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CONSTRAIN cold air outbreak DALES results Thomas Frederikse, Stephan de Roode, and Pier Siebesma LWP (kg m -2 ) at t=10 hr, N c = 10 cm -3

CONSTRAIN cold air outbreak DALES results

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CONSTRAIN cold air outbreak DALES results. LWP (kg m -2 ) at t=10 hr, N c = 10 cm -3. Thomas Frederikse, Stephan de Roode , and Pier Siebesma. Set up of the simulations. L (km) D x (m)N c (cm -3 )Purpose ________________________________________________ 102.420010Reference - PowerPoint PPT Presentation

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Page 1: CONSTRAIN cold air outbreak DALES results

CONSTRAIN cold air outbreakDALES results

Thomas Frederikse, Stephan de Roode, and Pier Siebesma

LWP (kg m-2) at t=10 hr, Nc = 10 cm-3

Page 2: CONSTRAIN cold air outbreak DALES results

Set up of the simulations

L (km) x (m) Nc (cm-3)Purpose

________________________________________________

102.4 200 10 Reference

102.4 400 10 Lower horizontal resolution

102.4 400 50 Larger droplet concentration

51.2 200 10 Smaller domain size

12.8 50 10 Fine-scale velocity structures

• No ice microphysics

Page 3: CONSTRAIN cold air outbreak DALES results

Time series: cloud covercl

oud

cove

r

time (hours)

L (km) x (m) Nc (cm-3)

102.4 200 10

102.4 400 10

102.4 400 50

51.2 200 10

Droplet concentration affects cloud cover evolution

Page 4: CONSTRAIN cold air outbreak DALES results

Liquid water potential temperatureL = 102.4 km, Nc = 10 cm-3

Coarser resolution hardly has an effect on the mean state evolution

t=3hr t=7hr

t=10hr

t=13hr

x = 200 m (solid)x = 400 m (dashed)

Page 5: CONSTRAIN cold air outbreak DALES results

Total water contentL = 102.4 km, Nc = 10 cm-3

Coarser resolution hardly has an effect on the mean state evolution

t=3hr t=7hr

t=10hr t=13hr

x = 200 m (solid)x = 400 m (dashed)

Page 6: CONSTRAIN cold air outbreak DALES results

Liquid water contentL = 102.4 km

Cloud droplet concentration has a large influence on the liquid water content

t=3hr t=7hr t=10hr

t=13hr

Nc = 10 cm-3 (solid)Nc = 50 cm-3 (dashed)

Page 7: CONSTRAIN cold air outbreak DALES results

Open-cell cloud structure t=7 hr, Nc = 10 cm-3

LWP (kg m-2)

x = 200 m x = 400 m

Page 8: CONSTRAIN cold air outbreak DALES results

Cell sizes grow with time t=10 hr, Nc = 10 cm-3

LWP (kg m-2)

x = 200 m x = 400 m

Page 9: CONSTRAIN cold air outbreak DALES results

Cell sizes grow with time t=13 hr, Nc = 10 cm-3

LWP (kg m-2)

x = 200 m x = 400 m

Page 10: CONSTRAIN cold air outbreak DALES results

Wind velocity structure t = 3hr, Nc = 10 cm-3 at z=362.5 m

Results from small domain size L=12.8 km, high horizontal resolution

U (-6 to 2 m/s) V (-15 to -8 m/s) W (+2 to -2 m/s)

12.8 km

12.8

km

Notice delicate vertical velocity (w) structure

Page 11: CONSTRAIN cold air outbreak DALES results

Effects of domain size (x=200m)t=13 hr, Nc = 10 cm-3

LWP (kg m-2)

L=50 km seems just sufficiently large

Page 12: CONSTRAIN cold air outbreak DALES results

Effects of cloud droplet concentration

LWP (kg m-2)

Open cells develop both for Nc = 10 and 50 cm-3

Nc = 50 cm-3 Nc = 10 cm-3

Page 13: CONSTRAIN cold air outbreak DALES results

Energy spectra (reference simulation, z = 487.5 m)

3 hours

7 hours

10 hours

13 hours

vertical velocity

wavenumber (m-1)

liquid water potential temperature

total water content

wavenumber (m-1)

wavenumber (m-1)

spec

tral e

nerg

ysp

ectra

l ene

rgy

spec

tral e

nerg

y

gradual shift of spectral energy towards larger scales

Page 14: CONSTRAIN cold air outbreak DALES results

Energy spectra (reference simulation, z = 1487.5 m)

3 hours

7 hours

10 hours

13 hours

vertical velocity

wavenumber (m-1)

liquid water potential temperature

total water content

wavenumber (m-1)

wavenumber (m-1)

spec

tral e

nerg

ysp

ectra

l ene

rgy

spec

tral e

nerg

y

gradual shift of spectral energy towards larger scales