atten_map_fast#
- pycraf.pathprof.atten_map_fast(freq, temperature, pressure, h_tg, h_rg, timepercent, hprof_data, polarization=0, version=16, base_water_density=<Quantity 7.5 g / m3>)[source]#
Calculate attenuation maps using a fast method.
- Parameters:
- freq
Quantity Frequency of radiation [GHz]
- temperature
Quantity Temperature (K)
- pressure
Quantity Pressure (hPa)
- h_tg, h_rg
Quantity Transmitter/receiver heights over ground [m]
- timepercent
Quantity Time percentage [%] (maximal 50%)
- hprof_data
dict, dict-like Dictionary with height profiles and auxillary maps of dimension
(my, mx)as calculated withheight_map_data.- polarization
int, optional Polarization (default: 0) Allowed values are: 0 - horizontal, 1 - vertical
- version
int, optional ITU-R Rec. P.452 version. Allowed values are: 14, 16
- base_water_density
Quantity, optional For atmospheric attenuation, the water vapor content plays a role. In Rec. ITU-R P.452, Eq. (9a), the water content is variable (depending on the fraction of the path over the water). However, the base level is set to \(7.5~\mathrm{g}/\mathrm{m}^3\). For extraordinarily dry places, which are often used for radio astronomy, this value can be too high. (Default: 7.5 g / m^3)
- freq
- Returns:
- results
dict Results of the path attenuation calculation. Each entry in the dictionary is a 2D
ndarraycontaining the associated value for the map of dimension(my, mx). The following entries are contained:L_b0p- Free-space loss including focussing effects(for p% of time) [dB]
L_bd- Basic transmission loss associated with diffractionnot exceeded for p% time [dB]; L_bd = L_b0p + L_dp
L_bs- Tropospheric scatter loss [dB]L_ba- Ducting/layer reflection loss [dB]L_b- Complete path propagation loss [dB]L_b_corr- As L_b but with clutter correction [dB]eps_pt- Elevation angle of paths w.r.t. Tx [deg]eps_pr- Elevation angle of paths w.r.t. Rx [deg]d_lt- Distance to horizon w.r.t. Tx [km]d_lr- Distance to horizon w.r.t. Rx [km]path_type- Path type (0 - LoS, 1 - Trans-horizon)
- results
Notes
The diffraction-loss algorithm was changed between ITU-R P.452 version 14 and 15. The former used a Deygout method, the new one is based on a Bullington calculation with correction terms.
In future versions, more entries may be added to the results dictionary.