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1 14tn ALADIN Workshop - Inns 14tn ALADIN Workshop - Inns bruck bruck Testing the Testing the new ACDRAG scheme new ACDRAG scheme in the ALPIA in the ALPIA environment environment A tricky A tricky ping-pong ping-pong game game Bart Catry Ghent University Belgium F. Bouyssel (Fr) R. Brozkova (Cz) J. Cedilnik (Si) M. Derkova (Sk) D. Dvar (Hr) J.-F. Geleyn (Fr) R. Mladek (Cz)

1 14tn ALADIN Workshop - Innsbruck Testing the new ACDRAG scheme in the ALPIA environment A tricky ping-ponggame Bart Catry Ghent University Belgium F

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Page 1: 1 14tn ALADIN Workshop - Innsbruck Testing the new ACDRAG scheme in the ALPIA environment A tricky ping-ponggame Bart Catry Ghent University Belgium F

1114tn ALADIN Workshop - Innsbruck14tn ALADIN Workshop - Innsbruck

Testing the Testing the new ACDRAG scheme new ACDRAG scheme

in the ALPIA in the ALPIA environmentenvironment

A tricky A tricky ping-pong ping-pong gamegame

Bart Catry

Ghent University

Belgium

F. Bouyssel (Fr)R. Brozkova (Cz)J. Cedilnik (Si)

M. Derkova (Sk)

D. Dvar (Hr)

J.-F. Geleyn (Fr)

R. Mladek (Cz)

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14tn ALADIN Workshop - Innsbruck14tn ALADIN Workshop - Innsbruck 22

Outline PresentationOutline Presentation• Introduction• The new ACDRAG scheme (short)• The ALPIA domain• Momentum Budgets• The experiments• Tuning of the new scheme• Need for a parameterization scheme ?• Suppression of the envelope• Conclusions

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IntroductionIntroduction

Representation of the subgrid scale effects

of the unresolved orography:• Increased surface roughness length• Envelope orography (flow blocking & valley air

isolation)• Gravity wave & from drag• Lift (volume effect orthogonal to the background

wind)

ProblemsProblems

Still needed while others don’tStill needed while others don’t

Contradiction concerning Contradiction concerning FFc c

Need for a geostrophic wind approximationNeed for a geostrophic wind approximation

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The new ACDRAG schemeThe new ACDRAG schemeF inverse Froude numberFc critical F value (=0.5)τ total surface stressτ lin surface stress from the linear theoryCd drag coefficient

FFclin /

Old scheme New scheme

F

F

F

FC

F

F ccd

clin 11

F

FC

F

F cd

clin 11

lin

F > Fc

F < Fc

+ new lift+ new lift

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The ALPIA domainThe ALPIA domainDomain centered over the French Alps in 4 different resolutions:

10km

5km 2.5km 1.25km

10 km 5 km

2.5 km 1.25 km

96 x 96 x 37192 x 192 x 52384 x 384 x 71768 x 768 x 96

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Momentum BudgetsMomentum Budgets

0param

2

y

hppfu

y

ppuw

y

v

x

uv

t

vhref

refz

,z

h

QdzQ

Momentum budgets are studied in a box (of which the height varies from 0 to 20km)

Should agree the following balance equation (e.g. for the meridional case):

AA

1QdxdyQ

With:Contribution ofparameterizations

h: surfacez: top of the box

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Experiments (Experiments (Semi-Academical))

• The atmosphere is dry, inviscid, in hydrostatic equilibrium and its static stability is given by a constant Brunt-Vaisälä frequency N = 0.01

• A constant reference flow of 7 m/s form the NW• Geostrophic equilibrium with a constant Coriolis

parameter f = 0.0001• Reference values of temperature and density prescribed

in the middle of the domain at sea level: T0 = 300K and ρ0 = 1 kg/m3

• Forecast length set to 6 hours• Two time level semi Lagrangian semi implicit approach

with an Aladin 15 master

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Experiments (Global)Experiments (Global)

• ARPEGE model in T358 resolution and in unstretched mode

• Equivalent to parallel suite in Toulouse• New topography database• No envelope

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Tuning of the new schemeTuning of the new scheme(resolution independent)(resolution independent)

Performed on ALPIA domain and checked with ARPEGE and ALADIN-CE tests + additional constraint given by the Olafsson & Bougeault 1997:

α = 1.0 (old value, Lott & Miller, 1997)

β = 0.5

HOBST = 3 (old value, a bit high)

GWDSE = 0.020 (theoretical value)

GWDLT = 1.0 (theoretical value)

GWDCD = 5.4 (a bit high)

lin

F F FFcc

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Need for a parameterization (1)Need for a parameterization (1)

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Need for a parameterization (2)Need for a parameterization (2)

1. Parameterization is needed for horizontal mesh sizes from ~ 5 km

2. New ACDRAG scheme is tuned resolution independent

• Without parameterization the budgets on the different scales are too widely distributed

• When applying the new scheme the budgets of different scales converge towards the 2.5km budget

• Strange behavior at 2.5km

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Need for a parameterization (3)Need for a parameterization (3)

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Suppression of the envelope (1)Suppression of the envelope (1)

New lift works orthogonal on a good estimation of the geostrophic wind

New lift scheme should be able to take care of the volume of the subgrid mountain and should change the direction of the wind

New lift scheme can remove volume effect of the New lift scheme can remove volume effect of the envelope while keeping its barrier effect by envelope while keeping its barrier effect by changing the wind directionchanging the wind direction

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Suppression of the envelope (2)Suppression of the envelope (2)

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Suppression of the envelope (3)Suppression of the envelope (3)

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ConclusionsConclusions

• The new ACDRAG scheme is tuned to be resolution independent

• Parameterization is needed for horizontal mesh sizes from ~ 5 km

• The envelope can be suppressed by the new lift scheme

• The thin line between param / no param is not clear