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Aristotle University of Thessaloniki Aristotle University of Thessaloniki Department of Geodesy and Surveying Department of Geodesy and Surveying A. Dermanis A. Dermanis Signals and Spectral Methods in Geoinformatics Signals and Spectral Methods in Geoinformatics Lecture 6: Signals Transmission Signals and Spectral Methods in Geoinformatics

Lecture 6: Signals Transmission

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Signals and Spectral Methods in Geoinformatics. Lecture 6: Signals Transmission. Signal transmission. 1 MODULATION : Placing the signal on a monochromatic signal ( carrier frequency ). 2 TRANSMISSION. 3 RECEPTION. 4 DEMODULATION : Signal recovery ( removal of carrier frequency ). - PowerPoint PPT Presentation

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Page 1: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

Lecture 6:Signals Transmission

Signals and Spectral Methodsin Geoinformatics

Page 2: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

Signal transmission

1 MODULATION : Placing the signal on a monochromatic signal (carrier frequency)

2 TRANSMISSION

3 RECEPTION

4 DEMODULATION : Signal recovery (removal of carrier frequency)

Page 3: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

modulation

Page 4: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

modulation

Modulation = placement of signal m(t) on a monochromatic signal xC(t) = aC cos(φ0C+ωCt) with carrier frequency ωC

Page 5: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

modulation

Modulation = placement of signal m(t) on a monochromatic signal xC(t) = aC cos(φ0C+ωCt) with carrier frequency ωC

Α. Amplitude modulation (general form) : )cos()()( 0 ttatx CC

Page 6: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

modulation

Modulation = placement of signal m(t) on a monochromatic signal xC(t) = aC cos(φ0C+ωCt) with carrier frequency ωC

Α. Amplitude modulation (general form) : )cos()()( 0 ttatx CC

m(t)

Page 7: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

modulation

Modulation = placement of signal m(t) on a monochromatic signal xC(t) = aC cos(φ0C+ωCt) with carrier frequency ωC

Α. Amplitude modulation (general form) :

Β. Angle modulation (general form) :

)cos()()( 0 ttatx CC

)](cos[)( 0 ttatx CCC

m(t)

Page 8: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

modulation

Modulation = placement of signal m(t) on a monochromatic signal xC(t) = aC cos(φ0C+ωCt) with carrier frequency ωC

Α. Amplitude modulation (general form) :

Β. Angle modulation (general form) :

)cos()()( 0 ttatx CC

)](cos[)( 0 ttatx CCC

m(t)

Page 9: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

modulation

Modulation = placement of signal m(t) on a monochromatic signal xC(t) = aC cos(φ0C+ωCt) with carrier frequency ωC

Α. Amplitude modulation (general form) :

Β. Angle modulation (general form) :

)cos()()( 0 ttatx CC

)](cos[)( 0 ttatx CCC

Α. AM = Amplitude Modulation :

m(t)

Page 10: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

modulation

Modulation = placement of signal m(t) on a monochromatic signal xC(t) = aC cos(φ0C+ωCt) with carrier frequency ωC

Α. Amplitude modulation (general form) :

Β. Angle modulation (general form) :

)cos()()( 0 ttatx CC

)](cos[)( 0 ttatx CCC

Α. AM = Amplitude Modulation :

)()( tmkAta a

m(t)

Page 11: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

modulation

Modulation = placement of signal m(t) on a monochromatic signal xC(t) = aC cos(φ0C+ωCt) with carrier frequency ωC

Α. Amplitude modulation (general form) :

Β. Angle modulation (general form) :

)cos()()( 0 ttatx CC

)](cos[)( 0 ttatx CCC

Α. AM = Amplitude Modulation :

)()( tmkAta a )cos()]([)( 0 ttmkAtx CCa

m(t)

Page 12: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

modulation

Modulation = placement of signal m(t) on a monochromatic signal xC(t) = aC cos(φ0C+ωCt) with carrier frequency ωC

Α. Amplitude modulation (general form) :

Β. Angle modulation (general form) :

)cos()()( 0 ttatx CC

)](cos[)( 0 ttatx CCC

Α. AM = Amplitude Modulation :

)()( tmkAta a )cos()]([)( 0 ttmkAtx CCa

Β. Angle modulation

m(t)

Page 13: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

modulation

Modulation = placement of signal m(t) on a monochromatic signal xC(t) = aC cos(φ0C+ωCt) with carrier frequency ωC

Α. Amplitude modulation (general form) :

Β. Angle modulation (general form) :

)cos()()( 0 ttatx CC

)](cos[)( 0 ttatx CCC

Α. AM = Amplitude Modulation :

)()( tmkAta a )cos()]([)( 0 ttmkAtx CCa

Β. Angle modulation

Β1. PM = Phase Modulation :

Β2. FM = Frequency Modulation :

m(t)

Page 14: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

modulation

Modulation = placement of signal m(t) on a monochromatic signal xC(t) = aC cos(φ0C+ωCt) with carrier frequency ωC

Α. Amplitude modulation (general form) :

Β. Angle modulation (general form) :

)cos()()( 0 ttatx CC

)](cos[)( 0 ttatx CCC

Α. AM = Amplitude Modulation :

)()( tmkAta a )cos()]([)( 0 ttmkAtx CCa

Β. Angle modulation

Β1. PM = Phase Modulation :

Β2. FM = Frequency Modulation :

)()( tmkt p

m(t)

Page 15: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

modulation

Modulation = placement of signal m(t) on a monochromatic signal xC(t) = aC cos(φ0C+ωCt) with carrier frequency ωC

Α. Amplitude modulation (general form) :

Β. Angle modulation (general form) :

)cos()()( 0 ttatx CC

)](cos[)( 0 ttatx CCC

Α. AM = Amplitude Modulation :

)()( tmkAta a )cos()]([)( 0 ttmkAtx CCa

Β. Angle modulation

Β1. PM = Phase Modulation :

Β2. FM = Frequency Modulation :

)()( tmkt p )](cos[)( 0 tmktatx pCCCC

m(t)

Page 16: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

modulation

Modulation = placement of signal m(t) on a monochromatic signal xC(t) = aC cos(φ0C+ωCt) with carrier frequency ωC

Α. Amplitude modulation (general form) :

Β. Angle modulation (general form) :

)cos()()( 0 ttatx CC

)](cos[)( 0 ttatx CCC

Α. AM = Amplitude Modulation :

)()( tmkAta a )cos()]([)( 0 ttmkAtx CCa

Β. Angle modulation

Β1. PM = Phase Modulation :

Β2. FM = Frequency Modulation :

)()( tmkt p )](cos[)( 0 tmktatx pCCCC

)()()( tmktdt

dt f

m(t)

Page 17: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

modulation

Modulation = placement of signal m(t) on a monochromatic signal xC(t) = aC cos(φ0C+ωCt) with carrier frequency ωC

Α. Amplitude modulation (general form) :

Β. Angle modulation (general form) :

)cos()()( 0 ttatx CC

)](cos[)( 0 ttatx CCC

Α. AM = Amplitude Modulation :

)()( tmkAta a )cos()]([)( 0 ttmkAtx CCa

Β. Angle modulation

Β1. PM = Phase Modulation :

Β2. FM = Frequency Modulation :

)()( tmkt p )](cos[)( 0 tmktatx pCCCC

)()()( tmktdt

dt f

])()(cos[)(

0

0 t

tfC dttmktttx

m(t)

Page 18: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

modulation

Modulation = placement of signal m(t) on a monochromatic signal xC(t) = aC cos(φ0C+ωCt) with carrier frequency ωC

Α. Amplitude modulation (general form) :

Β. Angle modulation (general form) :

)cos()()( 0 ttatx CC

)](cos[)( 0 ttatx CCC

Α. AM = Amplitude Modulation :

)()( tmkAta a )cos()]([)( 0 ttmkAtx CCa

Β. Angle modulation

Β1. PM = Phase Modulation :

Β2. FM = Frequency Modulation :

)()( tmkt p )](cos[)( 0 tmktatx pCCCC

)()()( tmktdt

dt f

])()(cos[)(

0

0 t

tfC dttmktttx

)(t

m(t)

Page 19: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

Example: Modulation of a sinusoidal signal m(t) = cosωt

Page 20: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

signal to be modulated

Example: Modulation of a sinusoidal signal m(t) = cosωt

)(tm

Page 21: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

signal to be modulated

carrier frequency

Example: Modulation of a sinusoidal signal m(t) = cosωt

)(tm

)cos( tC

Page 22: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

signal to be modulated

carrier frequency

amplitude modulation

Example: Modulation of a sinusoidal signal m(t) = cosωt

)cos()]([)( ttmkAtx Ca

)(tm

)cos( tC

AM

Page 23: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

signal to be modulated

carrier frequency

amplitude modulation

phase modulation

Example: Modulation of a sinusoidal signal m(t) = cosωt

)cos()]([)( ttmkAtx Ca

])(cos[)( tmkttx fC

)(tm

)cos( tC

AM

PM

Page 24: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

signal to be modulated

carrier frequency

amplitude modulation

phase modulation

frequency modulaion

Example: Modulation of a sinusoidal signal m(t) = cosωt

)cos()]([)( ttmkAtx Ca

])(cos[)( tmkttx fC

])(cos[)(0

t

tpC dttmkttx

)(tm

)cos( tC

AM

PM

FM

Page 25: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

signal to be modulated

carrier frequency

amplitude modulation

phase modulation

frequency modulaion

Example: Modulation of a sinusoidal signal m(t) = cosωt

)cos()]([)( ttmkAtx Ca

])(cos[)( tmkttx fC

dt

d

])(cos[)(0

t

tpC dttmkttx

dt

)(tm

)cos( tC

AM

PM

FM

Page 26: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

demodulation

Page 27: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

demodulation

Demodulation = separation of main signal m(t) from the received modulated signal x(t)

Page 28: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

demodulation

Demodulation = separation of main signal m(t) from the received modulated signal x(t)

Spectrum of signal m(t) = Fourier transform : dtetmM ti

)()(

Page 29: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

demodulation

Demodulation = separation of main signal m(t) from the received modulated signal x(t)

Spectrum of signal m(t) = Fourier transform : dtetmM ti

)()(

)(tm

Page 30: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

demodulation

Demodulation = separation of main signal m(t) from the received modulated signal x(t)

Spectrum of signal m(t) = Fourier transform : dtetmM ti

)()(

)(tm

)(tmA A

Page 31: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

demodulation

Demodulation = separation of main signal m(t) from the received modulated signal x(t)

Spectrum of signal m(t) = Fourier transform : dtetmM ti

)()(

)(tm

)(tmA A)(M0M

A2

mm 0

Page 32: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

demodulation

Demodulation = separation of main signal m(t) from the received modulated signal x(t)

Spectrum of signal m(t) = Fourier transform : dtetmM ti

)()(

)cos()()cos()cos()]([)( ttmtAttmAtx CCC

)(tm

)(tmA

)(tx

)(tmA A)(M0M

A2

mm 0

Page 33: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

demodulation

Demodulation = separation of main signal m(t) from the received modulated signal x(t)

Spectrum of signal m(t) = Fourier transform : dtetmM ti

)()(

)cos()()cos()cos()]([)( ttmtAttmAtx CCC

)()()(2

1)(

2

1)( CCCC AAMMX

)(tm

)(tmA

)(tx

)(X

A02

1 M

CC 0

)(tmA A)(M0M

A2

mm 0

Page 34: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

demodulation

Demodulation = separation of main signal m(t) from the received modulated signal x(t)

Spectrum of signal m(t) = Fourier transform : dtetmM ti

)()(

)cos()()cos()cos()]([)( ttmtAttmAtx CCC

)()()(2

1)(

2

1)( CCCC AAMMX

Properties used :

)(2)(21 AA

)(tm

)(tmA

)(tx

)(X

A02

1 M

CC 0

)(tmA A)(M0M

A2

mm 0

Page 35: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

demodulation

Demodulation = separation of main signal m(t) from the received modulated signal x(t)

Spectrum of signal m(t) = Fourier transform : dtetmM ti

)()(

)cos()()cos()cos()]([)( ttmtAttmAtx CCC

)()()(2

1)(

2

1)( CCCC AAMMX

Properties used :

)(2)(21 AA

Modulation theorem

)]()([2

1cos)(

)()(

000

ZZtz

Ztz

)(tm

)(tmA

)(tx

)(X

A02

1 M

CC 0

)(tmA A)(M0M

A2

mm 0

Page 36: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

demodulation

Demodulation = separation of main signal m(t) from the received modulated signal x(t)

Spectrum of signal m(t) = Fourier transform : dtetmM ti

)()(

)cos()()cos()cos()]([)( ttmtAttmAtx CCC

)()()(2

1)(

2

1)( CCCC AAMMX

Properties used :

)(2)(21 AA

Modulation theorem

)]()([2

1cos)(

)()(

000

ZZtz

Ztz

from which follows

)()()cos( CCC AAtA

)(2

1)(

2

1)cos()( CCC MMttm

)(tm

)(tmA

)(tx

)(X

A02

1 M

CC 0

)(tmA A)(M0M

A2

mm 0

Page 37: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

Double Band demodulation

Page 38: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

Double Band demodulation

)(2

1)(

2

1)()cos()()( CCC MMXttmtx

Modulation = multiplication of the signal m(t) with the carrier frequency cosωC t

Page 39: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

Double Band demodulation

)(2

1)(

2

1)()cos()()( CCC MMXttmtx

Demodulation = multiplication again with the carrier frequency cosωC t + low pass filter

Modulation = multiplication of the signal m(t) with the carrier frequency cosωC t

)(cos)()()cos()()( 2 ttxtmttxtd CC )(2

1)(

2

1)( CC XXD

Page 40: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

Double Band demodulation

)(2

1)(

2

1)()cos()()( CCC MMXttmtx

Demodulation = multiplication again with the carrier frequency cosωC t + low pass filter

Modulation = multiplication of the signal m(t) with the carrier frequency cosωC t

)(cos)()()cos()()( 2 ttxtmttxtd CC )(2

1)(

2

1)( CC XXD

)(2

1)(

2

1)( CC MMX

Page 41: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

Double Band demodulation

)(2

1)(

2

1)()cos()()( CCC MMXttmtx

Demodulation = multiplication again with the carrier frequency cosωC t + low pass filter

Modulation = multiplication of the signal m(t) with the carrier frequency cosωC t

)(cos)()()cos()()( 2 ttxtmttxtd CC )(2

1)(

2

1)( CC XXD

)(2

1)(

2

1)( CC MMX

)(2

1)2(

2

1)(

2

1)(

2

1)( MMMMX CCCCCCω ωωC

Page 42: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

Double Band demodulation

)(2

1)(

2

1)()cos()()( CCC MMXttmtx

Demodulation = multiplication again with the carrier frequency cosωC t + low pass filter

Modulation = multiplication of the signal m(t) with the carrier frequency cosωC t

)(cos)()()cos()()( 2 ttxtmttxtd CC )(2

1)(

2

1)( CC XXD

)(2

1)(

2

1)( CC MMX

)(2

1)2(

2

1)(

2

1)(

2

1)( MMMMX CCCCCC

)2(2

1)(

2

1)(

2

1)(

2

1)( CCCCCC MMMMX ω ω+ωC

ω ωωC

Page 43: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

Double Band demodulation

)(2

1)(

2

1)()cos()()( CCC MMXttmtx

Demodulation = multiplication again with the carrier frequency cosωC t + low pass filter

Modulation = multiplication of the signal m(t) with the carrier frequency cosωC t

)(cos)()()cos()()( 2 ttxtmttxtd CC )(2

1)(

2

1)( CC XXD

)(2

1)(

2

1)( CC MMX

)(2

1)2(

2

1)(

2

1)(

2

1)( MMMMX CCCCCC

)2(2

1)(

2

1)(

2

1)(

2

1)( CCCCCC MMMMX

)2(

2

1)(

2

1

2

1)(

2

1)2(

2

1

2

1)( CC MMMMD

ω ω+ωC

ω ωωC

Page 44: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

Double Band demodulation

)(2

1)(

2

1)()cos()()( CCC MMXttmtx

Demodulation = multiplication again with the carrier frequency cosωC t + low pass filter

Modulation = multiplication of the signal m(t) with the carrier frequency cosωC t

)(cos)()()cos()()( 2 ttxtmttxtd CC )(2

1)(

2

1)( CC XXD

)(2

1)(

2

1)( CC MMX

)(2

1)2(

2

1)(

2

1)(

2

1)( MMMMX CCCCCC

)2(2

1)(

2

1)(

2

1)(

2

1)( CCCCCC MMMMX

)2(

2

1)(

2

1

2

1)(

2

1)2(

2

1

2

1)( CC MMMMD

)2(4

1)(

2

1)2(

4

1)( CC MMMD

ω ω+ωC

ω ωωC

Page 45: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

Double Band demodulation

)(2

1)(

2

1)()cos()()( CCC MMXttmtx

Demodulation = multiplication again with the carrier frequency cosωC t + low pass filter

Modulation = multiplication of the signal m(t) with the carrier frequency cosωC t

)(cos)()()cos()()( 2 ttxtmttxtd CC )(2

1)(

2

1)( CC XXD

)(2

1)(

2

1)( CC MMX

)(2

1)2(

2

1)(

2

1)(

2

1)( MMMMX CCCCCC

)2(2

1)(

2

1)(

2

1)(

2

1)( CCCCCC MMMMX

)2(

2

1)(

2

1

2

1)(

2

1)2(

2

1

2

1)( CC MMMMD

)2(4

1)(

2

1)2(

4

1)( CC MMMD

After the low pass filter remains : )(2

1)(

2

1tmM

ω ω+ωC

ω ωωC

Page 46: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

Double Band demodulation

Page 47: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

original signal

| M(ω) | Double Band demodulation

Page 48: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

original signal

modulated signal

MODULATION

| M(ω) |

| Χ(ω) |

ωCωC

Double Band demodulation

Page 49: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

original signal

modulated signalTRANSMISSION - RECEPTION

MODULATION

| M(ω) |

| Χ(ω) |

ωCωC

Double Band demodulation

Page 50: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

original signal

modulated signalTRANSMISSION - RECEPTION

MODULATION

DEMODULATION

Multiplication with carrier frequency

| M(ω) |

| Χ(ω) |

ωCωC

| D(ω) |

2ωC2ωC

Double Band demodulation

Page 51: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

original signal

modulated signalTRANSMISSION - RECEPTION

MODULATION

DEMODULATION

Multiplication with carrier frequency

Application of low pass filter

| H(ω) |

| M(ω) |

| Χ(ω) |

ωCωC

| D(ω) |

2ωC2ωC

Double Band demodulation

Page 52: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

original signal

modulated signalTRANSMISSION - RECEPTION

MODULATION

DEMODULATION

Multiplication with carrier frequency

Application of low pass filter

| H(ω) |

½ | M(ω) |

| M(ω) |

| Χ(ω) |

ωCωC

| D(ω) |

2ωC2ωC

Double Band demodulation

Page 53: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

Double Band demodulation- preservation of outer parts

Page 54: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

| M(ω) | Double Band demodulation- preservation of outer parts

Page 55: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

Modulation = multiplication with cosωCt+ high pass filter

| M(ω) |

| Χ(ω) |

ωCωC

Double Band demodulation- preservation of outer parts

Page 56: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

Modulation = multiplication with cosωCt+ high pass filter

| M(ω) |

| H(ω) || Χ(ω) |

ωCωC

Double Band demodulation- preservation of outer parts

Page 57: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

Modulation = multiplication with cosωCt+ high pass filter

modulated signal

| M(ω) |

| H(ω) |

| Χ(ω) |

ωCωC

| Χ(ω) |

ωCωC

Double Band demodulation- preservation of outer parts

Page 58: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

Modulation = multiplication with cosωCt+ high pass filter

Demodulation = multiplication with cosωCt+ low pass filter

modulated signal

| M(ω) |

| H(ω) |

| Χ(ω) |

ωCωC

| Χ(ω) |

ωCωC

| D(ω) |

2ωC2ωC

Double Band demodulation- preservation of outer parts

Page 59: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

Modulation = multiplication with cosωCt+ high pass filter

Demodulation = multiplication with cosωCt+ low pass filter

modulated signal

| M(ω) |

| H(ω) |

| H(ω) |

| Χ(ω) |

ωCωC

| Χ(ω) |

ωCωC

| D(ω) |

2ωC2ωC

Double Band demodulation- preservation of outer parts

Page 60: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

Modulation = multiplication with cosωCt+ high pass filter

Demodulation = multiplication with cosωCt+ low pass filter

modulated signal

demodulated signal

| M(ω) |

¼| M(ω) |

| H(ω) |

| H(ω) |

| Χ(ω) |

ωCωC

| Χ(ω) |

ωCωC

| D(ω) |

2ωC2ωC

Double Band demodulation- preservation of outer parts

Page 61: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

Double Band demodulation- preservation of inner parts

Page 62: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

| M(ω) | Double Band demodulation- preservation of inner parts

Page 63: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

| M(ω) |

| Χ(ω) |

ωCωC

Double Band demodulation- preservation of inner parts

Modulation = multiplication with cosωCt+ low pass filter

Page 64: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

| H(ω) |

| M(ω) |

| Χ(ω) |

ωCωC

Double Band demodulation- preservation of inner parts

Modulation = multiplication with cosωCt+ low pass filter

Page 65: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

| H(ω) |

| M(ω) |

| Χ(ω) |

ωCωC

| Χ(ω) |

ωCωC

Double Band demodulation- preservation of inner parts

Modulation = multiplication with cosωCt+ low pass filter

modulated signal

Page 66: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

| H(ω) |

| M(ω) |

| Χ(ω) |

ωCωC

| D(ω) |

2ωC2ωC

| Χ(ω) |

ωCωC

Double Band demodulation- preservation of inner parts

Modulation = multiplication with cosωCt+ low pass filter

Demodulation = multiplication with cosωCt+ high pass filter

modulated signal

Page 67: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

| H(ω) |

| M(ω) |

| H(ω) |

| Χ(ω) |

ωCωC

| D(ω) |

2ωC2ωC

| Χ(ω) |

ωCωC

Double Band demodulation- preservation of inner parts

Modulation = multiplication with cosωCt+ low pass filter

Demodulation = multiplication with cosωCt+ high pass filter

modulated signal

Page 68: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

| H(ω) |

| M(ω) |

| H(ω) |

| Χ(ω) |

ωCωC

| D(ω) |

2ωC2ωC

| Χ(ω) |

ωCωC

¼| M(ω) |

Double Band demodulation- preservation of inner parts

Modulation = multiplication with cosωCt+ low pass filter

Demodulation = multiplication with cosωCt+ high pass filter

modulated signal

demodulated signal

Page 69: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

multiplexing

Page 70: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

multiplexing

band limited signals :

m

mmMtm||0

0)()(

Page 71: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

multiplexing

band limited signals :

m

mmMtm||0

0)()(

(spectrum concentrated in a band 2ωm wide centered at zero)

| M(ω) |

ωmωm

Page 72: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

multiplexing

band limited signals :

m

mmMtm||0

0)()(

(spectrum concentrated in a band 2ωm wide centered at zero)

Modulation : 0)()cos()()( Xttmtx C mCmC

mCmC

για

και

(spectrum concentrated in two bands 2ωm wide centered at –ωC and ωC )

| M(ω) |

ωmωm

Page 73: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

multiplexing

band limited signals :

m

mmMtm||0

0)()(

(spectrum concentrated in a band 2ωm wide centered at zero)

Modulation : 0)()cos()()( Xttmtx C mCmC

mCmC

για

και

(spectrum concentrated in two bands 2ωm wide centered at –ωC and ωC )

ωCωC

| Χ(ω) || M(ω) |

ωmωm

Page 74: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

multiplexing

band limited signals :

m

mmMtm||0

0)()(

(spectrum concentrated in a band 2ωm wide centered at zero)

Modulation : 0)()cos()()( Xttmtx C mCmC

mCmC

για

και

(spectrum concentrated in two bands 2ωm wide centered at –ωC and ωC )

ωCωC

| Χ(ω) || M(ω) |

ωmωm

ωC ωmωC ωm ωC ωmωC ωm

Page 75: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

multiplexing

band limited signals :

m

mmMtm||0

0)()(

(spectrum concentrated in a band 2ωm wide centered at zero)

Modulation : 0)()cos()()( Xttmtx C mCmC

mCmC

για

και

(spectrum concentrated in two bands 2ωm wide centered at –ωC and ωC )

Page 76: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

multiplexing

band limited signals :

m

mmMtm||0

0)()(

(spectrum concentrated in a band 2ωm wide centered at zero)

Modulation : 0)()cos()()( Xttmtx C mCmC

mCmC

για

και

(spectrum concentrated in two bands 2ωm wide centered at –ωC and ωC )

THEREFORE: Possibility of simultaneous moduletion of more signalsas long as there spectra do not overlap !

Separation with band pass filters + (usual) demodulation

Page 77: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

multiplexing

band limited signals :

m

mmMtm||0

0)()(

(spectrum concentrated in a band 2ωm wide centered at zero)

Modulation : 0)()cos()()( Xttmtx C mCmC

mCmC

για

και

(spectrum concentrated in two bands 2ωm wide centered at –ωC and ωC )

THEREFORE: Possibility of simultaneous moduletion of more signalsas long as there spectra do not overlap !

Separation with band pass filters + (usual) demodulation

Signals to be transmitted : )(,),(),( 21 tmtmtm n

Page 78: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

multiplexing

band limited signals :

m

mmMtm||0

0)()(

(spectrum concentrated in a band 2ωm wide centered at zero)

Modulation : 0)()cos()()( Xttmtx C mCmC

mCmC

για

και

(spectrum concentrated in two bands 2ωm wide centered at –ωC and ωC )

THEREFORE: Possibility of simultaneous moduletion of more signalsas long as there spectra do not overlap !

Separation with band pass filters + (usual) demodulation

Signals to be transmitted :

Corresponding carrier frequencyes :

)(,),(),( 21 tmtmtm n

n ,,, 21

Page 79: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

multiplexing

band limited signals :

m

mmMtm||0

0)()(

(spectrum concentrated in a band 2ωm wide centered at zero)

Modulation : 0)()cos()()( Xttmtx C mCmC

mCmC

για

και

(spectrum concentrated in two bands 2ωm wide centered at –ωC and ωC )

THEREFORE: Possibility of simultaneous moduletion of more signalsas long as there spectra do not overlap !

Separation with band pass filters + (usual) demodulation

Signals to be transmitted :

Corresponding carrier frequencyes :

Modulated signals :

)(,),(),( 21 tmtmtm n

n ,,, 21

)cos()(,),cos()(),cos()( 2211 ttmttmttm nn

Page 80: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

multiplexing

band limited signals :

m

mmMtm||0

0)()(

(spectrum concentrated in a band 2ωm wide centered at zero)

Modulation : 0)()cos()()( Xttmtx C mCmC

mCmC

για

και

(spectrum concentrated in two bands 2ωm wide centered at –ωC and ωC )

THEREFORE: Possibility of simultaneous moduletion of more signalsas long as there spectra do not overlap !

Separation with band pass filters + (usual) demodulation

Signals to be transmitted :

Corresponding carrier frequencyes :

Modulated signals :

Multiplexing = sum of modulated signals with non overlapping spectra

)cos()()cos()()cos()()( 2211 ttmttmttmtx nn

)(,),(),( 21 tmtmtm n

n ,,, 21

)cos()(,),cos()(),cos()( 2211 ttmttmttm nn

Page 81: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

multiplexing

Page 82: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

)(1 M

)(2 M

)(3 M

)(1 m

)(2 m

)(3 m

multiplexing

Page 83: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

)(1 M

)(2 M

)(3 M

)(1 m

)(2 m

)(3 m

~1cos

~2cos

~3cos

multiplexing

Page 84: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

)(1 M

)(2 M

)(3 M

)(1 m

)(2 m

)(3 m

~1cos

~2cos

~3cos

multiplexing

Page 85: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

)(1 M

)(2 M

)(3 M

)(1 m

)(2 m

)(3 m

~1cos

~2cos

~3cos

)(tx

multiplexing

Page 86: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

)(1 M

)(2 M

)(3 M

)(1 m

)(2 m

)(3 m

~1cos

~2cos

~3cos

)(tx

)(X

1 1 22 33

multiplexing

Page 87: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

)(1 M

)(2 M

)(3 M

)(1 m

)(2 m

)(3 m

~1cos

~2cos

~3cos

)(tx

)(X

1 1 22 33

BPF = Band Pass Filter (inside band)

multiplexing

Page 88: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

)(1 M

)(2 M

)(3 M

)(1 m

)(2 m

)(3 m

~1cos

~2cos

~3cos

)(tx

)(X

1 1 22 33

BPF = Band Pass Filter (inside band)

multiplexing

Page 89: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

)(1 M

)(2 M

)(3 M

)(1 m

)(2 m

)(3 m

~1cos

~2cos

~3cos

)(tx

)(X

1 1 22 33

multiplexing

Page 90: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

multiplexing – mathematical description

Page 91: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

)cos()()cos()()cos()()( 2211 ttmttmttmtx nn

)(2

1)(

2

1)(

2

1)(

2

1)(

2

1)(

2

1)( 22221111 nnnn MMMMMMX

)(tx

multiplexing – mathematical description

Page 92: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

)cos()()cos()()cos()()( 2211 ttmttmttmtx nn

)(2

1)(

2

1)(

2

1)(

2

1)(

2

1)(

2

1)( 22221111 nnnn MMMMMMX

BPF)(tx

BPF

BPF

Application of band pass filter (BPF, inside band) == preservation of a single term :

)cos()()()(2

1)(

2

1)( ttmtxMMX kkkkkkkk

multiplexing – mathematical description

Page 93: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

~2cos

)cos()()cos()()cos()()( 2211 ttmttmttmtx nn

)(2

1)(

2

1)(

2

1)(

2

1)(

2

1)(

2

1)( 22221111 nnnn MMMMMMX

BPF

~3cos

~1cos

LPF

)(tx

BPF

BPF

LPF

LPF

Application of band pass filter (BPF, inside band) == preservation of a single term :

)cos()()()(2

1)(

2

1)( ttmtxMMX kkkkkkkk

Usual demodulation =

= [ cosωi ] + [ LPF ] =

= retrieval of signal mk(t)

multiplexing – mathematical description

Page 94: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

~2cos

)cos()()cos()()cos()()( 2211 ttmttmttmtx nn

)(2

1)(

2

1)(

2

1)(

2

1)(

2

1)(

2

1)( 22221111 nnnn MMMMMMX

BPF

~3cos

~1cos

LPF

)(tx

BPF

BPF

LPF

LPF

BPF = Band Pass Filter, inside band

LPF = Low Pass Filter

Application of band pass filter (BPF, inside band) == preservation of a single term :

)cos()()()(2

1)(

2

1)( ttmtxMMX kkkkkkkk

Usual demodulation =

= [ cosωi ] + [ LPF ] =

= retrieval of signal mk(t)

multiplexing – mathematical description

Page 95: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

~2cos

)cos()()cos()()cos()()( 2211 ttmttmttmtx nn

)(2

1)(

2

1)(

2

1)(

2

1)(

2

1)(

2

1)( 22221111 nnnn MMMMMMX

BPF

)(1 m

)(2 m

)(3 m

~3cos

~1cos

LPF

)(tx

BPF

BPF

LPF

LPF

BPF = Band Pass Filter, inside band

LPF = Low Pass Filter

Application of band pass filter (BPF, inside band) == preservation of a single term :

)cos()()()(2

1)(

2

1)( ttmtxMMX kkkkkkkk

Usual demodulation =

= [ cosωi ] + [ LPF ] =

= retrieval of signal mk(t)

multiplexing – mathematical description

Page 96: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

heterodyning

Page 97: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

heterodyning

Heterodyning = Mixing (sum) of received signal having frequency f, with a signal of slightly different frequency fR produced in the receiver ( fR f )

Page 98: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

heterodyning

Rfff RRfff 222

Heterodyning = Mixing (sum) of received signal having frequency f, with a signal of slightly different frequency fR produced in the receiver ( fR f )

Page 99: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

heterodyning

Rfff RRfff 222

)sin()sin()2sin()2sin()( 0000 RRRRRR tatatfatfatx

Heterodyning = Mixing (sum) of received signal having frequency f, with a signal of slightly different frequency fR produced in the receiver ( fR f )

Page 100: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

heterodyning

Rfff RRfff 222

)sin()sin()2sin()2sin()( 0000 RRRRRR tatatfatfatx

:RΜε

Heterodyning = Mixing (sum) of received signal having frequency f, with a signal of slightly different frequency fR produced in the receiver ( fR f )

2

sin2

sinsin2

sin)( 00 ttattaatx RR

Page 101: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

signal of frequency f (angular ω) with amplitude which varies periodicallywith frequency Δf angular Δω)

heterodyning

Rfff RRfff 222

)sin()sin()2sin()2sin()( 0000 RRRRRR tatatfatfatx

:RΜε

Heterodyning = Mixing (sum) of received signal having frequency f, with a signal of slightly different frequency fR produced in the receiver ( fR f )

2

sin2

sinsin2

sin)( 00 ttattaatx RR

Page 102: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

heterodyning

Rfff RRfff 222

)sin()sin()2sin()2sin()( 0000 RRRRRR tatatfatfatx

:RΜε

Heterodyning = Mixing (sum) of received signal having frequency f, with a signal of slightly different frequency fR produced in the receiver ( fR f )

2

sin2

sinsin2

sin)( 00 ttattaatx RR

signal of frequency f (angular ω) with amplitude which varies periodically with frequency Δf angular Δω)

Page 103: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

heterodyning

Rfff RRfff 222

)sin()sin()2sin()2sin()( 0000 RRRRRR tatatfatfatx

:RΜε

2

sin2

sinsin2

sin)( 00 ttattaatx RR

Heterodyning = Mixing (sum) of received signal having frequency f, with a signal of slightly different frequency fR produced in the receiver ( fR f )

signal of frequency f (angular ω) with amplitude which varies periodically with frequency Δf angular Δω)

Page 104: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

heterodyning

Rfff RRfff 222

)sin()sin()2sin()2sin()( 0000 RRRRRR tatatfatfatx

:RΜε

Δf = f fR (angular Δω = ω ωR ) = beat frequency

2

sin2

sinsin2

sin)( 00 ttattaatx RR

Heterodyning = Mixing (sum) of received signal having frequency f, with a signal of slightly different frequency fR produced in the receiver ( fR f )

signal of frequency f (angular ω) with amplitude which varies periodically with frequency Δf angular Δω)

Page 105: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

heterodyning

Rfff RRfff 222

)sin()sin()2sin()2sin()( 0000 RRRRRR tatatfatfatx

:RΜε

signal of frequency f (angular ω) with amplitude which varies periodically with frequency Δf angular Δω)

Δf = f fR (angular Δω = ω ωR ) = beat frequency

Application: observations in space geodesy utilizing the Doppler phaenomenon (variation of frequency caused by the variation of the receiver-transmitter relative position)

2

sin2

sinsin2

sin)( 00 ttattaatx RR

Heterodyning = Mixing (sum) of received signal having frequency f, with a signal of slightly different frequency fR produced in the receiver ( fR f )

Page 106: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

Beat frequency :

Δf = f – fR = 1 – 5/6 = 1/6

(TΔf = 6)

T = 1 f = 1

TR = 6/5 fR = 5/6

Δf = f fR = 1/6

TΔf = 6

Example :

Received frequency : f = 1 (T = 1)

Frequency at receiver : fR = 5/6 (T = 6/5)

8

6

4

2

-2

-4

-6

-8

2 4 86 10 12 14 16

2 4 86 10 12 14 16

2 4 86 10 12 14 16

4

2

-2

-4

4

2

-2

-4

0

0

0

Page 107: Lecture 6: Signals Transmission

Aristotle University of ThessalonikiAristotle University of Thessaloniki – – Department of Geodesy and SurveyingDepartment of Geodesy and Surveying

A. DermanisA. Dermanis Signals and Spectral Methods in GeoinformaticsSignals and Spectral Methods in Geoinformatics

END