Tides of the northwestern Ross Sea and their impact on dense outflows of Antarctic Bottom Water

[1]  H. Hasumi,et al.  Modeling ice shelf water overflow and bottom water formation in the southern Weddell Sea , 2010 .

[2]  A. Orsi,et al.  A recount of Ross Sea waters , 2009 .

[3]  A. Gordon,et al.  Southern Ocean shelf slope exchange , 2009 .

[4]  G. Budillon,et al.  The nepheloid bottom layer and water masses at the shelf break of the western Ross Sea , 2009 .

[5]  A. Gordon,et al.  Western Ross Sea continental slope gravity currents , 2009 .

[6]  A. Thurnherr,et al.  High-resolution velocity and hydrographic observations of the Drygalski Trough gravity plume , 2009 .

[7]  A. Gordon,et al.  A dense water outflow from the Ross Sea, Antarctica: Mixing and the contribution of tides , 2009 .

[8]  T. Painter,et al.  MODIS-based Mosaic of Antarctica (MOA) data sets: Continent-wide surface morphology and snow grain size , 2007 .

[9]  M. Dinniman,et al.  Influence of sea ice cover and icebergs on circulation and water mass formation in a numerical circulation model of the Ross Sea, Antarctica , 2007 .

[10]  A. Orsi,et al.  Antarctic Bottom Water production and export by tides in the Ross Sea , 2006 .

[11]  Eric S. Johnson,et al.  Tidal currents of the Ross Sea and their time stability , 2006, Antarctic Science.

[12]  G. Egbert,et al.  Assimilation of Ship-Mounted ADCP Data for Barotropic Tides: Application to the Ross Sea , 2005 .

[13]  R. Robertson Baroclinic and barotropic tides in the Ross Sea , 2005, Antarctic Science.

[14]  Enrico Zambianchi,et al.  Energetic plumes over the western Ross Sea continental slope , 2004 .

[15]  A. Jenkins,et al.  Water mass modification over the continental shelf north of Ronne Ice Shelf, Antarctica , 2003 .

[16]  James C. McWilliams,et al.  A method for computing horizontal pressure‐gradient force in an oceanic model with a nonaligned vertical coordinate , 2003 .

[17]  Ian Joughin,et al.  Tides of the Ross Sea and Ross Ice Shelf cavity , 2003, Antarctic Science.

[18]  S. Lentz,et al.  Classical tidal harmonic analysis including error estimates in MATLAB using T_TIDE , 2002 .

[19]  J. Berntsen Internal Pressure Errors in Sigma-Coordinate Ocean Models , 2002 .

[20]  M. Levine,et al.  A Correction to the Baroclinic Pressure Gradient Term in the Princeton Ocean Model , 2001 .

[21]  Dale R. Durran,et al.  Further Comments on “The Differentiation between Grid Spacing and Resolution and Their Application to Numerical Modeling” , 2001 .

[22]  Michael K. Walters,et al.  commentary and analysis: Comments on "The Differentiation between Grid Spacing and Resolution and Their Application to Numerical Modeling" , 2000 .

[23]  K. Nicholls,et al.  Modeling tidal currents beneath Filchner‐Ronne Ice Shelf and on the adjacent continental shelf: Their effect on mixing and transport , 1999 .

[24]  Dale B. Haidvogel,et al.  Numerical Ocean Circulation Modeling , 1999 .

[25]  J. Molines,et al.  A sigma-coordinate primitive equation model for studying the circulation in the South Atlantic. Part I: Model configuration with error estimates , 1998 .

[26]  John M. Toole,et al.  Tidally Driven Vorticity, Diurnal Shear, and Turbulence atop Fieberling Seamount , 1997 .

[27]  Walter H. F. Smith,et al.  Global Sea Floor Topography from Satellite Altimetry and Ship Depth Soundings , 1997 .

[28]  Harold T. Shapiro Ethical and policy issues of human cloning. , 1997, Science.

[29]  D. DeMaster,et al.  Lateral transport of settling particles in the Ross Sea and implications for the fate of biogenic material , 1996 .

[30]  George L. Mellor,et al.  The Pressure Gradient Conundrum of Sigma Coordinate Ocean Models , 1994 .

[31]  Dale B. Haidvogel,et al.  Numerical Simulation of Flow around a Tall Isolated Seamount. Part I: Problem Formulation and Model Accuracy , 1993 .

[32]  R. Pinkel,et al.  Diurnal tides near the Yermak Plateau , 1992 .

[33]  S. Jacobs On the nature and significance of the Antarctic Slope Front , 1991 .

[34]  Robert L. Haney,et al.  On the Pressure Gradient Force over Steep Topography in Sigma Coordinate Ocean Models , 1991 .

[35]  J. Middleton,et al.  Mixing and bottom water formation in the shelf break region of the southern Weddell Sea , 1987 .

[36]  T. Foster,et al.  Diurnal Shelf Waves in the Southern Weddell Sea , 1987 .

[37]  D. Macayeal Numerical simulations of the Ross Sea tides , 1984 .

[38]  S. Pond,et al.  Introductory Dynamical Oceanography , 1983 .

[39]  G. Mellor,et al.  Development of a turbulence closure model for geophysical fluid problems , 1982 .

[40]  F. Carsey Microwave Observation of the Weddell Polynya , 1980 .

[41]  J. Loder Topographic Rectification of Tidal Currents on the Sides of Georges Bank , 1980 .

[42]  Arnold L. Gordon,et al.  Deep Antarctic Convection West of Maud Rise , 1978 .

[43]  J. Hunter,et al.  Fronts in the Irish Sea , 1974, Nature.

[44]  S. Jacobs,et al.  Ross sea oceanography and antarctic bottom water formation , 1970 .

[45]  S. Jacobs,et al.  Influence of submarine morphology on bottom water flow across the western Ross Sea continental margin , 2007 .

[46]  R. Muench,et al.  Internal tide generation along the South Scotia Ridge , 2006 .

[47]  M. Batteen,et al.  On reducing the slope parameter in terrain-following numerical ocean models , 2006 .

[48]  Alexander F. Shchepetkin,et al.  The regional oceanic modeling system (ROMS): a split-explicit, free-surface, topography-following-coordinate oceanic model , 2005 .

[49]  E. Fahrbach,et al.  Ice shelf water overflow and bottom water formation in the southern , 2004 .

[50]  Richard Coleman,et al.  A new tide model for the Antarctic ice shelves and seas , 2002, Annals of Glaciology.

[51]  Lewis D. Grasso,et al.  The differentiation between grid spacing and resolution and their application to numerical modeling , 2000 .

[52]  Ray F. Weiss,et al.  Ocean, Ice, and Atmosphere: Interactions at the Antarctic Continental Margin , 1998 .

[53]  James C. McWilliams,et al.  The Regional Ocean Modeling System : A Split-Explicit , Free-Surface , Topography-Following-Coordinate Ocean Model , 2022 .