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  • Hector simulation We found simulation largely depending on: Model initialization scheme Lateral boundary conditions Physical processes represented in the
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Hector simulation We found simulation largely depending on: • Model initialization scheme • Lateral boundary conditions • Physical processes represented in the model

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Page 1: Hector simulation We found simulation largely depending on: Model initialization scheme Lateral boundary conditions Physical processes represented in the

Hector simulation

We found simulation largely depending on:

• Model initialization scheme

• Lateral boundary conditions

• Physical processes represented in the model

Page 2: Hector simulation We found simulation largely depending on: Model initialization scheme Lateral boundary conditions Physical processes represented in the

Hector simulation – 06.02.2006 case

WRF initial conditions

1km resolution WRF domain

WRF lateral boundary conditions

Page 3: Hector simulation We found simulation largely depending on: Model initialization scheme Lateral boundary conditions Physical processes represented in the
Page 4: Hector simulation We found simulation largely depending on: Model initialization scheme Lateral boundary conditions Physical processes represented in the

1616thth November 2005 – single November 2005 – single `cell’`cell’

Page 5: Hector simulation We found simulation largely depending on: Model initialization scheme Lateral boundary conditions Physical processes represented in the

1616thth November 2005 November 2005

Page 6: Hector simulation We found simulation largely depending on: Model initialization scheme Lateral boundary conditions Physical processes represented in the

3030thth November 2005 – multi-cell November 2005 – multi-cell

Page 7: Hector simulation We found simulation largely depending on: Model initialization scheme Lateral boundary conditions Physical processes represented in the

3030thth November 2005 November 2005

Page 8: Hector simulation We found simulation largely depending on: Model initialization scheme Lateral boundary conditions Physical processes represented in the

1010thth February 2006 –squall - February 2006 –squall -likelike

Page 9: Hector simulation We found simulation largely depending on: Model initialization scheme Lateral boundary conditions Physical processes represented in the

1010thth February 2006 February 2006

Page 10: Hector simulation We found simulation largely depending on: Model initialization scheme Lateral boundary conditions Physical processes represented in the

1010thth February T, w February T, w

Page 11: Hector simulation We found simulation largely depending on: Model initialization scheme Lateral boundary conditions Physical processes represented in the

66thth February 2006 - weak February 2006 - weak

Page 12: Hector simulation We found simulation largely depending on: Model initialization scheme Lateral boundary conditions Physical processes represented in the

66thth February February

Page 13: Hector simulation We found simulation largely depending on: Model initialization scheme Lateral boundary conditions Physical processes represented in the

66thth February 2006 February 2006

Page 14: Hector simulation We found simulation largely depending on: Model initialization scheme Lateral boundary conditions Physical processes represented in the

Hector simulation – 06.02.2006 case

Radar observed WRF simulated

Precipitation

Page 15: Hector simulation We found simulation largely depending on: Model initialization scheme Lateral boundary conditions Physical processes represented in the

Hector simulation – 06.02.2006 case

Observed and simulated radar reflectivity along the W-E cross section of Hector

Observed Simulated

Page 16: Hector simulation We found simulation largely depending on: Model initialization scheme Lateral boundary conditions Physical processes represented in the

Hector simulation – 06.02.2006 case

Observed (red) and simulated (green) surface latent and sensible heat flux

Over the sea Over the land

Page 17: Hector simulation We found simulation largely depending on: Model initialization scheme Lateral boundary conditions Physical processes represented in the

Hector simulation – 06.02.2006 caseDornier observed (red) and WRF simulated (green) low level

variables

Tem

pera

ture R

ela

tive

hu

mid

ity

U w

ind

com

pon

en

t

V w

ind

com

pon

en

t

Page 18: Hector simulation We found simulation largely depending on: Model initialization scheme Lateral boundary conditions Physical processes represented in the

Hector simulation – 06.02.2006 caseEgret observed (red) and WRF simulated (green) high level

variables

Tem

pera

ture

U w

ind

com

pon

en

t

V w

ind

com

pon

en

t

Page 19: Hector simulation We found simulation largely depending on: Model initialization scheme Lateral boundary conditions Physical processes represented in the

Hector simulation – 06.02.2006 caseSimulated aerosol effect ?

Sim

ula

ted

tota

l ra

in

wate

r

Time

Page 20: Hector simulation We found simulation largely depending on: Model initialization scheme Lateral boundary conditions Physical processes represented in the

Hector simulation – 06.02.2006 caseSimulated aerosol effect ?

Sim

ula

ted

tota

l clo

ud

w

ate

r

Time

Page 21: Hector simulation We found simulation largely depending on: Model initialization scheme Lateral boundary conditions Physical processes represented in the

Hector simulation – 06.02.2006 caseSimulated aerosol effect ?

Sim

ula

ted

tota

l clo

ud

ice

Time

Page 22: Hector simulation We found simulation largely depending on: Model initialization scheme Lateral boundary conditions Physical processes represented in the

Hector simulation – 06.02.2006 caseSimulated aerosol effect ?

Sim

ula

ted

tota

l sn

ow

w

ate

r

Time

Page 23: Hector simulation We found simulation largely depending on: Model initialization scheme Lateral boundary conditions Physical processes represented in the

SummarySummary

• Two modes of simulationTwo modes of simulation– OF – doesn’t work too well in generalityOF – doesn’t work too well in generality– DA – gives good agreement for a lot of DA – gives good agreement for a lot of

cases, but the statistics show too low cases, but the statistics show too low cloud fraction.cloud fraction.

• Aerosol effects are present for the 6Aerosol effects are present for the 6thth February case.February case.– Need more simulations of different cases Need more simulations of different cases

to see how robust this is.to see how robust this is.


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