1' The Operational System of Weather Forecasting in MeteoGalicia 2' MOHID a water modelling system 3 - PowerPoint PPT Presentation

1 / 32
About This Presentation
Title:

1' The Operational System of Weather Forecasting in MeteoGalicia 2' MOHID a water modelling system 3

Description:

1. The Operational System of Weather Forecasting in ... Advection. Diffusion. Oil processes. Meteo. Galicia. MOHID hydrodynamic module. Main characteristics ... – PowerPoint PPT presentation

Number of Views:106
Avg rating:3.0/5.0
Slides: 33
Provided by: ramiro6
Category:

less

Transcript and Presenter's Notes

Title: 1' The Operational System of Weather Forecasting in MeteoGalicia 2' MOHID a water modelling system 3


1
1. The Operational System of Weather Forecasting
in MeteoGalicia2. MOHID a water modelling
system 3. Outlooks
Meteo
Galicia
Summary
2
The Operational System of Weather Forecasting in
MeteoGalicia
Universidade de Santiago de Compostela
Consellería de Medio Ambiente
Meteo
Galicia
  • V. Pérez-Muñuzuri, P. Montero, E. Penabad, C.F.
    Balseiro, P. Carracedo and B. Gómez
  • http//meteo.usc.es

3
Numerical model applied to Galicia weather
forecast
  • ARPS Advanced Regional Prediction System.
  • Prognostic
  • Navier-Stokes equations (u,v,w)
  • Conservation equation for heat (?)
  • Conservation equation for water substances (qi)
  • Pressure equation (p)
  • Turbulent kinetic energy equation (TKE)
  • Diagnostic
  • Equation of state of moist air (?)

4
Numerical model applied to Galicia weather
forecast
  • ARPS
  • Operational non-hydrostatic model
  • Widely tested and validated
  • Application to different environments (weather
    forecast, dispersion modeling (As Pontes, A
    Coruña harbor), coupling to climate models, etc)
  • nesting
  • standard initial and boundary conditions
  • specific parameterizations
  • high resolutions
  • Galicia forecast
  • wind, temperature, pressure, humidity
  • clouds
  • rain, ice, snow, graupel
  • storms

5
Numerical model topography
Fine Grid 43x43, 10 km
Coarse Grid 65x51, 50 km
6
Daily Operational System Twice per day 00Z 12Z
7
28 Oct, 2000
IR 1700 UTC
0700 UTC Rain
1200 UTC Rain
1800 UTC Rain
A
B
A
B
8
22 surface stations Galician meteorological
network
http//www.siam-cma.org
  • Model validation
  • Statistics
  • Data assimilation

9
Results Wind surface fields
  • Coarse Grid Fine Grid

10
Model Validation for the Prestige Case
  • Wind Surface Model Output vs Observations
    (Corrubedo)

Module
Direction
11
Wind Drift Trajectories
Trajectories Wind drift (3 ) Initial positions
from observations
Trajectories Wind drift (3 ) Confidence
Limit Initial position from sunk Prestige
12
  • An hydrodynamical model is needed
  • A strategy of sharing information was established
    between MeteoGalicia and IST to develop an
    atmospheric ocean coupled model (ARPS-MOHID)

13
MOHID a water modelling system
  • R. Neves, F. Braunschweig, R. Fernandes, P.
    Leitão, P. Pina and H. Coelho
  • http//www.mohid.com

14
Presentation contents
  • MOHID structure
  • Some results
  • The case of the prestige

15
Surface
http//www.mohid.com
Oil processes
Water Properties


Water Quality.
Waves
Dissolved properties
Currents
Advection Diffusion
Turbulence http//www.gotm.net
Particulated Properties
Módulo Interface BOTTOM
Sediment Properties
Sediment Quality.
Interstitial water
  • Physical processes
  • Consolidation, bioturbation

Solid phase
16
MOHID hydrodynamic module Main characteristics
  • Boussinesq and hydrostatic approximations
  • Finite volumes discretization
  • Generic vertical discretization
  • Baroclinic pressure z level
  • Semi-implicit
  • One-way nesting
  • Boundary conditions Flow relaxation, radiation

17
Processes and scales integration
Initial schematic profile
2D barotropic flow
3D 10 layers
3D 10 layers
Tide Constant North wind 0.1 Pa Density gradients
ModelLevel 2
18
10 days simulation
Velocity 2D
SST / velocity
SST / velocity
Tide Density gradients Constant North wind 0.1
Pa
Galicia West Coast
19
Satellite Images 1994
  • 19 Jun 25 Jun ? North Wind 0.1 Pa ?
    26 Jun 02 Jul

? N Wind 0.1 Pa ?
2nd day
10th day
20
Primary production
21
Climatologic forcing (Coelho et al., 2002)
  • Dx 1/4º . Result after 2 years of spin up

22
Global tide solution
This global tide results are being validate
comparing them with the FES95.2 solution
23
The Prestige Case
24
Oil drift before ship breaking
Ship Trajectory
Oil Drift - Mohid
Forcing Conditions - Wind (spatial / temporal
variation prediction from operational model of
Meteo Galicia and IST) - Hydrodynamics 20
layers (superficial layer 10cm) with variable
density (climatologic stratification) slope
current - Vertical turbulence (GOTM model) - 2 Km
minimum spatial step
25
Oil drift before ship breaking
26
Oil drift after ship breaking
Trajectory observed
Mohid simulations
Forcing Conditions - Wind (spatial / temporal
variation prediction from operational model of
Meteo Galicia and IST) - Hydrodynamics 20
layers (superficial layer 10cm) with variable
density (climatologic stratification) slope
current - Vertical turbulence (GOTM model) - 10
Km minimum spatial step
27
Near shore oil drift after ship breaking
Forcing Conditions - Wind (spatial / temporal
variation prediction from operational model of
Meteo Galicia and IST) - Hydrodynamics 20
layers (superficial layer 10cm) with variable
density (climatologic stratification) slope
current - Vertical turbulence (GOTM model) - 10
Km minimum spatial step
28
Outlooks
Meteo
Galicia
29
Current problems
  • Offshore aerial observations shows surface oil
    slicks transported by wind drift
  • Nearshore some oil slicks suddenly appeared in
    the right side of the wind drift trajectory
  • This can be explained by fuel oil transported
    in subsurface layers, by surface currents Coma
    Hypothesis. Tarballs, consisting mainly of the
    micelle part of the oilspill, have travelled
    within the mixed layer (approx. 15 m depth), thus
    being affected by the currents and not only by
    the wind stress.

30
Expected difficulties
  • How to validate nested model results ? Satellite
    images, CTD, ADCP?
  • How to validate ascending velocity of fuel oil
    escaping from the tanker?
  • How to validate currents along the ascending
    trajectory of fuel oil ?

31
Ongoing Work
  • Run a 3D baroclinic model for the North Atlantic
  • The solution will be refined in the prestige area
    of influence using several nesting levels (50 km
    1 km).
  • The joint effect of tide, wind, river run-off and
    atmosphere heat fluxes will be considered
  • Compute the fuel oil ascension using tracers with
    buoyancy

32
Future Work
  • Need for an Oceanographical-Meteorological
    Operational Model
  • Simulation and analysis of possible solutions for
    the Prestige considering the different scenarios
    of recovering the oil at 3.5 km depth
  • Management of a data base with different
    simulations of oil-spills in order to build a GIS
    system with these statistical results to prevent
    new oil spills and be able to offer results of
    trajectories within a few hours after the
    disaster.
  • Need of a strategical plan for quick response in
    case of new oil spills
Write a Comment
User Comments (0)
About PowerShow.com