Hidrodinámica Estuarina

Slides:



Advertisements
Similar presentations
Flow Over Notches and Weirs
Advertisements

About Estuarine Dynamics
MAST602: Advection, transports, budgets Flux, transport Radiation, Advection, Diffusion Conservation of volume Continuity Conservation of salt Freshwater.
Dr. Martin T. Auer MTU Department of Civil & Environmental Engineering CE5504 Surface Water Quality Modeling Lab 6. Coastal Zone Modeling: The Lake Ontario.
Convection in a planetary body Geosciences 519 Natalie D. Murray April 2, 2002.
The Islamic University of Gaza Faculty of Engineering Civil Engineering Department Numerical Analysis ECIV 3306 Chapter 1 Mathematical Modeling.
Flow and Thermal Considerations
Analysis of Disturbance P M V Subbarao Associate Professor Mechanical Engineering Department I I T Delhi Modeling of A Quasi-static Process in A Medium.
Hans Burchard 1,2, Joanna Staneva 3, Götz Flöser 4, Rolf Riethmüller 4, and Thomas Badewien 5 1. Baltic Sea Research Institute Warnemünde, Germany 2. Bolding.
Modelling 1: Basic Introduction. What constitutes a “model”? Why do we use models? Calibration and validation. The basic concept of numerical integration.
Sundermeyer MAR 550 Spring Laboratory in Oceanography: Data and Methods MAR550, Spring 2013 Miles A. Sundermeyer Observations vs. Models.
Modelling & Simulation of Chemical Engineering Systems Department of Chemical Engineering King Saud University 501 هعم : تمثيل الأنظمة الهندسية على الحاسب.
Typical Mean Dynamic Balances in Estuaries Along-Estuary Component 1. Barotropic pressure gradient vs. friction Steady state, linear motion, no rotation,
Coastal Ocean Dynamics Baltic Sea Research Warnemünde
An example of vertical profiles of temperature, salinity and density.
CEE 262A H YDRODYNAMICS Lecture 7 Conservation Laws Part III.
Fluid Flow Continuity and Bernoulli’s Equation
Richard Rotunno National Center for Atmospheric Research, USA Dynamical Mesoscale Mountain Meteorology.
Land-Ocean Interactions: Estuarine Circulation. Estuary: a semi-enclosed coastal body of water which has a free connection with the open sea and within.
12.808, Problem 1, problem set #2 This is a 3 part question dealing with the wind-driven circulation. At 26 o N in the N. Atlantic, the average wind stress.
Flux of mass in (kg/s) = Flux of mass out (kg/s) = Net Flux of mass in ‘x’ = Net Flux of mass in ‘y’ = Net Flux of mass in ‘z’ =, u, w, v Mass per volume.
MAE 5360: Hypersonic Airbreathing Engines
INTRODUCTION TO CONVECTION
Coastal Waters and Marginal Seas
Hans Burchard 1,2, Joanna Staneva 3, Götz Flöser 4, Rolf Riethmüller 4, Thomas Badewien 5, and Richard Hofmeister 1 1. Baltic Sea Research Institute Warnemünde,
 p and  surfaces are parallel =>  =  (p) Given a barotropic and hydrostatic conditions, is geostrophic current. For a barotropic flow, we have and.
1 Foundations of circulation modeling systems EBS566: Estuary and Ocean Systems II – Lecture 3, Winter 2010 Instructors: T. Peterson, M. Haygood, A. Baptista.
Flux of mass in (kg/s) = Flux of mass out (kg/s) = Net Flux of mass in ‘x’ = Net Flux of mass in ‘y’ = Net Flux of mass in ‘z’ =, u, w, v Mass per volume.
Estuaries Chapter 8 – Talley et al. Outline: What is an estuary?
1. Integral vs Differential Approach
Conservation of Tracers (Salt, Temperature) Chapter 4 – Knauss Chapter 5 – Talley et al.
1.Fundamental equations and concepts 2.Balanced flow and vortex motion 3.Waves 4.Instabilities 5.Nonlinear phenomena An Introduction to Geophysical Fluid.
OEAS 604: Introduction to Physical Oceanography Conservation of Mass Chapter 4 – Knauss Chapter 5 – Talley et al. 1.
15 Annual AOMIP Meeting. WHOI, 1- 4 November 2011 Numerical modeling of the Atlantic Water distribution in the upper Arctic Ocean: Sensitivity studies.
Typical Mean Dynamic Balances in Estuaries Along-Estuary Component 1. Barotropic pressure gradient vs. friction Steady state, linear motion, no rotation,
Chapter 1. Essential Concepts
© 2014 Pearson Education, Inc. Chapter 11 The Coastal Ocean Types of Coastal Waters.
Estuarine Hydrodynamics
Modelling of Marine Systems. Shallow waters Equations.
Surface LH, SH, and momentum drag are determined by turbulent transport near the surface.
For a barotropic flow, we have is geostrophic current.
The Chesapeake Bay Estuary
Estuarine Variability
Water, salt, and heat budget
Flushing Time or Turnover Time
Review of conservation equations State, Mass and Momentum
GLOBAL CONSERVATION EQUATIONS
Land-Ocean Interactions: Estuarine Circulation
Design of Passive (Adiabatic) Control Volumes
For a barotropic flow, we have is geostrophic current.
Diffusion Mass Transfer
t is obtained in seconds [ m3 / m3/s]
Estuarine models: what is under the hood?
MATH 3331—Ordinary Differential Equations
Integrated Science Glencoe Chapter 4
What is an estuary? Estuaries Coastal lagoons
s s Wind-induced circulation
s s Wind-induced circulation
Modeling Algorithm Draw a picture Schematic
Density Lab Pre-Questions
Today’s Lecture Objectives:
하구및 연안생태Coastal management
MAE 3241: AERODYNAMICS AND FLIGHT MECHANICS
Laboratory in Oceanography: Data and Methods
COMBUSTION TA : Donggi Lee PROF. SEUNG WOOK BAEK
Ocean Water & Ocean Life
하구및 연안생태Coastal management
하구및 연안생태Coastal management
하구및 연안생태Coastal management
하구및 연안생태Coastal management
Presentation transcript:

Hidrodinámica Estuarina Arnoldo Valle-Levinson University of Florida Civil and Coastal Engineering Department Gainesville, Florida

What is an estuary? Estuaries Coastal lagoons Semi-enclosed coastal body of water free communication with ocean ocean salinity is measurably diluted by runoff

Typical Estuarine Circulation

Review of conservation equations Mass and Momentum

Boussinesq approximation This is the Continuity Equation or Equation of Conservation of Mass

z x Continuity Equation in Bulk Form:

Advection-Diffusion Equation Conservation of Salt: At steady state and assuming constant diffusivities: Advection-Diffusion Equation Further assuming motion in one direction and integrated over the volume considered, the statement of CONSERVATION OF SALT may be given as: Vin Sin = Vout Sout

z Sb S0 x Continuity Equation in Bulk Form: Salt Conservation Equation in Bulk Form: VbSb = V0S0

Conservation of Salt: Conservation of Heat: Equation of State:

Conservation of Momentum (Equations of Motion)