- Ocean 420 Winter 2007 Project 7 Answers
- Thompson/Ocean 420/Winter 2005 Internal Gravity Waves 1 I. Two-layer internal waves
- Kawase/Ocean 420/Winter 2006 Dynamic Height and Thermal Wind 1 Dynamic height (at pressure p relative to pressure p0.)
- Thompson/Ocean 420/Winter 2005 Inertial Oscillations 1 Inertial Oscillations
- Thompson/Ocean 420/Winter 2004 2D waves 1 Two-dimensional wave propagation
- Ocean 420 Physical Processes in the Ocean Project 2: Force Balance and Geostrophy
- DECEMBER 2002 3657N O T E S A N D C O R R E S P O N D E N C E 2002 American Meteorological Society
- Thompson/Ocean 420/Winter 2005 Tide Dynamics 1 Tide Dynamics
- Thompson/Ocean 420/Winter 2004 Kelvin Waves 1 Kelvin Waves
- 3436 VOLUME 32J O U R N A L O F P H Y S I C A L O C E A N O G R A P H Y 2002 American Meteorological Society
- Ocean 420 Physical Processes in the Ocean Project 3: Ekman Transport
- STEADY-STATE FORCE BALANCES (1) Pressure gradient and Coriolis forces
- JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 105, NO. C3, PAGES 6437-6451, MARCH 15, 2000 Eklnan layers and two-dimensionalfrontogenesis
- Effect of ocean surface currents on wind stress, heat flux, and wind power input to the ocean
- Short Communication Propagation of wind and buoyancy forced density anomalies
- PDO-Related Heat and Temperature Budget Changes in a Model of the North Pacific JORDAN T. DAWE
- Kawase/Ocean 420/Winter 2006 Introduction 1 What We Study in Physical Oceanography
- Kawase/Ocean 420/Winter 2006 Conservation 1 Conservation
- Kawase/Ocean 420/Winter 2006 Rotation 1 An important concept in understanding ocean circulation is the effect of the earth's
- Kawase/Ocean 420/Winter 2006 Bottom Ekman Layer 1 Bottom Boundary Layers
- Kawase/Ocean 420/Winter 2006 Upwelling 1 Coastal upwelling circulation
- Thompson/Ocean 420/Winter 2004 Surface Gravity Surface Gravity Waves
- Thompson/Ocean 420/Winter 2005 Internal Gravity Waves 1 II. Internal waves in continuous stratification
- Ocean 420 Physical Processes in the Ocean Project 3: Force Balance and Ekman Transport
- Ocean 420 Winter 2007 Due: February 22
- Ocean 420 Physical Processes in the Ocean Project 6: Waves
- Ocean 420 Physical Processes in the Ocean Project 9: Internal waves, inertial oscillations and Kelvin waves
- Equations in Ocean 420 = g Hydrostatic balance
- Thompson/Ocean 420/Winter 2005 Local character of Tidal character in local waters.
- Equilibrium Tides Along with surface gravity waves, the predictable rise and fall of sea level at the coast are
- Viscosity-Dependent Internal Variability in a Model of the North Pacific JORDAN T. DAWE AND LUANNE THOMPSON
- Kawase/Ocean 420/Winter 2006 Ekman layers 1 Ekman layers
- Ocean 420 Physical Processes in the Ocean Project 6: Waves
- Short communication Equatorial influence of QuikSCAT winds in an isopycnal ocean model
- Ocean 420 Physical Processes in the Ocean Project 1: Hydrostatic Balance, Advection and Diffusion
- Variables and units in Ocean 420 u zonal velocity (east-west) m/s
- Kawase/Ocean 420/Winter 2006 Equation of Motion 1 Equation of Motion
- Kawase/Ocean 420/Winter 2006 Friction and turbulent stress 1 Equations of Motion Revisited
- Ocean 420 Physical Processes in the Ocean Answers to Project 9: Internal waves
- Thompson/Ocean 420/Winter 2004 Waves Introduction 1 What is a wave? It is a physical process whereby energy (or information about boundary
- Ocean 420 Physical Processes in the Ocean Project 2: Force Balance and Geostrophy
- Ocean 420 Physical Processes in the Ocean Project 6: Waves
- Kawase/Ocean 420/Winter 2006 Geostrophy 1 What other forces act on water parcels in the ocean?
- Water Masses in the Pacific in CCSM3 LUANNE THOMPSON
- Evaluation of HYCOM in the Kuroshio Extension region using new metrics
- Ocean 420 Physical Processes in the Ocean Answers to Project 8: Waves
- Thompson/Ocean 420/Winter 2005 Surface Gravity Wave Surface Gravity Wave Generation
