A Shared Atmosphere-Ocean Dynamical Core: First Validation (Semi-Implicit Semi-Lagrangian) Pierre Pellerin(2), François Roy(1,3), Claude Girard(2), François.

Slides:



Advertisements
Similar presentations
$1 Million $500,000 $250,000 $125,000 $64,000 $32,000 $16,000 $8,000 $4,000 $2,000 $1,000 $500 $300 $200 $100 Bienvenue.
Advertisements

Page 1 Pierre Pellerin and several collaborators Recherche en Prévision Numérique (RPN) Meteorological Research Division, Science and Technology Branch.
1 Water vapour self-continuum: Recent update from Reading/RAL Semi-annual CAVIAR meeting UCL, London Igor Ptashnik, Keith Shine, Andrey Vigasin.
LE MOMENT. Calcul des moments LE MOMENT Calcul des moments.
1 Improvements of regional emissions for air quality modelling Proposed in Eastern Canada Regional Border strategy by NEG/ECP Environment committee G.
1 APPLICATION DE LA MÉTHODE DE MAILLAGES DYNAMIQUES POUR LA PRÉDICTION DÉCOULEMENTS AUTOUR DUN PROFIL DAILE OSCILLANT DANS LE CONTEXTE DE LINTERACTION.
Nombres de solutions d’une équation. 1.Résoudre graphiquement : a. f (x) = –3 b. f (x) = –5 c. f (x) = 0 d. f (x) = 3.
Page 1 Hal Ritchie and many collaborators Recherche en Prévision Numérique (RPN) Meteorological Research Division, Science and Technology Branch Expert.
Simulation of Fluids using the Navier-Stokes Equations Kartik Ramakrishnan.
University of Southampton Southampton, UK
Flow Disturbance of Flow due to Bends and Obstacles, etc. Time Transients and Spatial Distribution of Fluid Force on Structure Surface FLAVOR-3D: 3-D Fluid.
SIMBAR Oil Spill Boom and Contingency Plan Modelling Objectives Optimal usages of booming in practice Partners –EIGSI Engineering School La Rochelle, Project.
Proposal for ½ MW photo-fission driver based on TESLA 1.3 GHz SCRF technology (Shane Koscielniak, 09 Nov 2007) Electron Linac CANADA ’ S NATIONAL LABORATORY.
Modeling lamps using commercial packages ROUFFET Jean-Baptiste CPAT – Université de Toulouse, France COST – Model Inventory Workshop, Funchal, April 2005.
(c) MSc Module MTMW14 : Numerical modelling of atmospheres and oceans Staggered schemes 3.1 Staggered time schemes.
1 National Institute for Earth Sciences and Astronomy (INSU) Institut National des Sciences de l’Univers 3, rue Michel Ange – Paris Cedex.
Effect of Pressure Gradient on the flow in a Boundary Layer Pressure gradient is found from freestream (external) velocity field Boundary layer equation:
Numerical Study of Island Wake in Deep Water Changming (Charles) Dong James McWilliams Alexander Shchepetkin IGPP/UCLA, Los Angels,USA Acknowledgements:
Innovation in Research and Knowledge Exchange Clémence Dallaire, RN, full professor Faculté des sciences infirmières Université Laval.
Adnan Khan Department of Mathematics Lahore University of Management Sciences.
Combined Lagrangian-Eulerian Approach for Accurate Advection Toshiya HACHISUKA The University of Tokyo Introduction Grid-based fluid.
Lagrangian dispersion of light solid particle in a high Re number turbulence; LES with stochastic process at sub-grid scales CNRS – UNIVERSITE et INSA.
Experimenting with the LETKF in a dispersion model coupled with the Lorenz 96 model Author: Félix Carrasco, PhD Student at University of Buenos Aires,
Separated Flows Wakes and Cavities Olivier Cadot, Equipe Dynamique des Fluides et Acoustique de l’Unité de Mécanique, ENSTA, Palaiseau. Overview Short.
1 st UNSTABLE Science Workshop April 2007 Science Question 3: Science Question 3: Numerical Weather Prediction Aspects of Forecasting Alberta Thunderstorms.
Modelling Realistic Water & Fire Sérgio Leal Socrates/Erasmus student at: AK Computer Graphics Institute for Computer Graphics and Vision Technical University.
Partially Resolved Numerical Simulation CRTI RD Project Review Meeting Canadian Meteorological Centre August 22-23, 2006.
The Canadian Numerical Weather Prediction System: Present and Future Gilbert Brunet Recherche en Prévision Numérique (RPN) Meteorological Research Branch.
Solution of the Implicit Formulation of High Order Diffusion for the Canadian Atmospheric GEM Model “High Performance Computing and Simulation Symposium.
Solutions stationnaires des équations de Navier-Stokes en domaines extérieurs dans le régime des faibles nombres de Reynolds Peter Wittwer Département.
Environment Canada Meteorological Service of Canada Environnement Canada Service météorologique du Canada Modeling Volcanic Ash Transport and Dispersion:
( ) A. Mangeney 1,3, O. Roche 2, L. Tsimring 3, F. Bouchut 4, O. Hungr 5, I. Ionescu 6, N. Mangold 7 1 Equipe de Sismologie, Institut de Physique du Globe.
© 2011 Autodesk Freely licensed for use by educational institutions. Reuse and changes require a note indicating that content has been modified from the.
(c) MSc Module MTMW14 : Numerical modelling of atmospheres and oceans Week 5: Lecture Plan 5.1 Revision class 5.2 Test.
Comparison of convective boundary layer velocity spectra calculated from large eddy simulation and WRF model data Jeremy A. Gibbs and Evgeni Fedorovich.
A cell-integrated semi-Lagrangian dynamical scheme based on a step-function representation Eigil Kaas, Bennert Machenhauer and Peter Hjort Lauritzen Danish.
Owned and operated as a joint venture by a consortium of Canadian universities via a contribution through the National Research Council Canada Propriété.
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss High resolution COSMO runs for dispersion applications.
Irregular plurals. To make nouns plural, you add an “s” just like English. You will change the article also. Indefinite articles will change from un and.
IIT-Madras, Momentum Transfer: July 2005-Dec 2005 Perturbation: Background n Algebraic n Differential Equations.
DIRECTION RECHERCHE & INNOVATION Centre de Recherche et Innovation Gaz et Energies Nouvelles Guillain Chapelon 12 september 2013.
© IFP Controlled CO 2 | Diversified fuels | Fuel-efficient vehicles | Clean refining | Extended reserves Écrire ici dans le masque le nom de votre Direction.
Convection dans les coquilles sphériques et circulation des planètes géantes Convection in spherical shells and general circulation of giant planets Pierre.
The structure of turbulence in a shallow water wind-driven shear current with Langmuir circulation Andrés E. Tejada-Martínez and Chester E. Grosch Center.
By Dirk Hekhuis Advisors Dr. Greg Wolffe Dr. Christian Trefftz.
Analysis of Lagrangian Coherent Structures of the Chesapeake Bay Stephanie Young, Kayo Ide,
Stephanie Young, Kayo Ide, Atmospheric and Oceanic Science Department
P. Meunier M. Bosco, P-Y Passaggia, S. Le Dizès Institut de Recherche sur les Phénomènes Hors-Equilibre, Marseille, France Lee waves of a tilted object.
Multigrid Methods The Implementation Wei E Universität München. Ferien Akademie 19 th Sep
November 2005 Center for Computational Visualization Institute of Computational and Engineering Sciences Department of Computer Sciences University of.
Hurricane Model Transitions to Operations at NCEP/EMC 2006 IHC Conference, Mobile, AL Robert Tuleya, S. Gopalkrishnan, Weixing Shen, N. Surgi, and H.Pan.
Introduction In 1904, Bjerknes pointed out that the future state of the atmosphere could be predicted by integrating the partial differential equations.
BEST PRACTICES ON MARINE INFORMATION MANAGEMENT AND DISSEMINATION Prof. Cherif SAMMARI
Animating smoke with dynamic balance Jin-Kyung Hong Chang-Hun Kim 발표 윤종철.
1 Julien Ramousse, Kodjo Agbossou, Yves Dubé and Pélopé Adzakpa Hydrogen Research Institute (IRH), Université du Québec à Trois-Rivières, C.P. 500, Trois-Rivières,
Page 1 – The Canadian Great Lakes Deterministic Coupled Water Cycle Prediction System PART 3 The Canadian Great Lakes Deterministic Coupled Water.
Emerging Research Opportunities at the Climate Modeling Laboratory NC State University (Presentation at NIA Meeting: 9/04/03) Fredrick H. M. Semazzi North.
GEMDM: SOFTWARE/PERFORMANCE
Chapter 1 Governing Equations of the Atmospheric Motion
Boundary layer equation:
Single column models Gunilla Svensson and Frank Kauker
Flammable extent of hydrogen jets close to surfaces
Models of atmospheric chemistry
Research Topic Image Name:.
Lecture 1: Introduction
M. Samaali, M. Sassi, V. Bouchet
Chapter 19 FORCED CONVECTION
Chapter 19 FORCED CONVECTION
Introduction results Forced Convection Excel Linear Regression tool
Presentation transcript:

A Shared Atmosphere-Ocean Dynamical Core: First Validation (Semi-Implicit Semi-Lagrangian) Pierre Pellerin(2), François Roy(1,3), Claude Girard(2), François J. Saucier(3), and Hal Ritchie(2) (1)Ocean Science Branch, Maurice Lamontagne Institute, Department of Fisheries and Oceans, Mont-Joli, Québec, Canada (1)Ocean Science Branch, Maurice Lamontagne Institute, Department of Fisheries and Oceans, Mont-Joli, Québec, Canada (2)Recherche en Prévision Numérique, Service Météorologique du Canada, Dorval, Québec, Canada (3)Institut des Sciences de la Mer, Université du Québec à Rimouski, Rimouski, Québec, Canada

Introduction The idea of a common kernel for the atmosphere and the ocean using the semi-implicit semi-Lagrangian method implemented at CMC/RPN: Advantages and Motivations for Recherche en Prévision Numérique (RPN) and Environment Canada: -Complete a pilot study initiated by the late André Robert -The method is already implemented at the Canadian Meteorological Centre (CMC) and optimized for operational runs on super-computers -Something to offer to oceanographers in favor of technical and scientific collaborations -Possible access to numerical and scientific developments from oceanographers - Identify approach for GEM or other future models

Quasi-unified semi-discrete equations AIR buoyancy generalized buoyancy generalized pressure Water Ref: Girard et Al. 2005: MWR

Lobjet Solide (advection semi-lagrangienne) U U V V P U V V P U U V P U V P Grille Arakawa Type C Objet solide 2)Interpolations Actions: 1) 1)Calcul des trajectoires Conditions Miroirs

Lobjet Solide (advection semi-lagrangienne) U U V V P U V V P U U V P U V P Grille Arakawa Type C Objet solide 2) 2)Interpolations 3) 3)Solveur Équation Elliptique Actions: 1) 1)Calcul des trajectoires Pour UU selon un mur en x: Pour VV selon un mur en x: Free slip

Lobjet solide (les masques): U U V V P U V V P U U V P U V P Le masque pour UU Le Masque VV Le masque pour P, WZ,BB …

Lobjet solide (Comparaisons IML – RPN):

RPN EAU IML EAU UU VV

Solid Objects: Von Karman Vortex Streets Evaluation of 3 physical parameters.

Solid object (RPN/IML cf laboratory): Reynolds = 104 Stagnation points Separation points ~ 80 ° Kundu: Fluid Mechanics Von Karman vortex streets Kundu: Fluid Mec.

Flow around a cylinder (RPN model: RE=140)

Laboratory Re=140 Cylinder RPN Re=140 Cylinder Few Numerical noise => Allow to produce realistic vortex Few Numerical diffusion => Allow to maintain the vortex Laboratory Re=140 Cylinder RPN Re=140 Cylinder

Demonstration experiment: Oklahoma city (300 x 200 x 50), DX=DY=1.5 meters, dt=0.12 sec, 4000 timesteps