Now showing items 1297-1316 of 4897

  • Eddies in the Canada Basin, Arctic Ocean, observed from ice-tethered profilers 

    Timmermans, Mary-Louise; Toole, John M.; Proshutinsky, Andrey; Krishfield, Richard A.; Plueddemann, Albert J. (American Meteorological Society, 2008-01)
    Five ice-tethered profilers (ITPs), deployed between 2004 and 2006, have provided detailed potential temperature θ and salinity S profiles from 21 anticyclonic eddy encounters in the central Canada Basin of the Arctic ...
  • Eddy dynamics of ß plumes 

    Kida, Shinichiro (Massachusetts Institute of Technology and Woods Hole Oceanographic Institution, 2003-09)
    The importance of eddies and nonlinearities in ß-plume dynamics in the deep ocean was investigated using reduced gravity models of the deep ocean forced by a small region of cross isopycnal transport in the interior. The ...
  • Eddy forcing of the mean circulation in the western North Atlantic 

    Brown, Ellen Dunning (Massachusetts Institute of Technology and Woods Hole Oceanographic Institution, 1984-08)
    This thesis addresses several aspects of the problem of determining the effect of the low-frequency eddy variability on the mean circulation of the Western North Atlantic. A framework for this study is first established ...
  • Eddy formation near the west coast of Greenland 

    Bracco, Annalisa; Pedlosky, Joseph; Pickart, Robert S. (American Meteorological Society, 2008-09)
    This paper extends A. Bracco and J. Pedlosky’s investigation of the eddy-formation mechanism in the eastern Labrador Sea by including a more realistic depiction of the boundary current. The quasigeostrophic model consists ...
  • Eddy generation at a convex corner by a coastal current in a rotating system 

    Klinger, Barry A. (Massachusetts Institute of Technology and Woods Hole Oceanographic Institution, 1992-03)
    Rotating baroclinic and barotropic boundary currents flowing around a corner in the laboratory were studied in order to discover the circumstances under which eddies were produced at the corner. Such flows are reminiscent ...
  • Eddy stirring in the Southern Ocean 

    Naveira Garabato, Alberto C.; Ferrari, Raffaele; Polzin, Kurt L. (American Geophysical Union, 2011-09-17)
    There is an ongoing debate concerning the distribution of eddy stirring across the Antarctic Circumpolar Current (ACC) and the nature of its controlling processes. The problem is addressed here by estimating the isentropic ...
  • Eddy transport of organic carbon and nutrients from the Chukchi Shelf : impact on the upper halocline of the western Arctic Ocean 

    Mathis, Jeremy T.; Pickart, Robert S.; Hansell, Dennis A.; Kadko, David; Bates, Nicholas R. (American Geophysical Union, 2007-05-04)
    In September 2004 a detailed physical and chemical survey was conducted on an anticyclonic, cold-core eddy located seaward of the Chukchi Shelf in the western Arctic Ocean. The eddy had a diameter of ∼16 km and was centered ...
  • Eddy-driven pulses of respiration in the Sargasso Sea 

    Mourino-Carballido, Beatriz (2009-02)
    An analysis of nine years of data from the NW subtropical Atlantic reveals that variability in heterotrophic processes associated with (sub)mesoscale features has a major impact on the balance between photosynthesis and ...
  • Eddy-driven sediment transport in the Argentine Basin : is the height of the Zapiola Rise hydrodynamically controlled? 

    Weijer, Wilbert; Maltrud, Mathew E.; Homoky, William B.; Polzin, Kurt L.; Maas, Leo R. M. (John Wiley & Sons, 2015-03-27)
    In this study, we address the question whether eddy-driven transports in the Argentine Basin can be held responsible for enhanced sediment accumulation over the Zapiola Rise, hence accounting for the existence and growth ...
  • Eddy-induced particle dispersion in the near-surface North Atlantic 

    Rypina, Irina I.; Kamenkovich, Igor V.; Berloff, Pavel S.; Pratt, Lawrence J. (American Meteorological Society, 2012-12)
    This study investigates the anisotropic properties of the eddy-induced material transport in the near-surface North Atlantic from two independent datasets, one simulated from the sea surface height altimetry and one derived ...
  • Eddy-mean flow interactions in western boundary current jets 

    Waterman, Stephanie N. (Massachusetts Institute of Technology and Woods Hole Oceanographic Institution, 2009-02)
    This thesis examines the nature of eddy-mean flow interactions in western boundary current jets and recirculation gyre dynamics from both theoretical and observational perspectives. It includes theoretical studies of ...
  • Eddy-resolving simulation of plankton ecosystem dynamics in the California Current System 

    Gruber, Nicolas; Frenzel, Hartmut; Doney, Scott C.; Marchesiello, Patrick; McWilliams, James C.; Moisan, John R.; Oram, John J.; Plattner, Gian-Kasper; Stolzenbach, Keith D. (2006-06-13)
    We study the dynamics of the planktonic ecosystem in the coastal upwelling zone within the California Current System using a three-dimensional, eddy-resolving circulation model coupled to an ecosystem/biogeochemistry ...
  • Eddys in the Arctic Ocean from IOEB ADCP data 

    Krishfield, Richard A.; Plueddemann, Albert J.; Honjo, Susumu (Woods Hole Oceanographic Institution, 2002-10)
    Filtered and Earth-referenced ADCP data from the B92, B97 and S97 IOEBs were demodulated to remove inertial and near-inertial tidal frequencies, in order to highlight the low frequency components for examination of Arctic ...
  • Eddy–mean flow interaction in the Kuroshio Extension region 

    Waterman, Stephanie N.; Hogg, Nelson G.; Jayne, Steven R. (American Meteorological Society, 2011-06)
    The authors use data collected by a line of tall current meter moorings deployed across the axis of the Kuroshio Extension (KE) jet at the location of maximum time-mean eddy kinetic energy to characterize the mean jet ...
  • The effect of a shallow low viscosity zone on mantle convection and its expression at the surface of the earth 

    Robinson, Elizabeth M. (Massachusetts Institute of Technology and Woods Hole Oceanographic Institution, 1987-08)
    Many features of the oceanic plates cannot be explained by conductive cooling with age. A number of these anomalies require additional convective thermal sources at depths below the plate: mid-plate swells, the evolution ...
  • The effect of breaking waves on a coupled model of wind and ocean surface waves. Part I : mature seas 

    Kukulka, Tobias; Hara, Tetsu (American Meteorological Society, 2008-10)
    This is the first of a two-part investigation of a coupled wind and wave model that includes the enhanced form drag of breaking waves. In Part I here the model is developed and applied to mature seas. Part II explores the ...
  • The effect of breaking waves on a coupled model of wind and ocean surface waves. Part II : growing seas 

    Kukulka, Tobias; Hara, Tetsu (American Meteorological Society, 2008-10)
    This is the second part of a two-part investigation of a coupled wind and wave model that includes the enhanced form drag of breaking waves. The model is based on the wave energy balance and the conservation of air-side ...
  • Effect of carbon addition and predation on acetate-assimilating bacterial cells in groundwater 

    Longnecker, Krista; Da Costa, Andreia; Bhatia, Maya P.; Kujawinski, Elizabeth B. (2009-07-13)
    Groundwater microbial community dynamics are poorly understood due to the challenges associated with accessing subsurface environments. In particular, microbial interactions and their impact on the subsurface carbon cycle ...
  • Effect of continental shelf canyons on phytoplankton biomass and community composition along the western Antarctic Peninsula 

    Kavanaugh, Maria T.; Abdala, F. N.; Ducklow, Hugh W.; Glover, David M.; Fraser, William R.; Martinson, Douglas G.; Stammerjohn, Sharon E.; Schofield, Oscar M. E.; Doney, Scott C. (Inter-Research, 2015-03-30)
    The western Antarctic Peninsula is experiencing dramatic climate change as warm, wet conditions expand poleward and interact with local physics and topography, causing differential regional effects on the marine ecosystem. ...
  • The effect of diurnal sea surface temperature warming on climatological air–sea fluxes 

    Clayson, Carol Anne; Bogdanoff, Alec S. (American Meteorological Society, 2013-04-15)
    Diurnal sea surface warming affects the fluxes of latent heat, sensible heat, and upwelling longwave radiation. Diurnal warming most typically reaches maximum values of 3°C, although very localized events may reach 7°–8°C. ...