- •Foreword
- •Policy on Intellectual Property Right (ipr)
- •A general purpose wide-range terrestrial propagation model in the frequency range 30 mHz to 50 gHz
- •Annex Wide-range propagation model Description of the calculation method
- •1 Introduction
- •1.1 Applicability
- •1.2 Reciprocity, and the designation of terminals
- •1.3 Iteration
- •1.4 Organization of the Recommendation
- •1.5 Style of description
- •2 Inputs
- •2.1 Terrain profile
- •2.2 Other inputs
- •Other inputs
- •2.3 Constants
- •Constants
- •2.4 Integral digital products
- •Digital products
- •3 Preliminary calculations
- •Principal parameters
- •3.1 Limited percentage times
- •3.2 Path length, intermediate points, and fraction over sea
- •3.3 Antenna altitudes and path inclination
- •3.4 Climatic parameters
- •3.4.1 Refractivity in the lowest 1 km
- •3.4.2 Refractivity in the lowest 65 m
- •3.4.3 Precipitation parameters
- •3.5 Effective Earth-radius geometry
- •3.6 Wavelength
- •3.7 Path classification and terminal horizon parameters
- •Case 1. Path is LoS
- •Case 2. Path is nLoS
- •Continue for both cases
- •3.8 Effective heights and path roughness parameter
- •3.9 Tropospheric-scatter path segments
- •3.10 Gaseous absorption on surface paths
- •3.11 Free-space basic transmission loss
- •3.12 Knife-edge diffraction loss
- •4 Obtaining predictions for the principal sub-models
- •5 Combining sub-model results
- •5.1 Combining sub-models 1 and 2
- •5.3 Combining sub-models within a Monte-Carlo simulator
- •Appendix a Diffraction loss a.1 Introduction
- •A.2 Spherical-Earth diffraction loss
- •A.3 First-term spherical-Earth diffraction loss
- •Start of calculation to be performed twice
- •A.4 Bullington diffraction loss for actual profile
- •Case 1. Path is LoS for effective Earth curvature not exceeded for p% time
- •Case 2. Path is nLoS for effective Earth curvature not exceeded for p% time
- •A.5 Bullington diffraction loss for a notional smooth profile
- •Case 1. Path is LoS for effective Earth radius exceeded for p% time
- •Case 2. Path is nLoS for effective Earth radius exceeded for p% time
- •Appendix b Clear-air enhancements and fading b.1 Introduction
- •B.2 Characterize multi-path activity
- •For LoS path:
- •For nLoS path:
- •B.3 Calculation of the notional zero-fade annual percentage time
- •B.4 Percentage time a given clear-air fade level is exceeded on a surface path
- •B.5 Percentage time a given clear-air fade level is exceeded on a troposcatter path
- •Appendix c Precipitation fading c.1 Introduction
- •C.2 Preliminary calculations
- •Probability distribution of rain height
- •C.3 Percentage time a given precipitation fade level is exceeded
- •C.4 Melting-layer model
- •Factor (abscissa) plotted against relative height h (ordinate)
- •C.5 Path-averaged multiplier
- •Example of path geometry in relation to melting layer slices
- •Appendix d Anomalous/layer-reflection model
- •D.1 Characterize the radio-climatic zones dominating the path
- •Radio-climatic zones
- •Large bodies of inland water
- •Large inland lake or wet-land areas
- •D.2 Point incidence of ducting
- •D.3 Site-shielding losses with respect to the anomalous propagation mechanism
- •D.4 Over-sea surface duct coupling corrections
- •D.5 Total coupling loss to the anomalous propagation mechanism
- •D.6 Angular-distance dependent loss
- •D.7 Distance and time-dependent loss
- •D.8 Basic transmission loss associated with ducting
- •Appendix e Troposcatter e.1 Introduction
- •E.2 Climatic classification
- •Climatic zones
- •Meteorological and atmospheric structure parameters
- •E.3 Calculation of troposcatter basic transmission loss
- •Appendix f Attenuation due to gaseous absorption f.1 Introduction
- •F.2 Gaseous absorption for surface path
- •F.3 Gaseous absorption for a troposcatter path
- •F.4 Gaseous absorption for terminal/common-volume troposcatter path
- •F.5 Water-vapour density in rain
- •F.6 Specific sea-level attenuations
- •Appendix g Sporadic-e propagation
- •G.1 Derivation of foEs
- •Conditions for setting p1 and p2
- •G.4 Basic transmission loss
- •Appendix h Great-circle path calculations h.1 Introduction
- •H.2 Path length and bearing
- •H.3 Calculation of intermediate path point
- •Appendix I Iterative procedure to invert a cumulative distribution function
- •I.1 Introduction
- •I.2 Iteration method
- •Stage 1: setting the search range
- •Stage 2: binary search
- •Appendix j Structure of the wide-range propagation model j.1 Introduction
- •J.2 Combining the sub-models
Continue for both cases
Calculate the horizon elevation angles limited such that they are positive.
mrad (3.7.11a)
mrad (3.7.11b)
3.8 Effective heights and path roughness parameter
The effective transmitter and receiver heights above terrain are calculated relative to a smooth surface fitted to the profile.
Calculate the initial provisional values for the heights of the smooth surface at the transmitter and receiver ends of the path, as follows:
(3.8.1)
(3.8.2)
masl (3.8.3a)
masl (3.8.3b)
If
,
re-evaluate hstip
using:
masl (3.8.4a)
If
,
re-evaluate hsrip
using:
masl (3.8.4b)
The slope of the least-squares regression fit is given by m:
m/km (3.8.5)
The effective heights of the transmitter and receiver antennas above the smooth surface are now given by:
m (3.8.6a)
m (3.8.6b)
Calculate the path roughness parameter given by:
m (3.8.7)
where the profile index i takes all values from ilt to ilr inclusive. The path roughness parameter, hm, is used in Appendix D.
Further calculations involving the smooth surface are now required for the obstruction gain correction described in Appendix A.
Find the highest obstruction height above the straight-line path from transmitter to receiver hobs, and the horizon elevation angles αobt, αobr, all based on flat-Earth geometry, according to:
m (3.8.8a)
mrad (3.8.8b)
mrad (3.8.8c)
where:
m (3.8.8d)
and the profile index i takes values from 2 to (n – 1).
Calculate provisional values for the heights of the smooth surface at the transmitter and receiver ends of the path:
If hobs is less than or equal to zero, then:
masl (3.8.9a)
masl (3.8.9b)
otherwise:
masl (3.8.9c)
masl (3.8.9d)
where:
(3.8.9e)
(3.8.9f)
Calculate the final values for the heights of the smooth surface at the transmitter and receiver ends of the path:
If hst is greater than h1 then:
masl (3.8.10a)
If hsr is greater than hn then:
masl (3.8.10b)
Calculate the effective antenna heights for the spherical-earth and the smooth-profile version of the Bullington model (described in §§ A.2 and A.5, respectively) given by:
masl (3.8.11a)
masl (3.8.11b)
3.9 Tropospheric-scatter path segments
For the tropospheric-scatter model described in Appendix E, calculate the horizontal path lengths from transmitter to common volume and common volume to receiver:
km (3.9.1a)
Limit dtcv such that 0 ≤ dtcv ≤ d:
km (3.9.1b)
where d, e, tpos, and rpos all appear in Table 3.1.
Calculate the longitude and latitude of the common volume, cve and cvn, from the transmitter and receiver longitudes and latitudes, as given in Table 2.2.1, using the great circle path method of Appendix H by setting dpnt = dtcv in equation (H.3.1).
Calculate the height of the troposcatter common volume given by:
masl (3.9.2)
Calculate the longitude and latitude of the mid-points of the path segments from transmitter to common volume and from receiver to common volume, tcve, tcvn, and rcve, rcvn. These can be obtained using the great circle path method of Appendix H by setting dpnt = 0.5 dtcv and dpnt = d − 0.5 drcv in equation (H.3.1), respectively.
