[Wrf-users] Some Notes About CFLS
HEDDE Thierry 137147
thierry.hedde at cea.fr
Tue Oct 3 01:44:12 MDT 2017
Hi Barry and thanks for the CFLs notes
I would add to point 5 (reduce time step)
6) Use the adaptative_time_step option which is working well with WRF 3.9.1
Here is the classical tuning, I'm using for it (-1 means : automatic) for a 2 domains run (9km, 3km) fed with gfs 0.25°
&domains
use_adaptive_time_step = .true.,
step_to_output_time = .true.,
target_cfl = 1.2, 1.2
target_hcfl = .84, .84,
max_step_increase_pct = 5, 51,
starting_time_step = -1, -1,
max_time_step = -1, -1,
min_time_step = -1, -1,
adaptation_domain = 1,
I'm testing it for my operational daily prognostics over France and as far as now, I've noticed no crash, it's quicker and the prognostic quality looks the same (qualitatively)
The timestep is mainly at 8*DX during the run but sometimes adapts itself down to 4*DX
Cheers
Thierry
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Today's Topics:
1. Some Notes About CFLS (Barry Lynn)
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Message: 1
Date: Sun, 1 Oct 2017 19:36:17 +0300
From: Barry Lynn <barry.h.lynn at gmail.com>
To: wrf-users at ucar.edu
Cc: wrfhelp <wrfhelp at ucar.edu>
Subject: [Wrf-users] Some Notes About CFLS
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<CAN7Bv264m961RoHS2DXr42pJkF8yiHEutjBTXQ3Ok1by990FfA at mail.gmail.com>
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Hello:
I had some problems with CFLS when setting up my 12/4 km domain.
I had particular points which (at almost every time step) had CFL "errors."
There are few things to do about this.
1) Change epssm to be closer to 0.5, rather than 0.1 (or 0.2).
2) Set smooth_option = 2 (this smoothes near the boundaries of the inner
domain.)
3) Set smooth_cg_top = .true. (smoothes topography near boundary of outer
domain.)
These steps together can reduce the number of CFLs.
4) damp_opt = 3 (reduces upper level instability; CFLs occurring at upper levels).
However, one other, but very important note, is to be sure to place the boundaries of the inner domain away from steep terrain (see attached pdf. I had CFLS near the right boundary until I moved the right upper boundary into the water.)
5) Lastly, if you get CFLs during severe or strong storms, you may have to reduce the timestep from 6 to 5 or even 4 times the grid size (at least until you've passed the period of greater model instability).
Barry Lynn
--
Barry H. Lynn, Ph.D
Senior Lecturer,
The Institute of the Earth Science,
The Hebrew University of Jerusalem,
Givat Ram, Jerusalem 91904, Israel
Tel: 972 547 231 170
Fax: (972)-25662581
C.E.O, Weather It Is, LTD
Weather and Climate Focus
http://weather-it-is.com
Jerusalem, Israel
Local: 02 930 9525
Cell: 054 7 231 170
Int-IS: x972 2 930 9525
US 914 432 3108
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