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Workspace Method DisortCalcClearsky
Description
Interface to DISORT for running clear-sky cases. The method runs DISORT with pnd_field set to zero. Note that this version returns spectral_radiance_field, i.e. the solution for the full atmosphere. The standard DisortCalc only returns the field inside the cloudbox.
Authors: Patrick Eriksson
Synopsis
DisortCalcClearsky( | spectral_radiance_field, atmfields_checked, atmgeom_checked, propmat_clearsky_agenda, atmosphere_dim, t_field, z_field, vmr_field, p_grid, f_grid, za_grid, stokes_dim, z_surface, surface_skin_t, surface_scalar_reflectivity, nstreams, quiet ) |
Variables
OUT | spectral_radiance_field | (Tensor7) | Spectral radiance field. |
IN | atmfields_checked | (Index) | OK-flag for atmospheric grids and (physical) fields. |
IN | atmgeom_checked | (Index) | OK-flag for the geometry of the model atmosphere. |
IN | propmat_clearsky_agenda | (Agenda) | Agenda calculating the absorption coefficient matrices. |
IN | atmosphere_dim | (Index) | The atmospheric dimensionality (1-3). |
IN | t_field | (Tensor3) | The field of atmospheric temperatures. |
IN | z_field | (Tensor3) | The field of geometrical altitudes. |
IN | vmr_field | (Tensor4) | VMR field. |
IN | p_grid | (Vector) | The pressure grid. |
IN | f_grid | (Vector) | The frequency grid for monochromatic pencil beam calculations. |
IN | za_grid | (Vector) | Zenith angle grid. |
IN | stokes_dim | (Index) | The dimensionality of the Stokes vector (1-4). |
IN | z_surface | (Matrix) | The surface altitude. |
IN | surface_skin_t | (Numeric) | Surface skin temperature. |
IN | surface_scalar_reflectivity | (Vector) | Surface reflectivity, assuming it can be described as a scalar value. |
GIN | nstreams | (Index, Default: 8) | Number of polar angle directions (streams) in DISORT solution (must be an even number). |
GIN | quiet | (Index, Default: 0) | Silence C Disort warnings. |