59 Geostrophy PPTs View free & download

Geostrophy - Hydrostatic Pressure. Hydrostatic pressure is simply the weight of water acting on a unit area at ... Hydrostatics give us ph = r g D ...

Hydrostatic Pressure. Hydrostatic pressure is simply the weight of water acting on a unit area at ... Hydrostatics give us ph = r g D ...

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Geostrophic and thermal wind PowerPoint PPT Presentation

Geostrophic and thermal wind - Geostrophic and thermal wind Reminder Geostrophic wind in pressure coordinates In the free atmosphere, wind is usually close to geostrophic. The departure from ...

Geostrophic and thermal wind Reminder Geostrophic wind in pressure coordinates In the free atmosphere, wind is usually close to geostrophic. The departure from ...

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Coriolis and Geostrophy PowerPoint PPT Presentation

Coriolis and Geostrophy - Geostrophic Currents and Winds. In geostrophic equilibrium, the horizontal pressure gradient force balances the Coriolis force. ...

Geostrophic Currents and Winds. In geostrophic equilibrium, the horizontal pressure gradient force balances the Coriolis force. ...

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Mass convergence from geostrophy and ADCP measurements PowerPoint PPT Presentation

Mass convergence from geostrophy and ADCP measurements - Apply a fitted coefficient in order to make the two lengths match. ... northeast until the 27th, southeast later on. Ekman transport ...

Apply a fitted coefficient in order to make the two lengths match. ... northeast until the 27th, southeast later on. Ekman transport ...

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Pressure Gradient Force PowerPoint PPT Presentation

Pressure Gradient Force - Geostrophic Balance. If: Only important forces are Pressure ... Geostrophic Currents. In x-dir: fv = 1 dp. Assuming the current is uniform ... Geostrophic ...

Geostrophic Balance. If: Only important forces are Pressure ... Geostrophic Currents. In x-dir: fv = 1 dp. Assuming the current is uniform ... Geostrophic ...

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EVAT 554 OCEAN-ATMOSPHERE DYNAMICS PowerPoint PPT Presentation

EVAT 554 OCEAN-ATMOSPHERE DYNAMICS - EVAT 554. OCEAN-ATMOSPHERE DYNAMICS. FILTERING OF EQUATIONS FOR ATMOSPHERE ... Advection. Horizontal Momentum Balance. Geostrophic Balance (zonal) (meridional) ...

EVAT 554. OCEAN-ATMOSPHERE DYNAMICS. FILTERING OF EQUATIONS FOR ATMOSPHERE ... Advection. Horizontal Momentum Balance. Geostrophic Balance (zonal) (meridional) ...

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Ocean Modeling EAS 8803 PowerPoint PPT Presentation

Ocean Modeling EAS 8803 - if pressure only a function of the sea level. Properties of Geostrophic homogeneous flows ... NEW continuity equation! Equations of Geostrophic homogeneous flows ...

if pressure only a function of the sea level. Properties of Geostrophic homogeneous flows ... NEW continuity equation! Equations of Geostrophic homogeneous flows ...

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Secondary Upwelling along the shelf break Vincent Rossi, Yves Morel, Vronique Garon PowerPoint PPT Presentation

Secondary Upwelling along the shelf break Vincent Rossi, Yves Morel, Vronique Garon - PV = (z f) . r (= (z f)/h ) is conserved for each ... knowledge of PVA (if geostrophic. balance is assumed) INVERSION PRINCIPLE. z. d PV 0 = cyclonic ...

PV = (z f) . r (= (z f)/h ) is conserved for each ... knowledge of PVA (if geostrophic. balance is assumed) INVERSION PRINCIPLE. z. d PV 0 = cyclonic ...

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Announcements PowerPoint PPT Presentation

Announcements - Announcements Exam #1 will be handed back Wednesday or Friday. First homework assignment due next Monday. No class Wednesday before Thanksgiving.

Announcements Exam #1 will be handed back Wednesday or Friday. First homework assignment due next Monday. No class Wednesday before Thanksgiving.

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The General Circulation of the Atmosphere PowerPoint PPT Presentation

The General Circulation of the Atmosphere - Advection The horizontal movement of air or atmospheric properties, solely by ... Measure of the relative importance of rotation and advection ...

Advection The horizontal movement of air or atmospheric properties, solely by ... Measure of the relative importance of rotation and advection ...

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Rotating Fluid -Part II A PowerPoint PPT Presentation

Rotating Fluid -Part II A - Rotating Fluid -Part II A GFD view of the Ocean and the Atmosphere (a follow up Raymond s Lectures) Arnaud Czaja

Rotating Fluid -Part II A GFD view of the Ocean and the Atmosphere (a follow up Raymond s Lectures) Arnaud Czaja

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1.%20The%20thermodynamic%20energy%20equation PowerPoint PPT Presentation

1.%20The%20thermodynamic%20energy%20equation - ATOC 4720 class35 1. The thermodynamic energy equation 2. The continuity equation Previous classes Cross-isobar flow due to friction The gradient wind Hydrostatic ...

ATOC 4720 class35 1. The thermodynamic energy equation 2. The continuity equation Previous classes Cross-isobar flow due to friction The gradient wind Hydrostatic ...

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---%20Introduction%20to%20Geophysical%20Fluid%20Dynamics PowerPoint PPT Presentation

---%20Introduction%20to%20Geophysical%20Fluid%20Dynamics - Ch. 7 Fundamentals of Atmospheric/Ocean Modeling--- Introduction to Geophysical Fluid Dynamics Pressure Gradient Force (PGF) Coriolis effect seen on a rotating ...

Ch. 7 Fundamentals of Atmospheric/Ocean Modeling--- Introduction to Geophysical Fluid Dynamics Pressure Gradient Force (PGF) Coriolis effect seen on a rotating ...

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Physical Oceanography PowerPoint PPT Presentation

Physical Oceanography - 75% of the ocean has a salinity of 34-35 ppt and a temperature of 0-6 deg C. ... As the ocean is in hydrostatic equilibrium, the redistribution of the buoyant ...

75% of the ocean has a salinity of 34-35 ppt and a temperature of 0-6 deg C. ... As the ocean is in hydrostatic equilibrium, the redistribution of the buoyant ...

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CHAPTER 4: ATMOSPHERIC MOTIONS and TRANSPORT PowerPoint PPT Presentation

CHAPTER 4: ATMOSPHERIC MOTIONS and TRANSPORT - CHAPTER 4: ATMOSPHERIC MOTIONS and TRANSPORT WHAT ARE THE FORCES BEHIND ATMOSPHERIC CIRCULATION? Global Circulation as a Giant Sea Breeze. Concepts: Pressure Gradient ...

CHAPTER 4: ATMOSPHERIC MOTIONS and TRANSPORT WHAT ARE THE FORCES BEHIND ATMOSPHERIC CIRCULATION? Global Circulation as a Giant Sea Breeze. Concepts: Pressure Gradient ...

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The Role of Canyons, Promontories and Topography in DOES PowerPoint PPT Presentation

The Role of Canyons, Promontories and Topography in DOES - The Role of Canyons, Promontories and Topography in DOES Susan Allen, Department of Earth & Ocean Science University of British Columbia Vancouver, Canada

The Role of Canyons, Promontories and Topography in DOES Susan Allen, Department of Earth & Ocean Science University of British Columbia Vancouver, Canada

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40-70 Day Meridional Propagation of Global Circulation Anomalies (A Global Convection Circulation Paradigm for the Annular Mode) PowerPoint PPT Presentation

40-70 Day Meridional Propagation of Global Circulation Anomalies (A Global Convection Circulation Paradigm for the Annular Mode) - 40-70 Day Meridional Propagation of Global Circulation Anomalies (A Global Convection Circulation Paradigm for the Annular Mode) Ming Cai1 and R-C Ren1,2

40-70 Day Meridional Propagation of Global Circulation Anomalies (A Global Convection Circulation Paradigm for the Annular Mode) Ming Cai1 and R-C Ren1,2

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Steady State General Ocean Circulation PowerPoint PPT Presentation

Steady State General Ocean Circulation - Steady State General Ocean Circulation steady state means: constant in time, no accelerations or Sum of all forces = 0 Outline: 1. Ekman dynamics (Coriolis ...

Steady State General Ocean Circulation steady state means: constant in time, no accelerations or Sum of all forces = 0 Outline: 1. Ekman dynamics (Coriolis ...

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QG Dynamics - QG Dynamics A Review Anthony R. Lupo Department of Soil, Environmental, and Atmospheric Science 302 E ABNR Building University of Missouri Columbia, MO 65211

QG Dynamics A Review Anthony R. Lupo Department of Soil, Environmental, and Atmospheric Science 302 E ABNR Building University of Missouri Columbia, MO 65211

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Lowlevel jets Various types and causes PowerPoint PPT Presentation

Lowlevel jets Various types and causes - East of Front Range (&Appalachians) SE coast of S. Africa, Australia. Great Plains ... not usually steady-state (steady-state is possible, eg Antarctic winter night) ...

East of Front Range (&Appalachians) SE coast of S. Africa, Australia. Great Plains ... not usually steady-state (steady-state is possible, eg Antarctic winter night) ...

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NOAA's%2033rd%20Climate%20Diagnostics%20and%20Prediction%20Workshop/CLIVAR%20Drought%20Workshop%20(CDPW)%20October%2020-24,%202008%20in%20Lincoln,%20Nebraska - none

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Variational Assimilation of HF Radar Surface Currents into the Coastal Ocean Circulation Model off Oregon PowerPoint PPT Presentation

Variational Assimilation of HF Radar Surface Currents into the Coastal Ocean Circulation Model off Oregon - ... (D. Folley, NOAA CoastWatch) gliders (T and S sections, once every 3 days, J Barth and R ... linear &adjoint codes AVRORA ... 5-10 steps ) (Egbert, 1997 ...

... (D. Folley, NOAA CoastWatch) gliders (T and S sections, once every 3 days, J Barth and R ... linear &adjoint codes AVRORA ... 5-10 steps ) (Egbert, 1997 ...

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CS 401: Applied Scientific PowerPoint PPT Presentation

CS 401: Applied Scientific - Science & Engineering. Scientific. computing. pure. applied. CIS Tools Curriculum ' ... Role of Computing in Science and Engineering ...

Science & Engineering. Scientific. computing. pure. applied. CIS Tools Curriculum ' ... Role of Computing in Science and Engineering ...

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Winddriven Circulation PowerPoint PPT Presentation

Winddriven Circulation - ... conditions in the red box... Ekman Transport. Westerlies. Trades ... The red box... Convergence (sea surface pile-up) Pressure gradient force. Coriolis force ...

... conditions in the red box... Ekman Transport. Westerlies. Trades ... The red box... Convergence (sea surface pile-up) Pressure gradient force. Coriolis force ...

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Barrier jets and other lowlevel jets a description of types and causes PowerPoint PPT Presentation

Barrier jets and other lowlevel jets a description of types and causes - Schwerdtfeger (1975, 1979) describes a barrier jet along the ... as an ageostrophic response to the damming of stably-stratified flow by the Sierra Nevada. ...

Schwerdtfeger (1975, 1979) describes a barrier jet along the ... as an ageostrophic response to the damming of stably-stratified flow by the Sierra Nevada. ...

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SAMOC: South Atlantic Meridional Overturning Circulation PowerPoint PPT Presentation

SAMOC: South Atlantic Meridional Overturning Circulation - SAMOC: South Atlantic Meridional Overturning Circulation International Programs and Plans http://www.aoml.noaa.gov/phod/research/moc/samoc/

SAMOC: South Atlantic Meridional Overturning Circulation International Programs and Plans http://www.aoml.noaa.gov/phod/research/moc/samoc/

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CHAPTER 4: ATMOSPHERIC MOTIONS and TRANSPORT - CHAPTER 4: ATMOSPHERIC MOTIONS and TRANSPORT WHAT ARE THE FORCES BEHIND ATMOSPHERIC CIRCULATION? Global Circulation as a Giant Sea Breeze. Concepts: Pressure Gradient ...

CHAPTER 4: ATMOSPHERIC MOTIONS and TRANSPORT WHAT ARE THE FORCES BEHIND ATMOSPHERIC CIRCULATION? Global Circulation as a Giant Sea Breeze. Concepts: Pressure Gradient ...

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4070 Day Meridional Propagation of Global Circulation Anomalies A Global Convection Circulation Para PowerPoint PPT Presentation

4070 Day Meridional Propagation of Global Circulation Anomalies A Global Convection Circulation Para - 40-70 Day Meridional Propagation of Global Circulation Anomalies ... potential = u' 0 follows poleward propagating T' 0 by a quarter of period. ...

40-70 Day Meridional Propagation of Global Circulation Anomalies ... potential = u' 0 follows poleward propagating T' 0 by a quarter of period. ...

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Distribution and pathways of Atlantic Water in the Greenland Sea. - Distribution and pathways of Atlantic Water in the Greenland Sea'

Distribution and pathways of Atlantic Water in the Greenland Sea'

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What drives the oceanic circulation PowerPoint PPT Presentation

What drives the oceanic circulation - some of the observed main global surface current systems. ... piling-up more and more water along the Equator; a clear physical impossibility! ...

some of the observed main global surface current systems. ... piling-up more and more water along the Equator; a clear physical impossibility! ...

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The Global Salinity Budget PowerPoint PPT Presentation

The Global Salinity Budget - The Global Salinity Budget From before, salinity is mass salts per mass seawater (S = 1000 * kg salts / kg SW) There is a riverine source BUT ...

The Global Salinity Budget From before, salinity is mass salts per mass seawater (S = 1000 * kg salts / kg SW) There is a riverine source BUT ...

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Regional%20Coastal%20Ocean%20Modeling:%20Forcing PowerPoint PPT Presentation

Regional%20Coastal%20Ocean%20Modeling:%20Forcing - Regional Coastal Ocean Modeling: Forcing

Regional Coastal Ocean Modeling: Forcing

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Coastal and Shelf Processes - Coastal and Shelf Processes

Coastal and Shelf Processes

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QUESTIONS - Former Alberta Premier Ralph Klein once suggested that we all quit breathing as ... Cloud formation: promote aqueous phase chemistry. CHAPTER 4: ATMOSPHERIC TRANSPORT ...

Former Alberta Premier Ralph Klein once suggested that we all quit breathing as ... Cloud formation: promote aqueous phase chemistry. CHAPTER 4: ATMOSPHERIC TRANSPORT ...

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Data Assimilation for Hurricane Initialization PowerPoint PPT Presentation

Data Assimilation for Hurricane Initialization - (an exact fit to observations) or through a least-square fit between the analysis ... Least-square fit. What does data assimilation do? ...

(an exact fit to observations) or through a least-square fit between the analysis ... Least-square fit. What does data assimilation do? ...

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AOS 101 Discussion 303 TA Brian Miretzky PowerPoint PPT Presentation

AOS 101 Discussion 303 TA Brian Miretzky - Station models are an efficient and concise way to represent weather conditions ... Isohaline: A line of constant salinity (saltiness in the ocean) ...

Station models are an efficient and concise way to represent weather conditions ... Isohaline: A line of constant salinity (saltiness in the ocean) ...

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Atmospheric Composition and Contour Weather Maps PowerPoint PPT Presentation

Atmospheric Composition and Contour Weather Maps - How your weather is going to change! How to Think about Contouring. Like topographic map ... In the olden days, all weather maps and contour maps were done by hand! ...

How your weather is going to change! How to Think about Contouring. Like topographic map ... In the olden days, all weather maps and contour maps were done by hand! ...

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Matlab%20Programming PowerPoint PPT Presentation

Matlab%20Programming - Function m-files--analogous to subroutines or methods, maintain their own memory (workspace) ... finishes are returned to the workspace (or calling function) ...

Function m-files--analogous to subroutines or methods, maintain their own memory (workspace) ... finishes are returned to the workspace (or calling function) ...

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Weather Analysis: Contouring AOS 101 Section 302 PowerPoint PPT Presentation

Weather Analysis: Contouring AOS 101 Section 302 - Station models are an efficient and concise way to represent weather conditions ... Isohaline: A line of constant salinity (saltiness in the ocean) ...

Station models are an efficient and concise way to represent weather conditions ... Isohaline: A line of constant salinity (saltiness in the ocean) ...

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Southern Ocean Variability - Southern Ocean Variability

Southern Ocean Variability

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VARIATIONAL DATA ASSIMILATION E'G' FOR ATMOSPHERIC MODELLING PowerPoint PPT Presentation

VARIATIONAL DATA ASSIMILATION E'G' FOR ATMOSPHERIC MODELLING - The matrix of second derivatives J''=2B-1 2HTR-1H is called the Hessian of J ... i.e. cost is mainly sensitive to the conditioning = ellipticity of the Hessian. ...

The matrix of second derivatives J''=2B-1 2HTR-1H is called the Hessian of J ... i.e. cost is mainly sensitive to the conditioning = ellipticity of the Hessian. ...

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Intro to Marine Resources Geography 158 PowerPoint PPT Presentation

Intro to Marine Resources Geography 158 - Intro to Marine Resources Geography 158. Professor David Siegel ... Canary rockfish. Stock assessments. Many rockfish stocks are now been. declared overfished ...

Intro to Marine Resources Geography 158. Professor David Siegel ... Canary rockfish. Stock assessments. Many rockfish stocks are now been. declared overfished ...

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The role of vorticity fluxes in the dynamics of the Zapiola Anticyclone PowerPoint PPT Presentation

The role of vorticity fluxes in the dynamics of the Zapiola Anticyclone - Denis Volkov and Lee-Lueng Fu. NASA Jet Propulsion Laboratory, California Institute of Technology ... Corresponding author: Denis Volkov, dvolkov@caltech.edu, ...

Denis Volkov and Lee-Lueng Fu. NASA Jet Propulsion Laboratory, California Institute of Technology ... Corresponding author: Denis Volkov, dvolkov@caltech.edu, ...

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Matlab Programming PowerPoint PPT Presentation

Matlab Programming - Computers can only do a few stupid things, but ... tot=tot u(j)*v(j); end. Conditionals. Conditional statements control flow of a program ...

Computers can only do a few stupid things, but ... tot=tot u(j)*v(j); end. Conditionals. Conditional statements control flow of a program ...

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Regional Coastal Ocean Modeling: Tutorial PowerPoint PPT Presentation

Regional Coastal Ocean Modeling: Tutorial - Data: bathymetry, hydrography, surface fluxes global climatological datasets are ... the nonlinear equation of state in a adiabatic part and a compressible part. ...

Data: bathymetry, hydrography, surface fluxes global climatological datasets are ... the nonlinear equation of state in a adiabatic part and a compressible part. ...

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ESM 203: Ocean Processes and Circulation PowerPoint PPT Presentation

ESM 203: Ocean Processes and Circulation - Dissolved salts, gases and organic substances, as well as particles. Physical properties are mainly ... Awarded Nobel Peace Prize in 1922. 25. Ekman transport ...

Dissolved salts, gases and organic substances, as well as particles. Physical properties are mainly ... Awarded Nobel Peace Prize in 1922. 25. Ekman transport ...

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Intrinsic Errors in Physical Ocean Climate Models PowerPoint PPT Presentation

Intrinsic Errors in Physical Ocean Climate Models - high resolution: 0.1 deg (~10 km) short duration: 10's of years ... case for importance of transport scheme at high resolution. Horizontal grid discretization ...

high resolution: 0.1 deg (~10 km) short duration: 10's of years ... case for importance of transport scheme at high resolution. Horizontal grid discretization ...

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South American Climate of the LGM: A regional modeling study PowerPoint PPT Presentation

South American Climate of the LGM: A regional modeling study - South American Climate of the LGM: A Regional Modeling Study Kerry H. Cook Department of Earth and Atmospheric Sciences Cornell University Thanks to Edward Vizy and ...

South American Climate of the LGM: A Regional Modeling Study Kerry H. Cook Department of Earth and Atmospheric Sciences Cornell University Thanks to Edward Vizy and ...

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Laboratory in Oceanography: Data and Methods PowerPoint PPT Presentation

Laboratory in Oceanography: Data and Methods - Assumed field is homogeneous and isotropic. ... Estimated field based on observations and correlation matrix (assumes the ... Anisotropy ...

Assumed field is homogeneous and isotropic. ... Estimated field based on observations and correlation matrix (assumes the ... Anisotropy ...

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A variational data assimilation system for the global ocean PowerPoint PPT Presentation

A variational data assimilation system for the global ocean - A variational data assimilation system for the global ocean ... Global (ORCA): 2o x 0.5o at eq., 31 levels (free surface) Variational assimilation environment ...

A variational data assimilation system for the global ocean ... Global (ORCA): 2o x 0.5o at eq., 31 levels (free surface) Variational assimilation environment ...

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SELFE Users Trainng Course 1 SELFE physical formulation Joseph Zhang, CMOP, OHSU PowerPoint PPT Presentation

SELFE Users Trainng Course 1 SELFE physical formulation Joseph Zhang, CMOP, OHSU - Inertial oscillation: no external forces, advection and vertical vel. ... apply wind-stress on surface (influences advection, location of density fronts) ...

Inertial oscillation: no external forces, advection and vertical vel. ... apply wind-stress on surface (influences advection, location of density fronts) ...

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Physical Oceanography An Introduction PowerPoint PPT Presentation

Physical Oceanography An Introduction - This book is concerned primarily with one of these applications, which is the ... sailed across the Atlantic to Madeira, recrossed to Rio de Janeiro, then ...

This book is concerned primarily with one of these applications, which is the ... sailed across the Atlantic to Madeira, recrossed to Rio de Janeiro, then ...

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Kein Folientitel - Kein Folientitel

Kein Folientitel

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An International Collaborative Effort Towards Automated Sea Ice Chart Production PowerPoint PPT Presentation

An International Collaborative Effort Towards Automated Sea Ice Chart Production - An International Collaborative Effort Towards Automated Sea ... information exchange - joint research (project based) - operational model and/or data exchange ...

An International Collaborative Effort Towards Automated Sea ... information exchange - joint research (project based) - operational model and/or data exchange ...

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Relationships between Convectively Coupled Kelvin Waves and Extratropical Wave Activity - Relationships between Convectively Coupled Kelvin Waves and Extratropical Wave Activity

Relationships between Convectively Coupled Kelvin Waves and Extratropical Wave Activity

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MERCATOR Data Assimilation Systems: From a Simple Altimeter Data Reduced Order Optimal System' Inter PowerPoint PPT Presentation

MERCATOR Data Assimilation Systems: From a Simple Altimeter Data Reduced Order Optimal System' Inter - MERCATOR Data Assimilation Systems: From a Simple Altimeter Data Reduced Order Optimal System. ... MERCATOR Assimilation System Altimeter Sea Level Anomalies ...

MERCATOR Data Assimilation Systems: From a Simple Altimeter Data Reduced Order Optimal System. ... MERCATOR Assimilation System Altimeter Sea Level Anomalies ...

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Geostrophy PowerPoint PPT Presentations