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Natalie Harvey, Steve Natalie Harvey, Steve

Natalie Harvey, Steve - PowerPoint Presentation

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Natalie Harvey, Steve - PPT Presentation

Woolnough Alision Stirling WP21ab High Resolution Simulations of Convection GOAL To inform parametrization development and in particular improve the temporal evolution of convection convective memory ID: 615812

500km tke time resolution tke 500km resolution time budget integrated hours vertically terms diagnostics simulations diurnal cycle convection 100m

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Slide1

Natalie Harvey, Steve

Woolnough, Alision Stirling

WP2.1a,b High Resolution Simulations of Convection

GOAL: To inform parametrization development and in particular improve the temporal evolution of convection (“convective memory”)Slide2

Idealised cloud-resolving simulations

2

“Radiative” Equilibrium ConvectionImposed “radiation”Interactive “radiation”500km x 500km at ~100m resolution

500km x 500km

at ~

100m

resolution

Diurnal cycle over land

Homogeneous surface

Heterogenous

surface

500km x 500km

at ~

100m

resolution

500km x 500km

at ~

100m

resolution

Also companion simulations at 4km, 12km and ~40km resolutionSlide3

Natalie Harvey, Steve

Woolnough, Alision Stirling

WP2.1a,b High Resolution Simulations of Convection

TODAY: Development of tools to analyse the TKE budget of an idealised diurnal cycle Slide4

4

Analysis methods and tools

Reynolds averaged budgets: TKE, w’

2

, w’

θ

Whole domain, steady state flow

Sub-domains – extra terms

Which terms control departures from local steady state?

Conditionally-sampled diagnostics

Spectral diagnostics

e.g. look at buoyant cloudy updrafts only

Scales for dissipation and production

Upscale and down scale transportsSlide5

TKE budget equation

5

TKE: Horizontal homogeneity and neglect subsidence

I: Tendency

III: Buoyancy

IV: Shear

V: turbulent transport

VI: pressure correlation

VII: DissipationSlide6

Diurnal cycle

6

Using LEM 2D Horizontal grid: 512 x 1kmVertical grid: 76 levels with 20 km top Surface forcing based on EUROCS, balanced by large scale cooling 20 days with 10 minute output Time (hours)Wm-2Slide7

How different?

7

Time (hours)

Height (km)Slide8

How different?

8

Time (hours)Height (km)Height (km)Vertically integrated qxVertically integrated qx

Cycle 3

Cycle 12Slide9

How different?

9

Time (hours)precipitationVertically integrated TKESlide10

TKE budget terms

10

Time (hours)

Time (hours)Slide11

TKE budget terms

11

Composite of 18 diurnal cycles Slide12

12

TKE budget terms:

vertical integralsSlide13

13

TKE budget terms:

vertical integrals

Time (hours)

Vertically integrated TKE

Vertically integrated budget term

Wm

-2Slide14

14

TKE budget terms:

regression on to vertically integrated TKE Slide15

15

Conditionally sampled diagnostics

How does TKE relate to conditionally averaged diagnostics? Time of vertically integrated TKE maximumSlide16

16

Spectral diagnostics

Spatial spectra2D vertical velocity - instantaneous every 10 minsTransports? Slide17

Next steps?

Continue the development of tools to analyse the diurnal cycle

Reynolds averaged budgetsExtend to: Conditional samplingSpectral diagnostics

Design and perform the high resolution simulations (MONC or idealised UM?)

17