Lorenz95 model¶
Introduction¶
The Lorenz95 model is an application of the Lorenz (1996) chaotic dynamics. This model is governed by I equations:
where i=1,2,…,I, with cyclic boundary conditions, and the constant F is independent of i. The variables of this model may be thought of as values of some atmospheric quantity in I locations of a latitude circle. The so-called 40-variable version of this model assumes I=40, with i=1,2,…,40, which implies to the cyclic boundary conditions being defined as: x0=x40; x−1=x39; and, x41=x1.
YAML parameters¶
The configurable Lorenz95 model parameters are as follows:
geometry
: define grid parametersresol
: define the number of variables I
model
: define model parametersf
: define the constant Fname
: define the modeltstep
: define the time step
forecast length
: define the length of the forecastinitial condition
: define initial condition parametersdate
: define the initial date to issue a forecastfilename
: define the name of the file to be used as initial condition
output
: define output parametersdatadir
: define the directory to save filesdate
: define the output dateexp
: define an experiment identificationfrequency
: define the frequency to save output filestype
: define the type of output file
Note
Although the YAML parameters are defined using real time quantities for dates and time intervals (e.g., date
, tstep
, forecast length
, frequency
), the actual equivalence between real time and the time considered for this model is defined as a combination of the number of variables I and the constant F. See details in Lorenz (1996) and Lorenz and Emanuel (1998).
References¶
Lorenz, E. N., 1996: Predictability: a problem partly solved. Seminar on Predictability, 4-8 September 1995, volume 1, pages 1–18, European Centre for Medium Range Weather Forecasts, Reading, England. ECMWF.
Lorenz, E. N. and Emanuel, K. A. (1998). Optimal sites for supplementary weather observations: Simulation with a small model. J. Atmos. Sci., 55(3):399–414.