Setup specifications here : http://www.knmi.nl/samenw/eurocs/ARM/case_ARM_html/case_ARM.html
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The runs start at 11.30 UTC, or t = 41400 s.
The surface pressure should be set to 97000 Pa, and 100000 Pa should be used as the reference pressure for converting between potential temperature and temperature.
Initial profils are given.
Surface sensible and latent heat fluxes to be imposed in model runs.
ILarge scale forcings and radiation: the values of Atheta, Rtheta and Aqt which are to be used to scale
 the values of the large-scale advective tendency of theta, of the large-scale advective tendency of qt,
 and of the radiative tendency to be applied to theta. 
These values are given at various times, and linear interpolation should be be used to obtain values
 at intermediate times.
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WARNING !!
For the moment, case runs only with 19 or 40 levels
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This case may also be used to run "Eddy diffusion mass flux" comparison, if we switch off convection.
See def_cas_EDMF.pdf in this directory.

More details on this case:
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	+ andy_caseARM_short.ps in this directory

	+ The diurnal cycle of shallow Cumulus clouds over land: ... Corresponding author address: Geert Lenderink, KNMI, 3730 AE De Bilt, P.O. Box ... QJRMS. 2. Siebesma and Holtslag 1996; Grant and Brown 1999; Bechtold et al.

	+ The diurnal cycle of shallow cumulus clouds over land: A single-column model intercomparison study
Duynkerke et al, QJRMS 2004	

	+ large essy-simulation of the diurnal cycle of shallow cumulus convection over land. Brown et al, QJRMS 2002
