Open WL Archief (OWA)

1.

(1) subtraction of the standard stratification and introduction of departures of temperature, T′, salinity, S′, density,ϱ′ and pressure, p′, from their standard values;

2.

(2) suitable transformation of coordinates and variables, which makes the energy equation more compact and the total “available energy” conserved, if the forcing and dissipation are neglected and some small reasonable modifications are introduced;

3.

(3) perfect conservation of total available energy (under the conditions mentioned in point 2) and no computational mode in the finite-difference scheme;

4.

(4) introduction of “flexible coefficients” and a modified splitting method for flexibility of computation and acceleration of convergence in time-integration.

A four-level version of such oceanic GCM has been applied to simulations of annual mean circulations in the World Ocean and the annual cycle in the Pacific Ocean under the forcings of the climatological surface wind stress, surface heat flux and air pressure. More than 60 years integration has been made and the results show successful simulations of most observed large-scale features of the annual mean and annual cycle of currents, temperature, sea surface elevation and other features in the Pacific Ocean.