experiences with a statistical cloud scheme in combination with kain-fritsch convection

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Experiences with a statistical cloud scheme in combination with Kain-Fritsch convection. Wim de Rooy KNMI. Pier Siebesma Geert Lenderink Sander Tijm. q sat(T). q t. (T,q t ). T. Statistical cloud scheme. Determine cloud cover and liquid water using the sub-grid variability :. - PowerPoint PPT Presentation

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Page 1: Experiences with a statistical cloud scheme in combination with Kain-Fritsch convection
Page 2: Experiences with a statistical cloud scheme in combination with Kain-Fritsch convection

T

qsat(T)

qt .(T,qt)

Statistical cloud scheme

•Determine cloud cover and liquid water using the sub-grid variability:

Page 3: Experiences with a statistical cloud scheme in combination with Kain-Fritsch convection

Go over to one variable:

s

satt qqtQ

For a certain PDF, cloud cover and liquid water can be written as a function of just one variable:

Main Problem: How to determine s?

(for simplicity: )2'2

ts q

s

satt Tpqqt

),(

sqt-qsat(p,T)

Page 4: Experiences with a statistical cloud scheme in combination with Kain-Fritsch convection

How to parameterize variance?

Link it to convection/turbulence schemes using a variance budget:

21t

tt q

z

qqw

2*)( tcloud

cut

tcut q

l

w

z

qqqM

z

ql

w

qqMq t

cloudcut

cut

t

*

2 )(

Production Dissipation

Lenderink& Siebesma 2000

2't

turb

ttturb q

l

e

z

q

z

qel

Variance due to convection2

22'

z

qlq tturbt

Variance due to turbulence

Page 5: Experiences with a statistical cloud scheme in combination with Kain-Fritsch convection

Variance due to/coupled with turbulence:

2

22'

z

qlq tturbt

Very simple: • = (0.02qs)2 (Lenderink)

Simple: •lturb=40 (Siebesma) •lturb=0.2z for z<900 and 180 for z> 900m (Chaboureau & Bechtold)

Less simple (stability dependent):•lturb from moist CBR (implementation Colin Jones)

Even without convective or turbulent activity (free atmosphere)some variance is needed!

2'tq

Page 6: Experiences with a statistical cloud scheme in combination with Kain-Fritsch convection

Project: Statistical cloud scheme(from simple to complex)

First 1D tests cases (start with BOMEX):

1. Use cloud cover (ac) diagnostically

2. Use ac and ql prognostically

Subsequently 3D

1. Test cases

2. Long time verification

Page 7: Experiences with a statistical cloud scheme in combination with Kain-Fritsch convection

Problems with Hirlam KF convection:

•Intermittent behavior

•Negative buoyant cloud (TV_UPDRAFT < TV_ENVIRONMENT)

•Artificially looking closure for shallow convection

•Mass flux does not decrease (enough) with height

•Results for Bomex are disappointing

•Fundamental problems? (Sander Jonker)

•Code is complex, hard to understand (and slow)

Page 8: Experiences with a statistical cloud scheme in combination with Kain-Fritsch convection

q profile BOMEX with standard Hirlam KF

Page 9: Experiences with a statistical cloud scheme in combination with Kain-Fritsch convection

Some of the adaptations to KF:

•Fractional entrainment/detrainment according to Siebesma (2003)

•Vertical velocity equation (Gregory, 2001)

•More simple and physically appealing closure (Grant, 2001)

Good results with convection and statistical cloud scheme for Bomex

Page 10: Experiences with a statistical cloud scheme in combination with Kain-Fritsch convection

q profile BOMEX with adaptations

Page 11: Experiences with a statistical cloud scheme in combination with Kain-Fritsch convection

Variance BOMEX

LES Hirlam (40 lvls) with modified KF

Page 12: Experiences with a statistical cloud scheme in combination with Kain-Fritsch convection

Cloud cover Bomex

LES Hirlam with modified KF

Page 13: Experiences with a statistical cloud scheme in combination with Kain-Fritsch convection

Our conclusion: It is not appealing to build further developments on the current Hirlam KF code.

Two alternatives:1. KF from Meso-NH2. Latest ECMWF IFS convection code

Peter Bechtold coded 1 and currently works on 2.His advice: Use 2 (performance, speed, use of AROME iscompatible with 2, synergy, etc.)

=> Implement 2 in Hirlam(1D)

Page 14: Experiences with a statistical cloud scheme in combination with Kain-Fritsch convection

Provisional results: Hirlam 1d with new ECMWF convection,old Sundqvist condensation and moist CBR (Colin Jones)