Ignore:
Timestamp:
Oct 26, 2015 4:17:44 PM (9 years ago)
Author:
maronga
Message:

various bugfixes and modifications of the atmosphere-land-surface-radiation interaction. Completely re-written routine to calculate surface fluxes (surface_layer_fluxes.f90) that replaces prandtl_fluxes. Minor formatting corrections and renamings

File:
1 edited

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  • palm/trunk/SOURCE/lpm_init.f90

    r1686 r1691  
    1414! PALM. If not, see <http://www.gnu.org/licenses/>.
    1515!
    16 ! Copyright 1997-2014 Leibniz Universitaet Hannover
     16! Copyright 1997-2015 Leibniz Universitaet Hannover
    1717!--------------------------------------------------------------------------------!
    1818!
    1919! Current revisions:
    2020! -----------------
    21 !
     21! Renamed prandtl_layer to constant_flux_layer.
    2222!
    2323! Former revisions:
     
    100100
    101101    USE control_parameters,                                                    &
    102         ONLY:  cloud_droplets, current_timestep_number, dz,                    &
    103                initializing_actions, message_string, netcdf_data_format,       &
    104                ocean, prandtl_layer, simulated_time
     102        ONLY:  cloud_droplets, constant_flux_layer, current_timestep_number,   &
     103               dz, initializing_actions, message_string, netcdf_data_format,   &
     104               ocean, simulated_time
    105105
    106106    USE dvrp_variables,                                                        &
     
    295295!-- To obtain exact height levels of particles, linear interpolation is applied
    296296!-- (see lpm_advec.f90).
    297     IF ( prandtl_layer )  THEN
     297    IF ( constant_flux_layer )  THEN
    298298       
    299299       ALLOCATE ( log_z_z0(0:number_of_sublayers) )
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