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Students: Lior Betzalel Michael Schwarcz Academic Advisor: Prof. Nathan Blaunstein.

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Presentation on theme: "Students: Lior Betzalel Michael Schwarcz Academic Advisor: Prof. Nathan Blaunstein."— Presentation transcript:

1 Students: Lior Betzalel Michael Schwarcz Academic Advisor: Prof. Nathan Blaunstein

2  Over the last years the demand for fast, accessible wireless communication has greatly increased.  The use of wireless communication in schools, coffee shops, buses and trains became very common.  Furthermore the need for reliable wireless communication aboard airplanes became very important.

3  There isn’t a full design of link budget for wireless communication in aircrafts accounting for the effects of atmospheric structures.  There isn’t a full prediction of fading phenomena in land-atmosphere communication links.  In order to reach a full link budget we have to take into account the environmental effects that have influence on the propagation of the radio signal and therefore on the quality of the channel.  We will focus on the tropospheric effects...

4  Tropospheric effects involve interactions between the radio waves and the lower layer of Earth’s atmosphere.  These Include effects of the gases composing the air and hydrometeors such as rain, clouds, fog, pollutions and turbulent structures.  The tropospheric effects influence on the signal are: Absorption, Scattering, Diffraction.

5  Absorption/Attenuation - occurs as the result of conversion from radio wave energy to thermal energy within an attenuating particle, such as a gas molecule and different hydrometeors. The absorption effects also rise with frequency of radio waves  Scattering - occurs from redirection of the radio waves into various directions. This process is frequency-dependent - wavelengths which are long when compared to the particles’ size will be only weakly scattered  Refraction - occurs as the result of propagation effects of layered quasi-homogeneous structure of the troposphere – it is simply the atmospheric bending of the radio path away from a straight line.

6  Analysis of effects of gaseous quasi-regular atmosphere on attenuation of radio signals passing the Land-Atmospheric Communication Channel (LACC).  Analysis of effects of hydrometeors (clouds and rain) on fading of radio signals passing the LACC.  Prediction of total path loss in the LACC.  Link budget design for the LACC.

7 In order to find the total path loss we used MATHEMATICA to simulate the channel. We can easily predict the free space loss from the well known equation:  Path loss = Free space loss + Gas loss + Additional path loss

8  Total attenuation in [dB]: where d is the link distance in [km] and r is a distance factor.  The ITU model was chosen to compute the attenuation due to rain, it depends only on frequency and rain rate at the region.  Specific attenution in [dB/km]: where a,b are regression coefficients which depends on frequency and R is the rainfall rate in [mm/hour].

9 ITU rain regions for Europe & Africa Specific attenuation versus frequency Due to rain at 1/5/10/20/50 [mm/hour] rainfall rate

10 The ITU provides a recommended model for fog or cloud attenuation that is valid up to 200GHz. The total cloud attenuation is: where: L is the total water density in kg/m² K1 is the specific attenuation coefficient in (dB/km)/(gr/m³) Θ is the elevation angle of the path

11  This graph represent the total cloud attenuation versus frequency for several elevation angles, using worst-case cloud density ( 1.6kg/m² ) f [GHz] Total cloud attenuation [dB] Θ = 5˚ Θ = 45˚ Θ = 15˚ Θ = 90˚  The effects are, of course, frequency-dependent.  It can be seen that cloud attenuation starts to become a consideration above about 10GHz Total cloud attenuation versus frequency at 5/15/45/90 deg elevation angle

12 Gaseous molecules in atmosphere may absorb energy from radio waves passing through them, thereby causing attenuation.  The Attenuation in the atmosphere over a path length d is given by: while : (Attenuation due to oxygen dB/Km)(Attenuation due to water vapor dB/Km)

13 for oxygen: for water vapor: f - is the frequency in GHz.  - is the water vapor density expressed in g/m3 (7.5 g/m ³ ). Oxygen Water vapor

14  For the simulation we used different height of transmitter and receiver antenna, and various frequencies.  for better results temperatures are taken into account by correction factors of –1.0% per  C   = 7.5 [g/m³]  p0= 1013 mb Total attenuation at 10/100/200 GHz 200 GHz 100 GHz 10 GHz

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16  Up to 20GHz attenuation is mostly due to free space loss. 10 [Km] 30 [Km] 50 [Km]

17  According to our results, upper bound for frequencies is for f< 20-25 GHz.  Up to f<20 [GHz] the main contributor to attenuation is free space loss.  At lower frequencies gaseous structures has the most influence on the total attenuation from all the atmospheric phenomena.  Because of the oxygen molecules, we can not use the frequency range of 57-64 GHz.  Investigating the affects of turbulent structures on fading phenomena and total link budget design in land-aircraft wireless communication channels.

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