By: Oleksandr (Sasha) Huziy, Luis Duarte
Experimental setup and driving data
Seasonal climatologies
SST and SSH timeseries
Vertical structure of lake temperature
Some results of a 30 year simulatoin (1958-1987)
Questions
Horizontal resolution: 0.1 degree, \(170\times90\) gridpoints (Rotated lat/lon projection)
35 vertical levels with partial steps at the bottom. Level thickness gradually increases from 25 cm at the surface to 30 m at the bottom
Time step: 1 hour (Scaled accordingly following Dupont et al 2012, who used 600 s at 2km horizontal resolution)
Model version: 3.4
Surface pressure gradient term is treated by filtering EGWs.
(Roullet and Madec 2000, preprocessor key: key_dynspg_flt)
Fresh water fluxes are corrected in a way that mean annual fresh water flux is 0.
\[E-P-R = 0\]
| key_trabbl | key_lim2 | key_ldfslp |
| key_dynldf_c3d | key_zdftke | key_zdfddm |
| key_dynspg_flt | key_traldf_c2d |
TVD scheme used for tracer advection
lateral diffusion scheme for tracers
laplacian operator
rn_aht_0 = 2.5 ! horizontal eddy diffusivity for tracers \([{\rm m^2/s}]\)
lateral diffusion on momentum
laplacian operator
rn_ahm_0_lap = 50.0 ! horizontal laplacian eddy viscosity \([{\rm m^2/s}]\)
DFS5.2 (Drakkar Forcing Set) available for 1958-2012
Variables:
wind components at 10 m, 3-hourly
temperature and humidity of air at 2m, 3-hourly
Longwave and shortwave radiation fluxes, daily
Snowrate and precipitation, daily














