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Multi-Scale Physics Faculty of Applied Sciences The formation of mesoscale fluctuations by boundary layer convection Harm Jonker
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The formation of mesoscale fluctuations by boundary layer convection

Jan 18, 2016

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The formation of mesoscale fluctuations by boundary layer convection. Harm Jonker. A spectral gap?. (Stull). time. Cold Air Outbreak. Liquid water path. LES of Sc (ASTEX). Dx = Dy = 100m. L = 25.6km (16hr). L = 12.8km (12hr). L = 6.4km (8hr). “Large Eddy Simulations: - PowerPoint PPT Presentation
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Page 1: The formation of mesoscale fluctuations by boundary layer convection

Multi-Scale Physics Faculty of Applied Sciences

The formation of mesoscale fluctuations by boundary layer

convection

Harm Jonker

Page 2: The formation of mesoscale fluctuations by boundary layer convection

Multi-Scale Physics Faculty of Applied Sciences

A spectral gap?

(Stull)

Page 3: The formation of mesoscale fluctuations by boundary layer convection

Multi-Scale Physics Faculty of Applied Sciences

Cold Air Outbreak

time

Page 4: The formation of mesoscale fluctuations by boundary layer convection

L = 6.4km(8hr)

Dx = Dy = 100m

L = 12.8km

(12hr)

L = 25.6km (16hr)

LES of Sc (ASTEX) Liquid water path

“Large Eddy Simulations: How large is large enough?”, de Roode, Duynkerke, Jonker, JAS 2004

“How long is long enough when measuring fluxes and other turbulence statistics?”, Lenschow, et al. J. Atmos. Oceanic Technol., 1994

Page 5: The formation of mesoscale fluctuations by boundary layer convection

w

qt u

lwp

Page 6: The formation of mesoscale fluctuations by boundary layer convection

Intermediate Conclusions

1) the formation of dominating mesoscale fluctuations is an integral part of PBL dynamics!- no mesoscale forcings

- what is the origin (mechanism) ?

- latent heat release- radiative cooling- entrainment- inverse cascade

Atkinson and ZhangFiedler, van Delden, Muller and Chlond, Randall and Shao,Dornbrack, ……

Page 7: The formation of mesoscale fluctuations by boundary layer convection

Multi-Scale Physics Faculty of Applied Sciences

Convective Atmospheric Boundary Layer

penetrative convection

zi

heat flux

entrainment

entrainment

tracer flux

Page 8: The formation of mesoscale fluctuations by boundary layer convection

Saline convection tank

Laser Induced Fluorescence (LIF)

fresh water

salt water (2%)

fresh water + fluorescent dye

buoyancy flux & tracer flux

Laser

(z)

digital camera

p

Han van Dop, IMAUMark Hibberd, CSIROJos Verdoold, Thijs Heus, Esther Hagen

Page 9: The formation of mesoscale fluctuations by boundary layer convection

Laser Induced Fluorescence

Page 10: The formation of mesoscale fluctuations by boundary layer convection

Laser Induced Fluorescence (LIF)“bottom-up” tracer

boundary layer depth structure

(Verdoold, Delft, 2001)(see also van Dop, et al. BLM 2005)

Page 11: The formation of mesoscale fluctuations by boundary layer convection

Multi-Scale Physics Faculty of Applied Sciences

Conclusions1) the formation of dominating mesoscale fluctuations is an integral part of PBL convective dynamics!

2) latent heat and radiation are not essential(but speed up the process considerably)

3) budgets: no inverse cascade on average. significant backscatter (on all scales)

4) production: ineffective (slow), but spectral transfer is just as ineffective

5) the spectral behaviour of w at large scales is crucial