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Workspace Method pnd_fieldSetup
Description
Calculation of pnd_field using ScatteringMetaData and massdensity_field.
The WSM first checks if cloudbox is empty. If so, the pnd calculations
will be skipped.
The cloudbox_limits are used to determine the p, lat and lon size for
the pnd_field tensor.
Currently there are three particle size distribution parameterisations implemented:
1. MH97 for ice particles. Using a first-order gamma distribution for particles
smaller than 100 microns (melted diameter) and a lognormal distribution for
particles bigger 100 microns. Values from both modes are cumulative.
See internal function 'IWCtopnd_MH97' for implementation/units/output.
(src.: McFarquhar G.M., Heymsfield A.J., 1997)
2. H11 for ice particles and precepitating ice (snow). H11 in NOT dependent
on massdensity of ice/snow, but on atmospheric temperature.
The PSD is scaled to the current IWC/Snow density in an additional step.
See internal function 'pnd_H11' and 'scale_H11' for implementation/units/output.
(src.: Heymsfield A.J., 2011, not published yet)
3. Gamma distribution for liquid cloud particles.
See internal function 'LWCtopnd' for implementation/units/output.
(src.: Deirmendjian D., 1963 and Hess M., et al 1998)
According to the selection criteria in part_species, the first specified
psd parametrisation is selected together with all particles of specified phase
and size. Then pnd calculations are performed on all levels inside the cloudbox.
The massdensity_field input weights the pnds by the amount of scattering
particles in each gridbox inside the cloudbox. Where massdensity_field is zero,
the pnd_field will be zero as well.
Subsequently the pnd values get written to pnd_field.
Now the next selection criteria string in part_species is used to repeat
the process.The new pnd values will be appended to the existing pnd_field.
And so on...
NOTE: the order of scattering particle profiles in massdensity_field is HARD WIRED!
Authors: Daniel Kreyling
Synopsis
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