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    Hydraulic Control of Three-Layer Exchange Flows: Application to the Bab al Mandab 

    Source: Journal of Physical Oceanography:;2000:;Volume( 030 ):;issue: 010:;page 2574
    Author(s): Smeed, David A.
    Publisher: American Meteorological Society
    Abstract: Two-layer hydraulic models have proven to be extremely useful in understanding a number of exchange flows through straits, for example, the Strait of Gibraltar. There are, though, some strait flows that cannot be represented ...
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    Underwater Glider Reliability and Implications for Survey Design 

    Source: Journal of Atmospheric and Oceanic Technology:;2014:;volume( 031 ):;issue: 012:;page 2858
    Author(s): Brito, Mario; Smeed, David; Griffiths, Gwyn
    Publisher: American Meteorological Society
    Abstract: t has been 20 years since the concept of the Autonomous Ocean Sampling Network (AOSN) was first introduced. This vision has been brought closer to reality with the introduction of underwater gliders. While in terms of ...
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    Vertical Water Velocities from Underwater Gliders 

    Source: Journal of Atmospheric and Oceanic Technology:;2010:;volume( 027 ):;issue: 003:;page 547
    Author(s): Merckelbach, Lucas; Smeed, David; Griffiths, Gwyn
    Publisher: American Meteorological Society
    Abstract: The underwater glider is set to become an important platform for oceanographers to gather data within oceans. Gliders are usually equipped with a conductivity?temperature?depth (CTD) sensor, but a wide range of other sensors ...
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    The Effects on Ocean Models of Relaxation toward Observations at the Surface 

    Source: Journal of Physical Oceanography:;2000:;Volume( 030 ):;issue: 001:;page 160
    Author(s): Killworth, Peter D.; Smeed, David A.; Nurser, A. J. George
    Publisher: American Meteorological Society
    Abstract: This paper discusses the errors in surface tracer and flux fields in ocean models induced by using approximate surface boundary conditions involving relaxation toward observed values rather than more physically realistic ...
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    Eddy-Induced Modulation of Turbulent Dissipation over Rough Topography in the Southern Ocean 

    Source: Journal of Physical Oceanography:;2013:;Volume( 043 ):;issue: 011:;page 2288
    Author(s): Brearley, J. Alexander; Sheen, Katy L.; Naveira Garabato, Alberto C.; Smeed, David A.; Waterman, Stephanie
    Publisher: American Meteorological Society
    Abstract: esoscale eddies are universal features of the ocean circulation, yet the processes by which their energy is dissipated remain poorly understood. One hypothesis argues that the interaction of strong geostrophic flows with ...
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    Observation of a Large Lee Wave in the Drake Passage 

    Source: Journal of Physical Oceanography:;2017:;Volume( 047 ):;issue: 004:;page 793
    Author(s): Cusack, Jesse M.; Naveira Garabato, Alberto C.; Smeed, David A.; Girton, James B.
    Publisher: American Meteorological Society
    Abstract: ee waves are thought to play a prominent role in Southern Ocean dynamics, facilitating a transfer of energy from the jets of the Antarctic Circumpolar Current to microscale, turbulent motions important in water mass ...
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    Teleconnection between the Atlantic Meridional Overturning Circulation and Sea Level in the Mediterranean Sea 

    Source: Journal of Climate:;2018:;volume 032:;issue 003:;page 935
    Author(s): Volkov, Denis L.; Baringer, Molly; Smeed, David; Johns, William; Landerer, Felix W.
    Publisher: American Meteorological Society
    Abstract: The Mediterranean Sea can be viewed as a ?barometer? of the North Atlantic Ocean, because its sea level responds to oceanic-gyre-scale changes in atmospheric pressure and wind forcing, related to the North Atlantic Oscillation ...
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    Observed Eddy–Internal Wave Interactions in the Southern Ocean 

    Source: Journal of Physical Oceanography:;2020:;volume( 50 ):;issue: 010:;page 3043
    Author(s): Cusack, Jesse M.;Brearley, J. Alexander;Naveira Garabato, Alberto C.;Smeed, David A.;Polzin, Kurt L.;Velzeboer, Nick;Shakespeare, Callum J.
    Publisher: American Meteorological Society
    Abstract: The physical mechanisms that remove energy from the Southern Ocean’s vigorous mesoscale eddy field are not well understood. One proposed mechanism is direct energy transfer to the internal wave field in the ocean interior, ...
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    Global Oceans 

    Source: Bulletin of the American Meteorological Society:;2020:;volume( 101 ):;issue: 008:;page S129
    Author(s): Baringer, Molly;Bif, Mariana B.;Boyer, Tim;Bushinsky, Seth M.;Carter, Brendan R.;Cetinić, Ivona;Chambers, Don P.;Cheng, Lijing;Chiba, Sanai;Dai, Minhan;Domingues, Catia M.;Dong, Shenfu;Fassbender, Andrea J.;Feely, Richard A.;Frajka-Williams, Eleanor;Franz, Bryan A.;Gilson, John;Goni, Gustavo;Hamlington, Benjamin D.;Hu, Zeng-Zhen;Huang, Boyin;Ishii, Masayoshi;Jevrejeva, Svetlana;Johns, William E.;Johnson, Gregory C.;Johnson, Kenneth S.;Kennedy, John;Kersalé, Marion;Killick, Rachel E.;Landschützer, Peter;Lankhorst, Matthias;Lee, Tong;Leuliette, Eric;Li, Feili;Lindstrom, Eric;Locarnini, Ricardo;Lozier, Susan;Lyman, John M.;Marra, John J.;Meinen, Christopher S.;Merrifield, Mark A.;Mitchum, Gary T.;Moat, Ben;Monselesan, Didier;Nerem, R. Steven;Perez, Renellys C.;Purkey, Sarah G.;Rayner, Darren;Reagan, James;Rome, Nicholas;Sanchez-Franks, Alejandra;Schmid, Claudia;Scott, Joel P.;Send, Uwe;Siegel, David A.;Smeed, David A.;Speich, Sabrina;Stackhouse, Paul W., Jr.;Sweet, William;Takeshita, Yuichiro;Thompson, Philip R.;Triñanes, Joaquin A.;Visbeck, Martin;Volkov, Denis L.;Wanninkhof, Rik;Weller, Robert A.;Westberry, Toby K.;Widlansky, Matthew J.;Wijffels, Susan E.;Wilber, Anne C.;Yu, Lisan;Yu, Weidong;Zhang, Huai-Min
    Publisher: American Meteorological Society
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