ece 5233 satellite communications prepared by: dr. ivica kostanic lecture 15: secondary atmospheric...

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ECE 5233 Satellite Communications Prepared by: Dr. Ivica Kostanic Lecture 15: Secondary atmospheric losses effects (Section 8.5-8.7) Spring 2011

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Page 1: ECE 5233 Satellite Communications Prepared by: Dr. Ivica Kostanic Lecture 15: Secondary atmospheric losses effects (Section 8.5-8.7) Spring 2011

ECE 5233 Satellite Communications

Prepared by:

Dr. Ivica Kostanic

Lecture 15: Secondary atmospheric losses effects

(Section 8.5-8.7)

Spring 2011

Page 2: ECE 5233 Satellite Communications Prepared by: Dr. Ivica Kostanic Lecture 15: Secondary atmospheric losses effects (Section 8.5-8.7) Spring 2011

Florida Institute of technologies

Page 2

Tropospheric scintillation (refractive effects)

Ionospheric scintillation

Faraday rotation (polarization loss)

Rain and ice crystal depolarization

Propagation impairment counter measures

Outline

Important note: Slides present summary of the results. Detailed derivations are given in notes.

Page 3: ECE 5233 Satellite Communications Prepared by: Dr. Ivica Kostanic Lecture 15: Secondary atmospheric losses effects (Section 8.5-8.7) Spring 2011

Florida Institute of technologies

Tropospheric scintillation

Losses associated with variations of the atmosphere close to the ground

Due to weather conditions (heating and cooling), the refractive index of the atmosphere changes

Change of refractive index changes the direction of signal propagation

Change of direction of arrival is “modulated” by antenna pattern -> causes signal fluctuation

Scintillation is more pronounced for higher frequencies

Scintillation does not cause depolarization

At low elevation angles (< 10 deg), scintillation may cause path loss behavior similar to terrestrial

multipath fading

Page 3

Physical explanation of atmospheric scintillation

Page 4: ECE 5233 Satellite Communications Prepared by: Dr. Ivica Kostanic Lecture 15: Secondary atmospheric losses effects (Section 8.5-8.7) Spring 2011

Florida Institute of technologies

Tropospheric scintillation - modeling

Scintillation losses depend ono Operating frequencyo Climateo Satellite elevation o Antenna beam

Modeled as additional random path loss Mitigation approaches

o Fade margino Error control coding

Page 4

Example. Scintilation losses may be modeled as a random variable with a PDF given by:

0,0

0,2

exp2

12

2

2

2

l

ll

lf

Where s is 1.2 dB.

Estimate required design margin to guarantee reliability of 90% with respect to the scintillation losses.

Answer: 2dB

0 20 40 60 80 100 120 140 160 180 200-2.5

-2

-1.5

-1

-0.5

0

RS

L at

tenu

atio

n du

e to

sci

ntila

tion

time

Example of scintilation losses

Page 5: ECE 5233 Satellite Communications Prepared by: Dr. Ivica Kostanic Lecture 15: Secondary atmospheric losses effects (Section 8.5-8.7) Spring 2011

Florida Institute of technologies

Ionospheric scintillation

Energy from the sun causes variations to total electron content in the ionosphere

Typical range 1018 during day, 1016 during night

At the local sunsets/sunrises there are rapid changes of concentration that cause changes of magnitude and phase of radio waves

The changes are further modulated by the antenna pattern

The net result are variations of the RSL at sunset and down

Magnitude of the ionosphere scintillation varies with sun activity

Page 5

Page 6: ECE 5233 Satellite Communications Prepared by: Dr. Ivica Kostanic Lecture 15: Secondary atmospheric losses effects (Section 8.5-8.7) Spring 2011

Florida Institute of technologies

Faraday rotation – polarization loss

Radio waves propagate through Earths magnetic field

Magnetic field changes the polarization of the wave

Two negative effects:

o Increased losses due to polarization mismatch between RX antenna and radio wave

o Increased adjacent channel interference

The rotation angle depends on

o Length of the path through ionosphere

o Concentration of ionosphere charges

o Operating frequency

The effects becomes smaller with frequency increase

Page 6

Illustration of Faraday’s rotation

Magnetic field of the Earth

cotlog20XPD

Estimation of losses

b – Faraday’s rotation angle

Page 7: ECE 5233 Satellite Communications Prepared by: Dr. Ivica Kostanic Lecture 15: Secondary atmospheric losses effects (Section 8.5-8.7) Spring 2011

Florida Institute of technologies

Depolarization losses Rain affects two polarizations in a

different way

Rain attenuates horizontal component more than the vertical one

If a linearly polarized wave has a general orientation w.r.t. rainfall, the wave tilts towards vertical polarization

In a non-wind condition, raindrops have elliptical shape with minor axis in the vertical direction

In wind-conditions, the orientation of the raindrop ellipse changes – canting angle

Page 7

Definition of canting angle

Page 8: ECE 5233 Satellite Communications Prepared by: Dr. Ivica Kostanic Lecture 15: Secondary atmospheric losses effects (Section 8.5-8.7) Spring 2011

Florida Institute of technologies

Tilt angle

Due to geometry – vertically polarized transmission from the satellite is received at a tilted angle

Tilt depends on the earth station location

May be estimated using

Page 8

ESe llL sin/tanarctan

Le – latitude of earth station

le – longitude of earth station

ls – longituide of su-satellite point

Page 9: ECE 5233 Satellite Communications Prepared by: Dr. Ivica Kostanic Lecture 15: Secondary atmospheric losses effects (Section 8.5-8.7) Spring 2011

Florida Institute of technologies

Prediction of XPD losses (ITU-R P.618-6)

Algorithm provided in the text book

Consists of eight steps

Review with students

Page 9

Page 10: ECE 5233 Satellite Communications Prepared by: Dr. Ivica Kostanic Lecture 15: Secondary atmospheric losses effects (Section 8.5-8.7) Spring 2011

Florida Institute of technologies

Propagation impairment counter measures

Adaptive power control

Diversity reception/transmission

Signal processing (on-board processing)

Adaptive modulation and coding

Adaptive power control

o TX power adjusted to compensate for losses

o Power control usually operates in closed loop

Measurement at the RX compared against threshold

If the signal falls below threshold – feedback is sent to TX

Page 10

Diversity reception/transmission

Used in high capacity FSS hubs

The signal is received/transmitted from multiple location on the ground

Probability of simultaneous fades is reduced with separation between earth stations

Signal (on-board processing)

Used in VSAT systems

Uplink demodulated to the baseband and rerouted towards different antenna beams

Each beam examined independently where rate, power, coding and modulation may be varied depending in the path loss

Page 11: ECE 5233 Satellite Communications Prepared by: Dr. Ivica Kostanic Lecture 15: Secondary atmospheric losses effects (Section 8.5-8.7) Spring 2011

Florida Institute of technologies

Propagation impairment counter measures

Adaptive modulation and coding

o Idea: Modulation and coding changes as a function of SNR

o The lower SNR – more robust modulation and coding

o The lower SNR – lower data rate

o Link designed for availability at the worst conditions (at the lowest rate)

o If the conditions are better than worst case – higher throughput is achieved

Page 11AMC example for DVBS-2 standard