-0254.1.

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AbstractThe time-mean zonal and meridional overturning circulations of the entire Mediterranean Sea are studied in both the Eulerian and residual frameworks. The overturning is characterized by cells in the vertical and either zonal or meridional planes with clockwise circulations in the upper water column and counterclockwise circulations in the deep and abyssal regions. The zonal overturning is composed of an upper clockwise cell in the top 600 m of the water column related to the classical Wüst cell and two additional deep clockwise cells, one corresponding to the outflow of the dense Aegea
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Perez, Renellys C., Molly O. Baringer, Shenfu Dong, et al. "Measuring the Atlantic Meridional Overturning Circulation." Marine Technology Society Journal 49, no. 2 (2015): 167–77. http://dx.doi.org/10.4031/mtsj.49.2.14.

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AbstractThe Atlantic meridional overturning circulation (AMOC) plays a crucial role in redistributing heat and salt throughout the global oceans. Achieving a more complete understanding of the behavior of the AMOC system requires a comprehensive observational network that spans the entire Atlantic basin. This article describes several different types of observational systems that are used by scientists of the National Oceanographic and Atmospheric Administration and their partners at other national and international institutions to study the complex nature of the AMOC. The article also highlig
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Rayner, Darren, Joël J. M. Hirschi, Torsten Kanzow, et al. "Monitoring the Atlantic meridional overturning circulation." Deep Sea Research Part II: Topical Studies in Oceanography 58, no. 17-18 (2011): 1744–53. http://dx.doi.org/10.1016/j.dsr2.2010.10.056.

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Samelson, R. M. "A Simple Dynamical Model of the Warm-Water Branch of the Middepth Meridional Overturning Cell." Journal of Physical Oceanography 39, no. 5 (2009): 1216–30. http://dx.doi.org/10.1175/2008jpo4081.1.

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Abstract A reduced-gravity model is presented of the warm-water branch of the middepth meridional overturning circulation in a rectangular basin with a circumpolar connection. The model describes the balance between production of warm water by Ekman advection across the circumpolar current, dissipation of warm water by eddy fluxes southward across the current, and the net production or dissipation of warm water by diabatic processes north of the current. The results emphasize the role of the eastern boundary condition in setting the thermocline structure north of the current and the nonlinear
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Cessi, Paola. "The Global Overturning Circulation." Annual Review of Marine Science 11, no. 1 (2019): 249–70. http://dx.doi.org/10.1146/annurev-marine-010318-095241.

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In this article, I use the Estimating the Circulation and Climate of the Ocean version 4 (ECCO4) reanalysis to estimate the residual meridional overturning circulation, zonally averaged, over the separate Atlantic and Indo-Pacific sectors. The abyssal component of this estimate differs quantitatively from previously published estimates that use comparable observations, indicating that this component is still undersampled. I also review recent conceptual models of the oceanic meridional overturning circulation and of the mid-depth and abyssal stratification. These theories show that dynamics in
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de Boer, A. M., J. R. Toggweiler, and D. M. Sigman. "Atlantic Dominance of the Meridional Overturning Circulation." Journal of Physical Oceanography 38, no. 2 (2008): 435–50. http://dx.doi.org/10.1175/2007jpo3731.1.

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Abstract North Atlantic (NA) deep-water formation and the resulting Atlantic meridional overturning cell is generally regarded as the primary feature of the global overturning circulation and is believed to be a result of the geometry of the continents. Here, instead, the overturning is viewed as a global energy–driven system and the robustness of NA dominance is investigated within this framework. Using an idealized geometry ocean general circulation model coupled to an energy moisture balance model, various climatic forcings are tested for their effect on the strength and structure of the ov
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Bire, Suyash, and Christopher L. P. Wolfe. "The Role of Eddies in the Zonal and Meridional Overturning Circulations of Buoyancy-Forced Basins." Journal of Physical Oceanography 51, no. 2 (2021): 575–90. http://dx.doi.org/10.1175/jpo-d-20-0025.1.

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AbstractThe zonal and meridional overturning circulations of buoyancy-forced basins are studied in an eddy-resolving model. The zonal overturning circulation (ZOC) is driven by the meridional gradient of buoyancy at the surface and stratification at the southern boundary. The ZOC, in turn, produces zonal buoyancy gradients through upwelling and downwelling at the western and eastern boundaries, respectively. The meridional overturning circulation (MOC) is driven by these zonal gradients rather than being directly driven by meridional gradients. Eddies lead to a broadening of the upwelling and
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Dissertations / Theses on the topic "Meridional overturning"

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Boos, William R. (William Ronald) 1975. "Diapycnal mixing transience and the meridional overturning circulation." Thesis, Massachusetts Institute of Technology, 2002. http://hdl.handle.net/1721.1/53161.

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Thesis (S.M.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 2002.<br>Includes bibliographical references (leaves 27-28).<br>Diapycnal mixing of ocean waters is crucial to the dynamics and associated heat transport of the meridional overturning circulation, yet uncertainty exists regarding the distribution and physical mechanisms of this mixing. This study uses a highly-idealized, single-hemisphere model of buoyancy-forced flow to examine the examine the effects of the transience of diapycnal mixing on the MOC. The strength of the MOC was found to
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Buckley, Martha Weaver. "Decadal variability of the Atlantic Meridional Overturning Circulation." Thesis, Massachusetts Institute of Technology, 2011. http://hdl.handle.net/1721.1/68891.

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Thesis (Sc. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 2011.<br>Cataloged from PDF version of thesis.<br>Includes bibliographical references (p. 141-149).<br>In the mean, the Atlantic Ocean transports 1 to 1.5 PW of heat northward, and estimates suggest that 60% of this heat transport is associated with a circulation that reaches the cold waters of the abyss. Due to the role of the Atlantic Meridional Overturning Circulation (AMOC) in ocean heat transport, numerous studies have suggested that AMOC variability plays a role in climate variabi
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Edwards, Erick Lee. "The pattern and dynamics of the meridional overturning Circulation in the upper ocean." Thesis, Monterey, Calif. : Naval Postgraduate School, 2008. http://edocs.nps.edu/npspubs/scholarly/theses/2008/Sept/08Sep%5FEdwards.pdf.

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Thesis (M.S. in Meteorology and Physical Oceanography)--Naval Postgraduate School, September 2008.<br>Thesis Advisor(s): Radko, Timour. "September 2008." Description based on title screen as viewed on November 4, 2008. Includes bibliographical references (p. 99-101). Also available in print.
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Widener, David J. "Influence of the Antarctic Circumpolar Current on the Atlantic meridional circulation." Thesis, Monterey, Calif. : Naval Postgraduate School, 2009. http://edocs.nps.edu/npspubs/scholarly/theses/2009/March/09Mar%5FWidener.pdf.

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Thesis (M.S. in Physical Oceanography)--Naval Postgraduate School, March 2009.<br>Thesis Advisor(s): Radko, Timour. "March 2009." Description based on title screen as viewed on April 23, 2009. Author(s) subject terms: Meridional overturning circulation, MOC, Antarctic Circumpolar Current, ACC, thermohaline circulation. Includes bibliographical references (p. 47-48). Also available in print.
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Galeotti, Chiara. "Multi-annual predictability of the Atlantic Meridional Overturning Circulation." Master's thesis, Alma Mater Studiorum - Università di Bologna, 2021. http://amslaurea.unibo.it/23508/.

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Decadal climate predictions have the main feature of being initialized, hence lying midway between initialized seasonal forecasts and forced multi-decadal projections. The North Atlantic is among the few places where decadal variations are considered potentially predictable with an added value of the initialization due to the Atlantic Meridional Overturning Circulation (AMOC), which exhibits slow multi-annual fluctuations. A correct representation of this process is fundamental to skillfully predict climate variability in the Northern Hemisphere at these timescales. In this thesis, AMOC pred
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Pillar, Helen. "Sensitivity of the Atlantic meridional overturning circulation to surface forcing." Thesis, University of Oxford, 2013. http://ora.ox.ac.uk/objects/uuid:42366dc7-e699-4349-95d2-89a97033d957.

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The determination of the mechanisms setting the strength and structure of the large scale circulation is a fundamental and long-standing problem in physical oceanography. In this thesis, we seek to explore the mechanisms contributing to the steady state and variability of the large scale flow, with a focus on better understanding the dynamics of the Atlantic meridional overturning circulation (AMOC). In the first part of this thesis, we explore the linear sensitivity of the monthly mean subtropical AMOC to surface fluxes of buoyancy and momentum. Our approach is to use a numerical adjoint. Key
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Atkinson, Christopher Paul. "Variability of the Atlantic Meridional Overturning Circulation at 26°N." Thesis, University of Southampton, 2011. https://eprints.soton.ac.uk/338869/.

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The Atlantic Meridional Overturning Circulation (AMOC) and its variability has received considerable attention, motivated by its major role in the global climate system. Observations of AMOC strength at 26�N made by Rapid-WATCH (Rapid climate change - Will the Atlantic Thermohaline Circulation Halt) provide our best current estimate of the state of the AMOC. This study aims to improve understanding of ongoing measurements of AMOC variability made by Rapid-WATCH, and provide context for the 5-year timeseries presently available. The Rapid-WATCH system combines Gulf Stream transport, zonally int
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Butler, Edward D. "The global Meridional Overturning Circulation's response to variable buoyancy forcing." Thesis, University of Southampton, 2015. https://eprints.soton.ac.uk/378965/.

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The meridional overturning circulation (MOC) is a large-scale circulation throughout the global ocean and plays a significant role in the complex global climate system. However, our traditional understanding of the processes driving the MOC has been questioned in recent years. In particular, it has been suggested that surface buoyancy forcing plays little energetic role in driving the MOC. Furthermore, doubt has also been cast over the relationship between meridional overturning and meridional density gradients. In this thesis, we revisit these two ideas using a series of equilibrium and trans
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Goodman, Paul Joseph. "The role of North Atlantic Deep Water formation in the thermohaline circulation /." Thesis, Connect to this title online; UW restricted, 2000. http://hdl.handle.net/1773/10025.

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Howe, Jacob Nathan William. "Investigating Atlantic meridional overturning circulation in the Quarternary using neodymium isotopes." Thesis, University of Cambridge, 2015. https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.709394.

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Books on the topic "Meridional overturning"

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Ivanova, E. V. Globalʹnai︠a︡ termokhalinnai︠a︡ paleot︠s︡irkuli︠a︡t︠s︡ii︠a︡. Nauchnyĭ mir, 2006.

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Mamaev, O. I. Termokhalinnyĭ analiz vod Mirovogo okeana. Gidrometeoizdat, 1987.

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Urakawa, L. Shogo. Energy budget analysis on the role of the Southern Ocean in driving the global thermohaline circulation. Division of Climate System Research, Atmosphere and Ocean Research Institute, University of Tokyo, 2011.

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Schmittner, Andreas, John C. H. Chiang, and Sidney R. Hemming, eds. Ocean Circulation: Mechanisms and Impacts—Past and Future Changes of Meridional Overturning. American Geophysical Union, 2007. http://dx.doi.org/10.1029/gm173.

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Andreas, Schmittner, Chiang John C. H, and Hemming Sidney R, eds. Ocean circulation: Mechanisms and impacts : past and future changes of meridional overturning. American Geophysical Union, 2007.

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Hellmer, Hartmut H. Ein zweidimensionales Modell zur thermohalinen Zirkulation unter dem Schelfeis =: A two-dimensional model for the thermohaline circulation under an ice shelf. Alfred-Wegener-Institut für Polar- und Meeresforschung, 1989.

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Hellmer, Hartmut H. Ein zweidimensionales Modell zur thermohalinen Zirkulation unter dem Schelfeis =: A two-dimensional model for the thermohaline circulation under an ice shelf. Alfred-Wegener-Institut für Polar- und Meeresforschung, 1989.

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Komuro, Yoshiki. Role of the arctic freshwater pathways in controlling the Atlantic meridional overturning circulation. Center for Climate Systems Research, University of Tokyo, 2004.

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Shcherbakov, A. V. Chislennoe modelirovanie globalʹnogo klimata okeana. In-t vychislitelʹnoĭ matematiki i matematicheskoĭ geofiziki SO RAN, 2008.

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Shcherbakov, A. V. Chislennoe modelirovanie globalʹnogo klimata okeana. In-t vychislitelʹnoĭ matematiki i matematicheskoĭ geofiziki SO RAN, 2008.

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Book chapters on the topic "Meridional overturning"

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Olbers, Dirk, Jürgen Willebrand, and Carsten Eden. "The Meridional Overturning of the Oceans." In Ocean Dynamics. Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-23450-7_15.

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Schmittner, Andreas, John C. H. Chiang, and Sidney R. Hemming. "Introduction: The ocean's meridional overturning circulation." In Ocean Circulation: Mechanisms and Impacts—Past and Future Changes of Meridional Overturning. American Geophysical Union, 2007. http://dx.doi.org/10.1029/173gm02.

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Rintoul, Stephen R. "Large-Scale Ocean ocean/oceanic Circulation: Deep Circulation ocean/oceanic deep circulation and Meridional Overturning ocean/oceanic meridional overturning." In Encyclopedia of Sustainability Science and Technology. Springer New York, 2012. http://dx.doi.org/10.1007/978-1-4419-0851-3_721.

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Paparella, Francesco. "Turbulence, Horizontal Convection, and the Ocean’s Meridional Overturning Circulation." In Mathematical Paradigms of Climate Science. Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-39092-5_2.

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Rintoul, Stephen R. "Large-Scale Ocean Circulation: Deep Circulation and Meridional Overturning." In Earth System Monitoring. Springer New York, 2012. http://dx.doi.org/10.1007/978-1-4614-5684-1_10.

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Gnanadesikan, Anand, Agatha M. de Boer, and Bryan K. Mignone. "A simple theory of the pycnocline and overturning revisited." In Ocean Circulation: Mechanisms and Impacts—Past and Future Changes of Meridional Overturning. American Geophysical Union, 2007. http://dx.doi.org/10.1029/173gm04.

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Schmittner, Andreas, Edward J. Brook, and Jinho Ahn. "Impact of the ocean's Overturning circulation on atmospheric CO2." In Ocean Circulation: Mechanisms and Impacts—Past and Future Changes of Meridional Overturning. American Geophysical Union, 2007. http://dx.doi.org/10.1029/173gm20.

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Vellinga, Michael, Bob Dickson, and Ruth Curry. "The Changing View on How Freshwater Impacts the Atlantic Meridional Overturning Circulation." In Arctic–Subarctic Ocean Fluxes. Springer Netherlands, 2008. http://dx.doi.org/10.1007/978-1-4020-6774-7_13.

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Cheng, Jun, Zhengyu Liu, Feng He, Bette L. Otto-Bliesner, Esther C. Brady, and Mark Wehrenberg. "Simulated Two-Stage Recovery of Atlantic Meridional Overturning Circulation During the Last Deglaciation." In Abrupt Climate Change: Mechanisms, Patterns, and Impacts. American Geophysical Union, 2011. http://dx.doi.org/10.1029/2010gm001014.

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Bryan, F. O., N. Nakashiki, Y. Yoshida, and K. Maruyama. "Response of the meridional overturning circulation during differing pathways toward greenhouse gas stabilization." In Ocean Circulation: Mechanisms and Impacts—Past and Future Changes of Meridional Overturning. American Geophysical Union, 2007. http://dx.doi.org/10.1029/173gm22.

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Conference papers on the topic "Meridional overturning"

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Jiang, Owen, David Nizovsky, Tingying Helen Zeng, and Mikhail Y. Shalaginov. "Modeling of the North Atlantic Gyre's Meridional Overturning Circulation with Neural Nets." In 2024 IEEE International Workshop on Metrology for the Sea; Learning to Measure Sea Health Parameters (MetroSea). IEEE, 2024. https://doi.org/10.1109/metrosea62823.2024.10765669.

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Rintoul, Steve R., M. Balmesada, S. Cunningham, et al. "Deep Circulation and Meridional Overturning: Recent Progress and a Strategy for Sustained Observations." In OceanObs'09: Sustained Ocean Observations and Information for Society. European Space Agency, 2010. http://dx.doi.org/10.5270/oceanobs09.pp.32.

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Kim, Joohee, Cecilia Bowe, Leopoldo Pena, et al. "The Atlantic Meridional Overturning Circulation and erosional events across the Mid-Pleistocene Transition." In Goldschmidt2023. European Association of Geochemistry, 2023. http://dx.doi.org/10.7185/gold2023.20494.

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Petridi, Nikoleta, Iliana Polychroni, and Maria Hatzaki. "The Impact of the Atlantic Meridional Overturning Circulation (AMOC) Variability on the Mediterranean Climate." In International Conference on Meteorology, Climatology and Atmospheric Physics. MDPI, 2023. http://dx.doi.org/10.3390/environsciproc2023026160.

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Chu, Peter C., Charles Sun, and Oleg V. Melnichenko. "Variability in the Atlantic Meridional Overturning Circulation and Heat Transport Detected Remotely from Argo Floats." In 2008 IEEE International Geoscience and Remote Sensing Symposium, IGARSS 2008. IEEE, 2008. http://dx.doi.org/10.1109/igarss.2008.4779493.

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Cunningham, Stuart, Stuart Cunningham, Stuart Cunningham, et al. "The Present and Future System for Measuring the Atlantic Meridional Overturning Circulation and Heat Transport." In OceanObs'09: Sustained Ocean Observations and Information for Society. European Space Agency, 2010. http://dx.doi.org/10.5270/oceanobs09.cwp.21.

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Remirez, Mariano, Natalie J. Burls, Geoffrey J. Gilleaudeau, et al. "WELL-OXYGENATED CONDITIONS IN THE NORTH PACIFIC SUPPORT PACIFIC MERIDIONAL OVERTURNING CIRCULATION (PMOC) DURING THE PLIOCENE." In GSA Connects 2023 Meeting in Pittsburgh, Pennsylvania. Geological Society of America, 2023. http://dx.doi.org/10.1130/abs/2023am-395848.

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Liu, Xiaoqing, Matthew Huber, and Nicholas Herold. "Atlantic Meridional Overturning Circulation Influence on the Annual Mean Intertropical Convergence Zone Location in the Miocene." In Goldschmidt 2024. Geochemical Society, 2024. https://doi.org/10.46427/gold2024.22180.

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Kim, Joohee, Steven L. Goldstein, Leopoldo D. Pena, Maria Jaume-Seguí, and Maayan Yehudai. "Reconstruction of the North Atlantic End-Member of the Atlantic Meridional Overturning Circulation over the Last 2 Myr." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.1306.

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Porinchu, David, Glen M. MacDonald, Nicolas Rolland, et al. "EVIDENCE OF ABRUPT CLIMATE CHANGE AT 9.3 KA AND 8.2 KA IN THE CENTRAL CANADIAN ARCTIC: CONNECTION TO THE NORTH ATLANTIC AND ATLANTIC MERIDIONAL OVERTURNING CIRCULATION." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-297240.

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Reports on the topic "Meridional overturning"

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Rene, Schubert. Computing the Meridional Overturning Circulation from NEMO Output. GEOMAR, 2021. http://dx.doi.org/10.3289/sw_3_2021.

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With this script, the Meridional Overturning Circulation (MOC) can be computed from NEMO ocean-model output for the whole globe or the Atlantic (AMOC), Indic (IMOC) and Pacific (PMOC) subbasins. The MOC is computable in z- and sigma coordinates. Moreover, for nested configurations, it is possible to combine data from both host and nest grids. Finally, it is possible to take into account of that the ORCA model grid is curvilinear north of 20°N: it is possible to compute the northward velocity component from the velocity field in x- and y- directions and to sum up the meridional flux over latitu
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Cessi, Paola, and Christopher L. Wolfe. Pulling the Meridional Overturning Circulation From the South DESC0005100. Office of Scientific and Technical Information (OSTI), 2015. http://dx.doi.org/10.2172/1227203.

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Honchar, Amy. Support of Publication Costs, Atlantic Meridional Overturning Circulation Special Issue of Deep Sea Research II Journal. Office of Scientific and Technical Information (OSTI), 2012. http://dx.doi.org/10.2172/1054606.

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Fedorov, Alexey. "What Controls the Structure and Stability of the Ocean Meridional Overturning Circulation: Implications for Abrupt Climate Change?". Office of Scientific and Technical Information (OSTI), 2013. http://dx.doi.org/10.2172/1107722.

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Ramsey, Andree L., Heather H. Furey, and Amy S. Bower. Overturning of the Subpolar North Atlantic Program (OSNAP): RAFOS Float Data Report June 2014 - January 2019. Woods Hole Oceanographic Institution, 2022. http://dx.doi.org/10.1575/1912/29540.

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The Overturning in the Subpolar North Atlantic Program (OSNAP) is an international effort started in 2014 dedicated to achieving a better understanding of the link between dense-water formation and the meridional overturning circulation in the high-latitude North Atlantic. Moorings, gliders, and subsurface acoustically-tracked RAFOS floats have been used to collect temperature, salinity, and current data across the Labrador Sea, Irminger Sea, Reykjanes Ridge, Iceland Basin, Rockall-Hatton Plateau, and Rockall Trough. The specific objective of the OSNAP float program is to gather information on
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Condron, Alan. High Resolution Model Development to Quantify the Impact of Icebergs on the Stability of the Atlantic Meridional Overturning Circulation. Office of Scientific and Technical Information (OSTI), 2016. http://dx.doi.org/10.2172/1329258.

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Hill, Christopher. Abrupt Climate Change and the Atlantic Meridional Overturning Circulation: sensitivity and non-linear response to Arctic/sub-Arctic freshwater pulses. Collaborative research. Final report. Office of Scientific and Technical Information (OSTI), 2015. http://dx.doi.org/10.2172/1184378.

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8

Bigorre, Sebastien P., Raymond Graham,, and Matthias Lankhorst. The Northwest Tropical Atlantic Station (NTAS): NTAS-21 Mooring Turnaround Cruise Report Cruise On Board RV Ronald H. Brown JOctober 6-25, 2022 Bridgetown, Barbados – Bridgetown, Barbados. Woods Hole Oceanographic Institution, 2023. http://dx.doi.org/10.1575/1912/66127.

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Abstract:
The Northwest Tropical Atlantic Station (NTAS) was established to address the need for accurate air-sea flux estimates and upper ocean measurements in a region with strong sea surface temperature anomalies and the likelihood of significant local air–sea interaction on interannual to decadal timescales. The approach is to maintain a surface mooring outfitted for meteorological and oceanographic measurements at a site near 15°N, 51°W by successive mooring turnarounds. These observations are used to investigate air–sea interaction processes related to climate variability. The NTAS Ocean Reference
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9

Bigorre, Sebastien P., and Raymond Graham. The Northwest Tropical Atlantic Station (NTAS): NTAS-20 Mooring Turnaround Cruise Report Cruise On Board RV Pisces November 4-28, 2021 Newport, RI - Pascagoula, MS. Woods Hole Oceanographic Institution, 2023. http://dx.doi.org/10.1575/1912/29647.

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Abstract:
The Northwest Tropical Atlantic Station (NTAS) was established to address the need for accurate air-sea flux estimates and upper ocean measurements in a region with strong sea surface temperature anomalies and the likelihood of significant local air–sea interaction on interannual to decadal timescales. The approach is to maintain a surface mooring outfitted for meteorological and oceanographic measurements at a site near 15°N, 51°W by successive mooring turnarounds. These observations are used to investigate air–sea interaction processes related to climate variability. The NTAS Ocean Reference
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