Software Open Access
Martin Jucker; Edwin P. Gerber
&spectral_dynamics_nml specify_initial_conditions = .true.
Commit d4ae0aa: Possibility to use the navy topography as land mask. This works the same as
topography_option = 'interpolated', which looks for the navy topography data and interpolates on the MiMA grid. This does not require a land mask on the same grid as the simulation.
&simple_surface_nml land_opttion = 'interpolated' &topography_nml water_file = 'INPUT/navy_topography.data/navy_pctwater.data.nc'
Commit 70de265affc6dcd73454b7c99f05ff0eba288a26: Possibility to use an external file as land mask. Within the mask, any value > 0 is considered land.
&simple_surface_nml land_option = 'input', land_sea_mask_file = 'lmask_filename',
&simple_surface_nml land_option = 'zsurf', zsurf_cap_limit = 10.,
loncenterto a negative value. There is also the possibility for seasonal variation (positive parts of cosine) with cosine wave number
hphase. The wave number determines the length and recurrence of the heating during a calendar year, and the phase the months of the year when heating is active. The heating can be activated with the following input parameters:
&physics_driver_nml do_local_heating = .true., &local_heating_nml hamp = A [K/d], loncenter = lambda_0 [degrees] loncenter = lambda_0 [degrees], latwidth = delta_phi [degrees], latwidth = delta_phi [degrees], pcenter = p_0 [hPa], pwidth = delta_p [decades hPa], hk = wave_num , hphase = wave_phase [multiples of Pi] /
calendarattribute with value
360. However, the input files need to have a calendar
thirty_day_months, and don't understand the
360calendar. This is now fixed, which makes it easier to use previous output to force a new simulation
warmpool_phasefrom degrees to radians
warmpool_phasehas been switched to work as expected. Setting
warmpool_phase = xwill now have the warmpool peak at longitude