fogpl

RF signal attenuation due to fog and clouds

Syntax

L = fogpl(R,freq,T,den)

Description

L = fogpl(R,freq,T,den) returns attenuation, L, when signals propagate in fog or clouds. R represents the signal path length. freq represents the signal carrier frequency, T is the ambient temperature, and den specifies the liquid water density in the fog or cloud.

The fogpl function applies the International Telecommunication Union (ITU) cloud and fog attenuation model to calculate path loss of signals propagating through clouds and fog. See [1]. Fog and clouds are the same atmospheric phenomenon, differing only by height above ground. Both environments are parametrized by their liquid water density. Other model parameters include signal frequency and temperature. This function applies to cases when the signal path is contained entirely in a uniform fog or cloud environment. The liquid water density does not vary along the signal path. The attenuation model applies only for frequencies at 10–1000 GHz.

Examples

Attenuation in Cumulus Clouds

Compute the attenuation of signals propagating through a cloud that is 1 km long at 1000 meters altitude. Compute the attenuation for frequencies from 15 to 1000 GHz. A typical value for the cloud liquid water density is 0.5 $$g/m^3$$. Assume the atmospheric temperature at 1000 meters is ${20}^{\circ }$C.

R = 1000.0;
freq = [15:5:1000]*1e9;
T = 20.0;
lwd = 0.5;
L = fogpl(R,freq,T,lwd);

Plot the specific attenuation as a function of frequency. Specific attenuation is the attenuation or loss per kilometer.

loglog(freq/1e9,L)
grid
xlabel('Frequency (GHz)')
ylabel('Specific Attenuation (dB/km)')

Input Arguments

R — Signal path length in meters

positive real-valued scalar | M-by-1 nonnegative real-valued vector | 1-by-M nonnegative real-valued vector

Signal path length in meters, specified as a scalar or as an M-by-1 or 1-by-M vector of nonnegative real-values. Total attenuation is the specific attenuation multiplied by the path length.

Example: [1300.0,1400.0]

freq — Signal frequency in Hz

positive real-valued scalar | N-by-1 nonnegative real-valued column vector | 1-by-N nonnegative real-valued row vector

Signal frequency in Hz, specified as a positive real-valued scalar or as an N-by-1 nonnegative real-valued vector or 1-by-N nonnegative real-valued vector. Frequencies must lie in the range 10–1000 GHz.

Example: [14.0e9,15.0e9]

T — Ambient temperature in °C

real-valued scalar

Ambient temperature in fog or cloud, in °C, specified as a real-valued scalar.

Example: -10.0

den — Liquid water density in g/m³

nonnegative real-valued scalar

Liquid water density, specified as a nonnegative real-valued scalar. Typical values for liquid water density in fog range from approximately 0.05 g/m³ for medium fog to approximately 0.5 g/m³ for thick fog. For medium fog, visibility is about 300 meters. For heavy fog, visibility is about 50 meters. Cumulus cloud liquid water density is typically 0.5 g/m³.

Example: 0.01

Output Arguments

L — Signal attenuation in dB

real-valued M-by-N matrix

Signal attenuation in dB, returned as a real-valued M-by-N matrix. Each matrix row represents a different path where M is the number of paths. Each column represents a different frequency where N is the number of frequencies.

More About

Fog and Cloud Attenuation Model

This model calculates the attenuation of signals that propagate through fog or clouds.

Fog and cloud attenuation are due to the same atmospheric phenomenon. The ITU model, Recommendation ITU-R P.840-6: Attenuation due to clouds and fog is used. The model computes the specific attenuation (attenuation per kilometer), of a signal as a function of liquid water density, signal frequency, and temperature. The model applies to polarized and nonpolarized fields. The formula for specific attenuation at each frequency is

$${\gamma }_c=K_l\left(f\right)M,$$

where M is the liquid water density in gm/m³. The quantity K_l(f) is the specific attenuation coefficient and depends on frequency. The cloud and fog attenuation model is valid for frequencies 10–1000 GHz. Units for the specific attenuation coefficient are (dB/km)/(g/m³).

To compute the total attenuation for narrowband signals along a path, the function multiplies the specific attenuation by the path length R. Total attenuation is L_c = Rγ_c. You can also apply the attenuation model to wideband signals. First, divide the wideband signal into frequency subbands, and apply narrowband attenuation to each subband. Then, sum all attenuated subband signals into the total attenuated signal.

References

[1] Radiocommunication Sector of International Telecommunication Union. Recommendation ITU-R P.840-6: Attenuation due to clouds and fog. 2013.

Extended Capabilities

C/C++ Code Generation

Generate C and C++ code using MATLAB® Coder™.

Usage notes and limitations:

Does not support variable-size inputs.

Version History

Introduced in R2016a