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A Single Column Model version of HIRLAM

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Title: A Single Column Model version of HIRLAM


1
A Single Column Model version of HIRLAM
  • Javier Calvo

2
Motivation
  • 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.

3
Background
  • 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.

4
The 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.

5
How 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
6
Calling tree dynamics
reads namelists
reads departure data
vertical interpolation to model levels
dynamical tendencies
prescribed tendecies if needed
Postprocesing and printinds
7
Calling tree
8
Calling tree
9
Select physics routines with NOPTION()
Probably more options than in the complete HIRLAM
CBR turbulence NOPTION(2)2
10
Send 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
11
Clouds and Convection STRACO
STRACO NOPTION(2)1
12
Clouds and Convection KF/RK
KF/RK NOPTION(2)4
CBR turbulence NOPTION(2)2
13
SCM 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

14
To 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.

15
Feedback
  • Feedback and help is welcome to improve the SCM
    and to achieve a wide use of it.

16
The end
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