Estimation of Water Vapour Attenuation And Rain Attenuation

K.Kalyana Srinivas Int. Journal of Engineering Research and Applications www.ijera.com
ISSN : 2248-9622, Vol. 5, Issue 4, ( Part -1) April 2015, pp.20-23
www.ijera.com 20 | P a g e
Estimation of Water Vapour Attenuation And Rain Attenuation
K.Kalyana Srinivas1
, T.Venkata Ramana2
Assistant professor, ECE, VNR-VJIET, Hyderabad, India 1
Associate professor 2
ECE,GITAM University,Visakhapatnam
Abstract
Attenuation due to and water vapour and rain can severely degrade the radio wave propagation at centimeter or
millimeter wavelengths. It restricts the path length of radio communication systems and limits the use of higher
frequencies for line-of-sight microwave links and satellite communications. The attenuation will pose a greater
problem to communication as the frequency of occurrence of heavy rain increases.In a tropical region, like
Malaysia, where excessive rainfall is a common phenomenon throughout the year, the knowledge of the rain
attenuation at the frequency of operation is extremely required for the design of a reliable terrestrial and earth
space communication link at a particular location.
I. ITU-R MODEL OF WATER VAPOUR
ATTENUATION:
The specific attenuation due to water vapor
[dB/Km] at ground level (pressure equal to 1013hpa)
and at temperature 15⁰ C can be approximatedthe
following equation for frequencies
below 350 HZ.
[1.1]
Where:
f = frequency, (GHz).
= water vapour density (g/ )
P = total air pressure (hPa)
= p/1013
T = temperature (C)
= 288/(T+273) = reciprocal temperature ( )
The water vapour value may not exceed the
saturation value at the temperature considered in the
equation 1.1, at a temperature of 15◦C the saturation
value is 12 g/m3
. For highervapour densities the
equation (1.1) must be corrected for higher
temperatures necessary to sustain such densities.
Equation (1.1) applies to the pressure range of
1013±50hpa with an accuracy of 15% over a
temperature range of -20◦C to 40◦C and a water
vapour density range from 0 to 50 gm/m3
.
As an approximation to Zenith path attenuation
(at sea level) may be obtained by multiplying the
specific attenuation given by the equation (1.1) by the
equivalent heights of water vapour given by (below
frequencies 350GHz).
( km) [1.2]
Where = Water Vapour equivalent height in the
window regions.
Equal to 1.6 km (clear weather) and 2.1 km (rain
conditions).
For a ground temperature different from 15◦C the
equivalent height of water vapour can be corrected by
0.1 %( clear weather) or 1 %( rain) per◦C.
The water vapour Zenith attenuation is then:
(dB) [1.3]
For elevation angles between 10◦and 90◦, the path
attenuation is obtained by using the cosecant law:
(dB) [1.4]
Where:
Θ =elevation angle.
For elevation angles between 0◦ and 10◦ a more
accurate formula must be used, modeling the real
length of the atmospheric path.
The ITU-R model was compared to an exact, but
computationally intensive, model like the MPM .The
data set used for this test contained 24 stations,
selected according to the criteria of geographical
coverage, data quality and availability, and covering
10 years of observations.
The MPM93 and ITU models have been used to
calculate the total attenuation in the absence of liquid
water, using the data from radio soundings and from
meteorological measurements .The relative error of
the gaseous attenuation calculated using the ITU-R
model, AITU, with respect to the attenuation calculated
using Liebe’s model and local radiosonde data, AMPM
, has been defined as:
(%) [1.5]
II. Results of water vapour attenuation
RESEARCH ARTICLE OPEN ACCESS

0 50 100 150 200 250 300 350
0
0.5
1
1.5
2
2.5
3
FREQUENCY (GHz)
SPECIFICATTENUATION(dB)
VARIATION OF SPECIFIC ATTENUATION WITH FREQUENCY
0 50 100 150 200 250 300 350
33
33.5
34
34.5
35
FREQUENCY(GHz)
EQUIVALENTHEIGHT(Km)
VARIATIONOFEQUIVALENTHEIGHTWITHFREQUENCY
0 50 100 150 200 250 300
0
20
40
60
80
100
FREQUENCY(GHZ)
WATERVAPOURATTENUATION(dB)
VARIATIONOFWATERVAPOURATTENUATIONWITHFREQUENCY
III. Calculation of rain attenuation and
variation of rain attenuation with
elevation angle and probability of
period of reference by using Itu-r
model:
Above about 10 GHz, rain attenuation becomes
the dominant impairment to wave propagation
through the troposphere. Extensive efforts have been
undertaken to measure and model long-term rain
attenuation statistics to aid communication system
design. Measured data is necessarily restricted to
specific locations and link parameters. For this
reason, models are most often used to predict the rain
attenuation expected for a given system specification.
In this section, two rain attenuation models are
presented that have performed well for many
diverse.regions and types of rain: the ITU-R Rain
Attenuation Model, and the DAH model. The models
are semi-empirical in nature, and they are based on
the relationship relating the specific
attenuation to the rain rate R (mm/hr)
through the parameters a and b. The models differ in
the methods used to convert the specific attenuation
to total attenuation over the path of the rain.
The ITU-R rain attenuation model is the
most widely accepted international method for the
prediction of rain effects on communications
systems. The model was first approved by the ITU in
1982 and is continuously updated, as rain attenuation
modeling is better understood and additional
information becomes available from global sources.
The ITU-R model has, since 1999, been based on the
DAH rain attenuation model, named for its authors
(Dissanayake, Allnutt, and Haidara). The DAH
model has been shown to be the best in overall
performance when compared with other models in
validation studies. The ITU-R states that the
modeling procedure estimates annual statistics of
path attenuation at a given location for frequencies up
to 55 GHz.
2)Steps for determining the expected
attenuation exceeded on a given slant-path
using itu-r (p.618-5) are as follows
The input parameters required for the ITU-R Rain
Model are:
 Latitude of the earth station –
 Altitude of the earth station above mean sea-
level –
 Point rainfall rate for 0.01% of an average year -
 Percentage exceedance probability for which
attenuation is to be calculated –
 Elevation angle –
 Frequency –
Step 1:Determine the rain rate for 0.01% of an
average year, .
The rainfall intensity corresponding to the
geographical area corresponding to coordinates of
our receiving station is must be found. 0.01%
corresponds to a signal availability of 99.99% of the
year, which means for 0.01% of the year the service
will be interrupted. This value is obtained from ITU-
R P.837 Recommendation paper.
Step 2:Determine the rain height at the ground station
of interest, .

Determination of the rain height, which according to
the ITU-R P.839 referenceis given by:
=4-0.075(Ø-36) km (2.1)
Step 3:Calculate the slant-path length,
The slant path length , , in the rain is:
Ls=( - )/sinθ (2.2)
where is the height above mean sea-level of the
earth station (km).
Step 4: Compute the path reduction factor,
The path adjustment factor is given by:
r0.01=1/(1+( cosθ/L0)) (2.3)
Where
L0=35eˆ(-0.015/R0.01 )km (2.4)
Step 5: Calculate the effective path length in the rain,
The effective path length in the rain is given by:
Le= r0.01 km (2.5)
Step 6:Calculate the specific attenuation,
Calculate the specific attenuation
using frequency and polarization
dependent coefficients and and the rainfall
rate , determined from step 1, by
using:
γ=k(R0.01)ˆα dB/km (2.6)
Step 7: The attenuation exceeded for 0.01% of an
average year, , is obtained from:
A0.01 = γ Le dB (2.7)
Step 8:The estimated attenuation to be exceeded for
other percentages of an average year, , in the
range 0.001% to 1.0%, is determined from the
attenuation to be exceeded for 0.01% for an average
year:
(2.8)
Note: The attenuation due to rain does not only
deteriorate the quality of the signal, it also increases
the atmospheric noise collected by the ground station
antenna, which is given by the equation:
(2.9)
Where:
= total attenuation due to rain (dB)
= effective temperature of the medium =
Variation of rain attenuation with elevation angle
Tabular Form Showing Variation Of Rain
Attenuation With Elevation Angle And
Probability Of Period Of Reference On
01.09.2010 :
IV. Conclusion
Radio wave propagation through the earth’s
atmosphere will experience reduction in signal level
due to the water vapour and rain parameter present
in the transmission path. Accurate estimation of radio
waves propagation impairments that affect link
quality and availability and determination of the
signal performance are essential to design a reliable
satellite or terrestrial communication systems and
earth terminals networks.
 /
prob%
0.0100 0.0160 0.0270 0.0450 0.0770
 = 10 44.9819 37.5756 30.4584 24.5691
19.3954
 = 20 30.0976 25.1419 20.3798 16.4393 12.9775
 = 30 23.1429
19.3324
15.6706 12.6406
9.9788
 = 40 19.2747 16.1011 13.0514 10.5278 8.3109
 = 50 16.9558 14.1640 11.4812 9.2613 7.3110
 = 60 15.5569 12.9954 10.5340 8.4972 6.7079
 = 70 14.7863 12.3517 10.0122 8.0763 6.3756

Thus the rain fading variation with changes in
the elevation angle has been carried out and is
observed to be decreased with increase in the
elevation angle. Thus the control of rain
attenuationthrough variation in angle of elevation has
been achieved.
References
[1] A comparision of measured rain
attenuation, rain rates and drop
sizedistributions Walther Åsen, Chris
Gibbins , Terje Tjelta
[2] Ku-Band Rain Attenuation Observations On
an earth-space path in the INDIAN Region
Animesh Maitra and Kaustav Chakravarty
[3] Rain Rate Statistics and fade distribution of
millimeter waves in indian continents
Saxena Poonam and T. K. Bandopadhyaya
Department of Electronics and Computer
Engineering Maulana Azad College of
Technology Regional Engineering College
Bhopal 462 007 India Received Received
December 27, 1997
[4] Rain Rate and rain attenuation prediction for
satellite communication in KU AND KA
bands Over Nigeria J. S. Ojo † and M. O.
Ajewole Department of Physics Federal
University of Technology Akure Ondo
State, Nigeria S. K. Sarkar National Physical
Laboratory Radio and Atmospheric Science
Division Dr. K. S Krishnan Road, New
Delhi 110012, India
[5] ITU-R: Draft new Recommendation ITU-R
P.[AFADE] – “Prediction method of fade
dynamics on Earth-space paths”, Document
P.3/BL/49, Radiocommunication Study
Group 3, December 2002.
[6] van de Kamp, M.M.J.L.: Climatic
Radiowave Propagation Models for the
design of Satellite Communication Systems,
Ph.D. Thesis, Eindhoven University of
Technology, ISBN 90-386-1700-3,
November 1999.

Estimation of Water Vapour Attenuation And Rain Attenuation

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Estimation of Water Vapour Attenuation And Rain Attenuation