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Workspace Method iyActiveSingleScat
Description
Simulation of radar/lidar, restricted to single scattering.
The WSM treats e.g. radar measurements of cloud and precipitation,
on the condition that multiple scattering can be ignored. Beside
the direct backsacttering, the two-way attenuation by gases and
particles is considered. Surface scattering is ignored.
The method could potentially be used for lidars, but multiple
scattering poses here a must stronger constrain for the range of
applications.
The method can be used with iyCalc, but not with yCalc. In the
later case, use instead yActive.
The method returns the backscattering for each point of ppath.
Several frequencies can be treated in parallel. The size of iy
is [ nf*np, stokes_dim ], where nf is the length of f_grid and
np is the number of path points. The data are stored in blocks
of [ np, stokes_dim ]. That is, all the results for the first
frequency occupy the np first rows of iy etc.
The polarisation state of the transmitted pulse is taken from
iy_transmitter_agenda. If the radar transmits several polarisations
at the same frequency, you need to handle this by using two frequencies
in f_grid, but these can be almost identical.
This method does not consider iy_unit. Unit changes are insted applied
in *yActive. The output of this method matches the option "1".
Transmission is handled in a slightly simplified manner for efficiency
reasons. First of all, the transmission matrix is assumed to be the same
in both directions between the sensor and the point of back-scattering.
This should in general be true, but exceptions could exist. The extinction
due to particles can also be scaled, which could be of interest when e.g.
characterising inversions.
Further, for Jacobian calculations the default is to assume that the
transmission is unaffected by the retrieval quantities. This is done
to save computational time, and should be a valid approximation for the
single-scattering conditions. Set *trans_in_jacobian* to 1 to obtain
the more accurate Jacobian.
Some auxiliary radiative transfer quantities can be obtained. Auxiliary
quantities are selected by iy_aux_vars and returned by iy_aux.
Valid choices for auxiliary data are:
"Radiative background": Index value flagging the radiative
background. The following coding is used: 0=space, 1=surface
and 2=cloudbox.
"Backscattering": The unattenuated backscattering. That is, as
iy but with no attenuated applied. Here all columns are filled.
"Optical depth": Scalar, total and two-way, optical depth between
sensor and each point of the propagation path. Calculated based on
the (1,1)-element of the transmission matrix (1-based indexing),
i.e. only fully valid for scalar RT.
"Particle extinction": As "Optical depth", but only with particle
attenuation included. That is, gas absorption is ignored.
If nothing else is stated, only the first column of iy_aux is filled,
i.e. the column matching Stokes element I, while remaing columns are
are filled with zeros.
Authors: Patrick Eriksson
Synopsis
iyActiveSingleScat( | iy, iy_aux, diy_dx, ppvar_p, ppvar_t, ppvar_nlte, ppvar_vmr, ppvar_wind, ppvar_mag, ppvar_pnd, ppvar_f, ppvar_trans_cumulat, stokes_dim, f_grid, atmosphere_dim, p_grid, t_field, nlte_field, vmr_field, abs_species, wind_u_field, wind_v_field, wind_w_field, mag_u_field, mag_v_field, mag_w_field, cloudbox_on, cloudbox_limits, pnd_field, dpnd_field_dx, scat_species, scat_data, scat_data_checked, iy_aux_vars, jacobian_do, jacobian_quantities, ppath, propmat_clearsky_agenda, water_p_eq_agenda,
iy_transmitter_agenda, iy_agenda_call1, iy_transmission, rte_alonglos_v, trans_in_jacobian, pext_scaling, t_interp_order ) |
Variables