Regional Advanced School on Physical and Mathematical Tools for the study of Marine Processes of Coastal Areas Physical and Biogeochemical Coupled Modelling.

Slides:



Advertisements
Similar presentations
Hydrodynamics and Sediment Transport Modelling Ramiro Neves
Advertisements

Development and validation of a Benthic Flux Model for the Adriatic Sea Presenter: F. Zaffagnini Zaffagnini F. 1, Vichi.
Geographical Information System & Modelling LIFE02/ENV/P/
Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009 Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009.
JSSBIO1Huttula Lecture Set Sediment transport models.
The ChesROMS Community Model
How do geotechnical properties contribute to failures and resulting fluxes to the deep sea? Subsurface flows and impacts on chemical fluxes, geotechnics,
About Estuarine Dynamics
AMCE6081 General Description Physical and biological processes are inter-related aspects that govern the productivity of marine ecosystems. Provides an.
The effect of food composition on feeding, growth and reproduction of bivalves Sofia SARAIVA 1,3, Jaap VAN DER MEER 1,2, S.A.L.M. KOOIJMAN 2, T. SOUSA.
COLLABORATORS: P. Estrade, S. Herbette, C. Lett, A. Peliz, C. Roy, B. Sow, C. Roy EDDY-DRIVEN DISPERSION IN COASTAL UPWELLING SYSTEMS California Canary.
Institute of Oceanogphy Gdańsk University Jan Jędrasik The Hydrodynamic Model of the Southern Baltic Sea.
Juan Carlos Ortiz Royero Ph.D.
Suspended Load Above certain critical shear stress conditions, sediment particles are maintained in suspension by the exchange of momentum from the fluid.
The Physical Modulation of Seasonal Hypoxia in Chesapeake Bay Malcolm Scully Outline: 1)Background and Motivation 2)Role of Physical Forcing 3)Simplified.
A T HREE- D IMENSIONAL W ATER Q UALITY M ODEL OF S OUTHERN P UGET S OUND Greg Pelletier, P.E., Mindy Roberts, P.E., Skip Albertson, P.E., and Jan Newton,
MAMA Malta meeting, January 2004 Expert Meeting Towards Operational ecological models in coastal areas
Simple coupled physical-biogeochemical models of marine ecosystems
Courtney K. Harris Virginia Institute of Marine Sciences In collaboration with Katja Fennel and Robin Wilson (Dalhousie), Rob Hetland (TAMU), Kevin Xu.
Biogeochemical Controls and Feedbacks on the Ocean Primary Production.
The modeling of the channel deformations in the rivers flowing into permafrost with an increase in ambient temperature E. Debolskaya, E. Zamjatina, I.Gritsuk.
Iron and Biogeochemical Cycles
SIMPLE COUPLED PHYSICAL-BIOGEOCHEMICAL MODELS OF MARINE ECOSYSTEMS.
Inga Hense & Hans Burchard What is GOTM ? GOTM is a Public Domain water column model with a library of state-of-the-art turbulence closure models GOTM.
High-resolution 3D modelling of oceanic fine structures using vertically adaptive coordinates Hans Burchard 1, Ulf Gräwe 1, Richard Hofmeister 2, Peter.
Rho-Taek Jung Date Title 2 June MEC Ocean Model Introduction, Hydrostatic Model, Full-3D Model, Eddy Viscosity, Boundary Condition 9 June Exercise1: MEC.
4. Atmospheric chemical transport models 4.1 Introduction 4.2 Box model 4.3 Three dimensional atmospheric chemical transport model.
The Governing Equations The hydrodynamic model adopted here is the one based on the hydrostatic pressure approximation and the boussinesq approximation,
1 CORIE circulation modeling system Simulation databases Daily forecasts Codes: SELFE, ELCIRC 3D baroclinic Unstructured grids.
Mediterranean Sea Basin Scale model P.Lazzari, S. Salon, A. Teruzzi, K.Beranger, A. Crise Sesame WP3 meeting Villefranche sur Mer, Februay 2008 OGS,
First results from the isopycnic ocean carbon cycle model HAMOCC & MICOM/BCM Karen Assmann, Christoph Heinze, Mats Bentsen, Helge Drange Bjerknes Centre.
11/03/2014PHY 711 Fall Lecture 291 PHY 711 Classical Mechanics and Mathematical Methods 10-10:50 AM MWF Olin 103 Plan for Lecture 29: Chap. 9 of.
General Description of coastal hydrodynamic model.
J.M. Abril Department of Applied Physics (I); University of Seville (Spain) IAEA Regional Training Course on Sediment Core Dating Techniques. RAF7/008.
International Workshop for GODAR WESTPAC Global Ocean Data Archeology and Rescue: Scientific Needs from the Carbon Cycle Study in the Ocean Toshiro Saino.
Regional Advanced School on Physical and Mathematical Tools for the study of Marine Processes of Coastal Areas A new Mechanistic Modular Ecological Model:
WLRD Science Seminar Sammamish River Water Quality Model Status Report November 19, 2002.
Modelling 2: Introduction to modelling assignment. A basic physical-biological model. Model equations. Model operation. The assignment.
Marine Ecosystem Simulations in the Community Climate System Model
An Overview of Biogeochemical Modeling in ROMS
CHANGSHENG CHEN, HEDONG LIU, And ROBERT C. BEARDSLEY
Primary production and the carbonate system in the Mediterranean Sea
Regional Advanced School on Physical and Mathematical Tools for the study of Marine Processes of Coastal Areas Physical and Biogeochemical Coupled Modelling.
Biogeochemical Controls and Feedbacks on the Ocean Primary Production
1 Foundations of circulation modeling systems EBS566: Estuary and Ocean Systems II – Lecture 3, Winter 2010 Instructors: T. Peterson, M. Haygood, A. Baptista.
OEAS 604: Final Exam Tuesday, 8 December 8:30 – 11:30 pm Room 3200, Research Innovation Building I Exam is cumulative Questions similar to quizzes with.
Jeopardy Vocab Marine Zones Threats Marine Org. Misc Q $100 Q $200 Q $300 Q $400 Q $500 Q $100 Q $200 Q $300 Q $400 Q $500 Final Jeopardy.
Conservation of Tracers (Salt, Temperature) Chapter 4 – Knauss Chapter 5 – Talley et al.
Ecosystem Modeling II Kate Hedstrom, ARSC November 2006 With help from Sarah Hinckley, Katja Fennel, Georgina Gibson, and Hal Batchelder.
Coastal Ocean Circulation and biogeochemical modeling
Modeling phytoplankton seasonal variation and nutrients budget of a Semi-Arid region ecosystem in the Southern Mediterranean Sea: -Case of the Bizerte.
Modelling of Marine Systems. Shallow waters Equations.
Simple coupled physical-biogeochemical models of marine ecosystems
Hypoxia Forecasts as a Tool for Chesapeake Bay Fisheries
11:628:320 Dynamics of Marine Ecosystems 2015
Enhancement of Wind Stress and Hurricane Waves Simulation
FlexSim 3D Ecological modelling made user friendly
Simple coupled physical-biogeochemical models of marine ecosystems
14 – University of Venice ECASA modelling workshop,
Elizabeth River PCB TMDL Study: Numerical Modeling Approach
Estuarine models: what is under the hood?
Continuity Equation.
James River PCB TMDL Study: Numerical Modeling Approach
Iron and Biogeochemical Cycles
Simple coupled physical-biogeochemical models of marine ecosystems
Lecture 1: Introduction
Convective Heat Transfer
PHY 711 Classical Mechanics and Mathematical Methods
  Robin Robertson Lamont-Doherty Earth Observatory
Radionuclide transport modelling
Presentation transcript:

Regional Advanced School on Physical and Mathematical Tools for the study of Marine Processes of Coastal Areas Physical and Biogeochemical Coupled Modelling Presented by Christel PINAZO Mediterranean University Oceanographic Center of Marseille Physical & Biogeochemical Oceanographic Laboratory

Introduction Why use Coupled Models ? Historical considerations Different types of Coupled Models Box models Fine grid Models (1D, 2D and 3D) Different ways of Coupling Models « Off-line » Coupling « On-line » Coupling Examples LECTURE SCHEDULE

Introduction Why use Coupled Models ? Historical considerations Different types of Coupled Models Box models Fine grid Models (1D, 2D and 3D) Different ways of Coupling Models « Off-line » Coupling « On-line » Coupling Examples LECTURE SCHEDULE

INTRODUCTION WHY USE PHYSICAL AND BIOGEOCHEMICAL COUPLED MODELS TO STUDY ECOSYSTEM FUNCTIONING? Regional Advanced School on Physical and Mathematical Tools for the study of Marine Processes of Coastal Areas INTRODUCTION > WHY?COUPLING TYPESCOUPLING WAYS EXAMPLES

INTRODUCTION A BIOGEOCHEMICAL MODEL TO DESCRIBE ECOSYSTEM FUNCTIONING Regional Advanced School on Physical and Mathematical Tools for the study of Marine Processes of Coastal Areas INTRODUCTION > WHY?COUPLING TYPESCOUPLING WAYS EXAMPLES

Sediment River Inputs Schematic Marine Ecosystem IRRADIANCE Nutrients POM DOM Erosion Benthic Fluxes Phytoplankton Uptake Exudation Zooplankton Grazing Faeces Bacteria Mineralisation Uptake GEOCHEMICAL MODEL Atmospheric inputs T° BIOGEOCHEMICAL MODEL

INTRODUCTION A PHYSICAL MODEL TO DESCRIBE ECOSYSTEM FORCING CONDITIONS Regional Advanced School on Physical and Mathematical Tools for the study of Marine Processes of Coastal Areas INTRODUCTION > WHY?COUPLING TYPESCOUPLING WAYS EXAMPLES

Sediment Schematic Marine Ecosystem IRRADIANCE Nutrients POM DOM Erosion Benthic Fluxes Phytoplankton Zooplankton Bacteria PHYSICAL MODEL River Inputs Atmospheric inputs Tide WIND Waves Currents T°

INTRODUCTION A PHYSICAL AND BIOGEOCHEMICAL COUPLED MODEL IS NEEDED TO DESCRIBE BOTH ECOSYSTEM FUNCTIONING AND FORCING CONDITIONS Regional Advanced School on Physical and Mathematical Tools for the study of Marine Processes of Coastal Areas INTRODUCTION > WHY?COUPLING TYPESCOUPLING WAYS EXAMPLES

Introduction Why use Coupled Models ? Historical considerations Different types of Coupled Models Box models Fine grid Models (1D, 2D and 3D) Different ways of Coupling Models « Off-line » Coupling « On-line » Coupling Examples LECTURE SCHEDULE

INTRODUCTION Physical and Biogeochemical Coupled Modelling is a Recent Scientific Discipline Developed since the 1990’s Regional Advanced School on Physical and Mathematical Tools for the study of Marine Processes of Coastal Areas INTRODUCTION > HISTORY COUPLING TYPES COUPLING WAYS EXAMPLES

BECAUSE Biogeochemical Modelling was Developed since the 1940’s with Riley’s (1946) and Steele’s (1962) Models INTRODUCTION Regional Advanced School on Physical and Mathematical Tools for the study of Marine Processes of Coastal Areas INTRODUCTION > HISTORY COUPLING TYPES COUPLING WAYS EXAMPLES 1

PHYTOPLANKTON MODELS Riley’s Model (1946) Regional Advanced School on Physical and Mathematical Tools for the study of Marine Processes of Coastal Areas INTRODUCTION > HISTORY COUPLING TYPES COUPLING WAYS EXAMPLES From Tett & Wilson (2000) Phytoplankton Carbon Concentration Phytoplankton Carbon Concentration Photosynthesis Respiration Grazing Photosynthesis depending on light limitation Steele’s Model (1962)

N-P-Z-D MODELS Fasham’s Model (1990) Regional Advanced School on Physical and Mathematical Tools for the study of Marine Processes of Coastal Areas INTRODUCTION > HISTORY COUPLING TYPES COUPLING WAYS EXAMPLES Nutrient-Phytoplankton-Zooplankton-Detritus PhytoplanktonDONNitrate Ammonium BacteriaZooplanktonDetritus

INTRODUCTION & BECAUSE Hydrodynamical Modelling was Developed since the 1970’s with the development of computers and computing resources Regional Advanced School on Physical and Mathematical Tools for the study of Marine Processes of Coastal Areas INTRODUCTION > HISTORY COUPLING TYPES COUPLING WAYS EXAMPLES 2

INTRODUCTION POM was created by Blumberg in late 1970’s Blumberg & Yamada (1974) Blumberg & Mellor (1980)

INTRODUCTION THUS First coupled Models appeared in the 1980’s Cloern & Cheng (1981) 1DH (Phytopk) Klein & Coste (1984) 1DV (Nutrients) Klein & Steele (1985) 1DV (N-P) Regional Advanced School on Physical and Mathematical Tools for the study of Marine Processes of Coastal Areas INTRODUCTION > HISTORY COUPLING TYPES COUPLING WAYS EXAMPLES 3

INTRODUCTION First 3D coupled Models appeared in the 1990’s Regional Advanced School on Physical and Mathematical Tools for the study of Marine Processes of Coastal Areas INTRODUCTION > HISTORY COUPLING TYPES COUPLING WAYS EXAMPLES Sarmiento et al. (1993) (Fasham’s model) Buckley and O’Kane (1993) (GHER model) Skogen et al. (1995) (NORWECOM model) Six and Maier-Reimer (1996) (HAMOCC model) Pinazo et al. (1996) (ECO3M model)

Introduction Why use Coupled Models ? Historical considerations Different types of Coupled Models Box models Fine grid Models (1D, 2D and 3D) Different ways of Coupling Models « Off-line » Coupling « On-line » Coupling Examples LECTURE SCHEDULE

Regional Advanced School on Physical and Mathematical Tools for the study of Marine Processes of Coastal Areas INTRODUCTION COUPLING TYPES COUPLING WAYS EXAMPLES COUPLING OR FORCING? THAT IS THE QUESTION! Ecological Model Hydrodynamic Model FORCING FEED BACK NO FORCING

Introduction Why use Coupled Models ? Historical considerations Different types of Coupled Models Box models Fine grid Models (1D, 2D and 3D) Different ways of Coupling Models « Off-line » Coupling « On-line » Coupling Examples LECTURE SCHEDULE

COUPLING TYPES Regional Advanced School on Physical and Mathematical Tools for the study of Marine Processes of Coastal Areas INTRODUCTIONCOUPLING TYPES>BOX COUPLING WAYS EXAMPLES THE STUDY SITE COULD BE SPATIALLY DESCRIBED BY BOXES

SEDIMENT z=-h BOX MODEL Regional Advanced School on Physical and Mathematical Tools for the study of Marine Processes of Coastal Areas INTRODUCTIONCOUPLING TYPES>BOX COUPLING WAYS EXAMPLES VERTICALLY HOMOGENEOUS O x y z z=0  Velocity =

CONSERVATION LAWS Regional Advanced School on Physical and Mathematical Tools for the study of Marine Processes of Coastal Areas INTRODUCTIONCOUPLING TYPES>BOX COUPLING WAYS EXAMPLES TO CALCULATE ADVECTION OF BIOGEOCHEMICAL SUBSTANCES : - FLUID MASS CONSERVATION = CONTINUITY EQUATION - SUBSTANCE MASS CONSERVATION

CONSERVATION LAWS Regional Advanced School on Physical and Mathematical Tools for the study of Marine Processes of Coastal Areas INTRODUCTIONCOUPLING TYPES>BOX COUPLING WAYS EXAMPLES FLUID MASS CONSERVATION = CONTINUITY EQUATION In case of incompressible fluids Density is constant

SEDIMENT z=-h BOX MODEL Regional Advanced School on Physical and Mathematical Tools for the study of Marine Processes of Coastal Areas INTRODUCTIONCOUPLING TYPES>BOX COUPLING WAYS EXAMPLES O x y z z=0  Along Ox axis

SEDIMENT z=-h BOX MODEL Regional Advanced School on Physical and Mathematical Tools for the study of Marine Processes of Coastal Areas INTRODUCTIONCOUPLING TYPES>BOX COUPLING WAYS EXAMPLES O x y z z=0  Along Ox axis

CONSERVATION LAWS Regional Advanced School on Physical and Mathematical Tools for the study of Marine Processes of Coastal Areas INTRODUCTIONCOUPLING TYPES>BOX COUPLING WAYS EXAMPLES FLUID MASS CONSERVATION = CONTINUITY EQUATION In case of incompressible fluids is constant Boundary conditions along Oz axis:

CONSERVATION LAWS Regional Advanced School on Physical and Mathematical Tools for the study of Marine Processes of Coastal Areas INTRODUCTIONCOUPLING TYPES>BOX COUPLING WAYS EXAMPLES FLUID MASS CONSERVATION = CONTINUITY EQUATION In case of incompressible fluids is constant

CONSERVATION LAWS Regional Advanced School on Physical and Mathematical Tools for the study of Marine Processes of Coastal Areas INTRODUCTIONCOUPLING TYPES>BOX COUPLING WAYS EXAMPLES SUBSTANCE MASS CONSERVATION = STATE EQUATION C is the concentration of the substance

SEDIMENT z=-h BOX MODEL Regional Advanced School on Physical and Mathematical Tools for the study of Marine Processes of Coastal Areas INTRODUCTIONCOUPLING TYPES>BOX COUPLING WAYS EXAMPLES O x y z z=0  Along Ox axis zz yy

CONSERVATION LAWS Regional Advanced School on Physical and Mathematical Tools for the study of Marine Processes of Coastal Areas INTRODUCTIONCOUPLING TYPES>BOX COUPLING WAYS EXAMPLES SUBSTANCE MASS CONSERVATION = STATE EQUATION C is the concentration of the substance withAnd at the surface at the bottom

Regional Advanced School on Physical and Mathematical Tools for the study of Marine Processes of Coastal Areas INTRODUCTIONCOUPLING TYPES>BOX COUPLING WAYS EXAMPLES If C is the concentration of a biologic substance, C is not conservative BOX MODEL Concentration Trend term= Sources – Sinks

COUPLING TYPES Regional Advanced School on Physical and Mathematical Tools for the study of Marine Processes of Coastal Areas ADVANTAGES: -SHORT COMPUTATIONAL TIME -VERY LONG SIMULATION OF YEARS OR DECADES DISADVANTAGES: -MAINLY ADVECTIVE TRANSPORT: Paul Tett TRIED TO ADD VERTICAL EDDY DIFFUSIVITY THROUGH 3 VERTICAL LAYERS -ROUGH SPATIAL DESCRIPTION -NUMERICAL HORIZONTAL DIFFUSIVITY INTRODUCTIONCOUPLING TYPES>BOX COUPLING WAYS EXAMPLES BOX MODEL