Overview
OpenIFS includes a number of idealised configurations. In this article we explain how to configure the model for an 'aqua-planet' simulation. An aqua-planet is one that includes no topography and no land. It's a highly simplified representation of Earth but useful for a number of studies.
Further information
The aquaplanet configuration (enabled by namelist variable LAQUA) is based on the Neale & Hoskins publications:
- Neale, R. B. and Hoskins B. J., 2000a, A standard test for AGCMs and their physical parameterizations. I: The proposal, Atmos. Sci. Letters, 1, pp. 101-107, DOI: 10.1006/asle.2000.0022
- Neale, R. B. and Hoskins, B. J., 2000b, A standard test for AGCMs and their physical parameterizations. II: Results for The Met. Office Model, Atmos. Sci. Letters, 1, pp. 108-114, DOI: 10.1006/asle.2000.0024
More recent publications on the aqua-planet:
- Medeiros, B., et al,2008, Aquaplanets, climate sensitivity, and low clouds. Journal of Climate, DOI: 10.1175/2008JCLI1995.1
- Blackburn, M., et al. (2013) The Aqua-Planet Experiment (APE): CONTROL SST Simulation. Journal of the Meteorological Society of Japan, 91A. pp. 17-56. ISSN 2186-9057 doi: 10.2151/jmsj.2013-A02
Blackburn, M. and Hoskins, B. J. (2013) Context and aims of the Aqua-Planet Experiment. Journal of the Meteorological Society of Japan, 91A. pp. 1-15. ISSN 2186-9057 doi: 10.2151/jmsj.2013-A01
See also for example, the PCMDI Aqua-Planet website.
Please note that aqua-planet and other idealized configurations are a research tool and therefore may change between model versions.
For further assistance with idealised configurations of OpenIFS, please contact: openifs-support@ecmwf.int.
Configuration
Configuring OpenIFS for an aqua-planet simulation requires appropriate changes to:
- the model namelists
- initial files
- no changes to the code are required for the Neale & Hoskins cases; other configurations may require code changes.
Dynamical core
The model namelist NAMDYNCORE
controls the configuration for the model's dynamical core.
To enable the aqua-planet edit the fort.4
file (containing the input model namelist) and make sure the settings are as below. You may find this namelist is blank in your file as it does not need altering for normal forecasts, in which case add the following:
&NAMDYNCORE LDYNCORE=true, ! switches on idealized planet configurations. LAQUA=true, ! switches on idealized aqua planet. MSSTSCHEME=1, ! controls SST choice for aquaplanet following Neale & Hoskins (2000a) (see ifs/module/yomdyncore.F90 for more details). ! 1 = Control; 2 = Peaked; 3 = Flat; 4 = Qobs; 5 = Control5N; 6 = 1KEQ, chi=1.0; 7 = 3KEQ, chi=3.0; 8 = 3KW1, chi=3.0 /
The SST modifications can be further changed using the variables:
RLAMBDA0 : Longitude of maximum SST anomaly RLAMBDAD, RPHID: Half width in long/lat of SST anomaly RCHI : Maximum magnitude of SST anomaly
For more details of the SST configuration, see: ifs/phys_ec/gp_sstaqua.F90
. Modifications to the SST distributions can be made in this routine.
Mass conservation
Ensure that the mass conservation correction is enabled to prevent mass drifting in long integrations.
Edit namelist NAMDYN in the fort.4 file and add (or change) this variable:
&NAMDYN LMASCOR=true, ! if true, apply mass correction. /
Edit namelist NAMCT0 in fort.4 to set the mass correction frequency:
&NAMCT0 NFRMASSCON=24, ! frequency of mass conversation fixups (time-steps)
Model physics
Aqua-planet simulations normally use the full model physics and no changes are necessary in the NAEPHY namelist. It is included here for completeness.
If necessary edit the fort.4 file (containing the input model namelist) and make sure the settings are as below.
Note in this example, the model physics is turned on (enabled). By setting LEPHYS=false
, the model would run an aqua-planet with all the physics switched off.
For more information on these switches see the relevant modules in the model code: yoephy.F90
and yoewcou.F90
.
&NAEPHY LEPHYS=true, ! switch the full ECMWF physics package on/off. LEVDIF=true, ! turn on/off the vertical diffusion scheme. LESURF=true, ! turn on/off the interface surface processes. LECOND=true, ! turn on/off the large-scale condensation processes. LECUMF=true, ! turn on/off the mass-flux cumulus convection. LEPCLD=true, ! turn on/off the prognostic cloud scheme. LEEVAP=true, ! turn on/off the evaporation of precipitation LEVGEN=true, ! turn on/off Van Genuchten hydrology (with soil type field) LESSRO=true, ! turn on/off orographic (VIC-type) runoff LECURR=false, ! if true, ocean current boundary condition is used. LEGWDG=true, ! turn on/off gravity wave drag. LEGWWMS=true, ! turn on/off the Warner-McIntyre-Scinocca non-orographic gravity wave drag scheme. LEOZOC=true, ! turn on/off the climatological ozone. LEQNGT=true, ! turn on/off the negative humidity fixer. LERADI=true, ! turn on/off the radiation scheme. LERADS=true, ! turn on/off the interactive surface radiative properties. LESICE=true, ! turn on/off the interactive sea-ice processes. LEO3CH=false, ! turn on/off the ozone chemistry (for prognostic ozone). LEDCLD=true, ! turn on/off the diagnostic cloud scheme. LDUCTDIA=false, ! turn on/off computation and archiving of ducting diagnostics. LWCOU=false, ! turn on/off coupled wave model (n.b. always off for OpenIFS model version 38r1). LWCOU2W=false, ! turn on/off two-way interaction with the wave model (n.b. always off for OpenIFS model version 38r1). /
Initialisation
OpenIFS (and IFS) can be initialized either with real fields or idealized starting conditions.This is controlled both by the namelist switch N3DINI and by the code in the model.
It is crucial that the orography, surface pressure and land-sea-mask are set correctly (see below).
&NAMCT0 N3DINI=0, ! normally 0 to initialise the model from a real atmosphere, but see ifs/module/yomdyncore.F90 for other possibilities.
Orography, surface pressure and land-sea mask
In order to correctly run the aqua-planet in OpenIFS (and IFS), it is important that the orography field in the model is set to zero to ensure a flat surface. The surface pressure must also be adjusted to be consistent with the flat orography and the land-sea-mask in the model set to zero to indicate all sea-points.
There are two ways in which this can be achieved; either take an existing set of model initial files (the ICM*INI* files) and interpolate
Also see
ECMWF took part in the 2012 Dynamical Core Model Intercomparison Project (DCMIP). More information can be found here: https://www.earthsystemcog.org/projects/dcmip-2012/
Acknowledgements
OpenIFS would like to thank Sylvie Malardel (ECMWF) and Peter Bechtold (ECMWF) for their assistance in preparing this material
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