Title: A Single Column Model version of HIRLAM
1A Single Column Model version of HIRLAM
2Motivation
- The have a reference SCM version of HIRLAM for
research and validation of model physics. - The idea is to maintain a code very close to the
reference complete HIRLAM or even included within
it. - Including different case studies to be used as
reference cases. - Trying to gather as many users as possible within
HIRLAM community.
3Background
- Currently several SCMs are used by Hirlam
researchers. - Its difficult to maintain them updated with the
reference model. - Comparisons are always uncertain due to the
different set ups. - Version most widely used is the one developed by
B. Sass and previously used for the turbulence
intercomparisons. - Complete model change significantly due to the
inclusion of ISBA surface scheme (tile approach). - New cases coded for some versions from EUROCS
cloud project.
4The new Single Column Model
- Case set up and philosophy from B. Sasss 1D
model lifted to the new SCM. - Dinamics follow quite closely the complete HIRLAM
- SCM versions of some routines included.
- 3D structure of the arrays kept.
- This facilitates updates from the complete model.
- The SCM can be better used for debugging and
optimization. - Maybe the model could be extent to 2 point model
or 2D model.
5How to run the model
- Simple steering unix script
- Makefile
- Control through namelist
- Output in ASCII format
- In principle plotting bu gnuplot or grads
- Input data in ASCII format
- Source versions based on RCS
H1d/EXP/bin/Run1d,Plot Data/iniARM_Cu.dat Grdy1d p
hys
6Calling tree dynamics
reads namelists
reads departure data
vertical interpolation to model levels
dynamical tendencies
prescribed tendecies if needed
Postprocesing and printinds
7Calling tree
8Calling tree
9Select physics routines with NOPTION()
Probably more options than in the complete HIRLAM
CBR turbulence NOPTION(2)2
10Send diagnostics from physics to printing routine
- Deviation from the complete model physics trough
directives H1D - SCM physics shoud work without modications in the
complete HIRLAM
CBR turbulence
i fdef H1D endif
11Clouds and Convection STRACO
STRACO NOPTION(2)1
12Clouds and Convection KF/RK
KF/RK NOPTION(2)4
CBR turbulence NOPTION(2)2
13SCM cases studies
Dry boundary layer 1.- Convective BL with some
shear (case WC05 in Ayotte et al., BLM, 1996) 4.-
Pure convective case with no wind (Ayotte,
1995) 5.- Lepzig case thermally neutral and
shear driven with strong winds 6.- Intermittent
turbulence in a thermally stable BL layer (from
SABLES) BL clouds 2.- Sc case from GCSS case 3
(Duynkerke, 1998) 8.- Diurnal cycle of Sc over
sea (EUROCS) 3.- Shallow Cu over sea from BOMEX
(Siebesma and Holtslag, 1996) 7.- Diurnal cycle
of Shallow Cu over land (ARMEUROCS) Deep
convection 10.- Diurnal cycle of Deep Cu over
land (ARMGCSS 3a case) 9.- Diurnal cycle of
Deep Cu over land (ARMidealized case from EUROCS)
- 0.- Initialization and dynamical tendencies
from the complete HIRLAM model. - xx.- Sensitivity of Deep Cu to environmental
humidity (idealized case from EUROCS) - xx.- Long integration (at least 30 days) from
TOGA COARE
14To be done
- Coding of all case studies
- Inclusion of new physics schemes under
development - moist turbulence and statistical clouds (Sander
volunteers) - Tiedtke convection with statistical clouds?
- Documentation of the SCM and the cases.
- Basic plotting tool?
- Based on gnuplot/grads?
- Inclusion of observations and LES results for
comparison.
15Feedback
- Feedback and help is welcome to improve the SCM
and to achieve a wide use of it.
16The end