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EITN90 Radar and Remote Sensing Lecture 2: The Radar Range Equation Daniel Sj¨ oberg Department of Electrical and Information Technology Spring 2019

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Page 1: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

EITN90 Radar and Remote SensingLecture 2: The Radar Range Equation

Daniel Sjoberg

Department of Electrical and Information Technology

Spring 2019

Page 2: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Outline

1 Radar Range EquationReceived powerSignal to noise ratioLossesMultiple pulsesApplication oriented RRE:s

2 Radar Search and DetectionSearch mode fundamentalsDetection fundamentals

3 Conclusions

2 / 62

Page 3: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Learning outcomes of this lecture

In this lecture we will

I Develop a physical model for the received power of a radarfrom a target at a distance

I Interpret the result in user terms and designer terms fordifferent applications

I Investigate the requirements and methods of search anddetection

3 / 62

Page 4: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Outline

1 Radar Range EquationReceived powerSignal to noise ratioLossesMultiple pulsesApplication oriented RRE:s

2 Radar Search and DetectionSearch mode fundamentalsDetection fundamentals

3 Conclusions

4 / 62

Page 5: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Outline

1 Radar Range EquationReceived powerSignal to noise ratioLossesMultiple pulsesApplication oriented RRE:s

2 Radar Search and DetectionSearch mode fundamentalsDetection fundamentals

3 Conclusions

5 / 62

Page 6: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Isotropic radiation pattern

Equal radiation in all directions.

I Pt = transmitted power [W]

I R = distance from source [m]

I Qi = power density [m2]

6 / 62

Page 7: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Directional radiation pattern

Stronger radiation in some directions.

Transmitting antenna gain Gt(θ, φ)def= lim

R→∞Qi(R,θ,φ)Pt/(4πR2)

def= 4πAe

λ2.

Effective area Ae and gain Gt represent the same physical concept,just a scaling by 4π/λ2.

7 / 62

Page 8: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Scattered power from a target

Target is hit by power density Qi, and scatters the power.

Radar cross section (RCS) σdef= lim

R→∞4πR2Qr

Qi(Qi held constant).

8 / 62

Page 9: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Received power

Received power is Pr = AeQr , effective area Aedef= λ2

4πGr.

Putting everything together implies the Radar Range Equation

Pr =PtGtGrλ

(4π)3R49 / 62

Page 10: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Radar Range Equation

The radar range equation is the fundamental model for estimatingthe received power in a given scenario.

Pr =PtGtGrλ

(4π)3R4

I Pt = peak transmitted power [W]

I Gt = gain of transmit antenna (unitless)

I Gr = gain of receive antenna (unitless)

I λ = carrier wavelength [m]

I σ = mean RCS of target [m2]

I R = range from radar to target [m]

Discussion question

10 / 62

Page 11: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Radar Range Equation, dB scale

The decibel (dB) scale is defined as

Pr [dB]def= 10 log10(Pr)

The logarithm function has the propertieslog10(ab) = log10(a) + log10(b), log10(a/b) = log10(a)− log10(b),and log10(a

b) = b log10(a). The RRE is then

Pr [dB] = Pt [dB] +Gt [dB] +Gr [dB] + 2 · λ [dB] + σ [dB]

−30 log10(4π)︸ ︷︷ ︸=−33 dB

−4 ·R [dB]

For quantities with physical units, it is common to introduce areference level (note context sensitivity for dBm):

I 10 log10(Pr1W

) def= Pr [dBW] (W for Watt)

I 10 log10(

Pr1mW

) def= Pr [dBm] (m for milli-Watt)

I 10 log10(λ1m

) def= λ [dBm] (m for meter)

I 10 log10(

σ1m2

) def= σ [dBsm] (sm for square meters)

11 / 62

Page 12: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Radar Range Equation, dB scale

The decibel (dB) scale is defined as

Pr [dB]def= 10 log10(Pr)

The logarithm function has the propertieslog10(ab) = log10(a) + log10(b), log10(a/b) = log10(a)− log10(b),and log10(a

b) = b log10(a). The RRE is then

Pr [dB] = Pt [dB] +Gt [dB] +Gr [dB] + 2 · λ [dB] + σ [dB]

−30 log10(4π)︸ ︷︷ ︸=−33 dB

−4 ·R [dB]

For quantities with physical units, it is common to introduce areference level (note context sensitivity for dBm):

I 10 log10(Pr1W

) def= Pr [dBW] (W for Watt)

I 10 log10(

Pr1mW

) def= Pr [dBm] (m for milli-Watt)

I 10 log10(λ1m

) def= λ [dBm] (m for meter)

I 10 log10(

σ1m2

) def= σ [dBsm] (sm for square meters)

11 / 62

Page 13: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Bistatic scenario

In a bistatic scenario, with two antennas separated in space, thetransmit and receive distances Rt and Rr are usually different:

Pr =PtGtGrλ

(4π)3R2tR

2r

Rt Rr

We will focus on the monostatic scenario.

12 / 62

Page 14: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Outline

1 Radar Range EquationReceived powerSignal to noise ratioLossesMultiple pulsesApplication oriented RRE:s

2 Radar Search and DetectionSearch mode fundamentalsDetection fundamentals

3 Conclusions

13 / 62

Page 15: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Thermal noise

The power of the thermal noise in the radar receiver is

Pn = kTsB = kT0FB

where the different factors are

I k is Boltzmann’s constant (1.38 · 10−23 Ws/K)

I T0 is the standard temperature (290 K)

I Ts is the system noise temperature (Ts = T0F )

I B is the instantaneous receiver bandwidth in Hz

I F = SNRinSNRout

is the noise figure of the receiver subsystem(unitless)

14 / 62

Page 16: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

SNR version of RRE

The thermal noise of the receiver can be combined with the RREto yield the signal to noise ratio

SNR =Pr

Pn=

PtGtGrλ2σ

(4π)3R4kT0FB

The final radar performance is determined by the signal tointerference ratio, where

SIR =S

N + C + J=PtGtGrλ

(4π)3R4

1

kT0FB + C + J

I S = signal powerI N = noise powerI C = clutter powerI J = jammer power

Often only one of S/N , S/C or S/J is dominating.

15 / 62

Page 17: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

SNR version of RRE

The thermal noise of the receiver can be combined with the RREto yield the signal to noise ratio

SNR =Pr

Pn=

PtGtGrλ2σ

(4π)3R4kT0FB

The final radar performance is determined by the signal tointerference ratio, where

SIR =S

N + C + J=PtGtGrλ

(4π)3R4

1

kT0FB + C + J

I S = signal powerI N = noise powerI C = clutter powerI J = jammer power

Often only one of S/N , S/C or S/J is dominating.

15 / 62

Page 18: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Clutter

The radar signal can be scattered against many other things in thebackground. These interfering signals are called clutter.

Since the clutter scatterers are typically located close to thescatterer we want to detect, all terms in the radar equation canceland the target signal to clutter ratio is

SCR =σ

σc

The clutter RCS σc can be significant, depending on how much isbeing illuminated by the radar. There are two typical kinds ofclutter:

I Surface clutter

I Volume clutter

More on clutter in Chapter 5.Discussion question

16 / 62

Page 19: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Surface clutter

σcs = Acσ0

I σcs is the surface clutter radar cross section (square meters)

I Ac is the area of the illuminated (ground or sea surface)clutter cell (square meters)

I σ0 is the surface backscatter coefficient (average reflectivityper unit area) (square meters per square meters, or unitless)

17 / 62

Page 20: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Volume clutter

σcv = Vcη

I σcv is the volume clutter radar cross section (square meters)I Vc is the volume of the illuminated clutter cell (cubic meters)I η is the volumetric backscatter coefficient (average reflectivity

per unit volume) (square meters per cubic meters, orreciprocal meters)

18 / 62

Page 21: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Jamming

Jamming is a method of disabling a radar system by sending astrong interfering signal, saturating the receiver. The receivedpower from this signal is calculated by the one-way equation

Prj =PjGjGrjλ

2

(4π)2R2jrLs

I Prj received power from the jammer

I Pj transmitted power from the jammer

I Gj gain of the jammer antenna

I Grj gain of the receive antenna (in direction of jammer)

I Rjr distance between jammer and receiver

I Ls system losses

19 / 62

Page 22: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Outline

1 Radar Range EquationReceived powerSignal to noise ratioLossesMultiple pulsesApplication oriented RRE:s

2 Radar Search and DetectionSearch mode fundamentalsDetection fundamentals

3 Conclusions

20 / 62

Page 23: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Losses

We have neglected a number of real-life losses in the RRE so far.The typical system loss would be the combination of several:

Ls = LtLaLrLsp

where the different factors areI Ls is the system lossI Lt is the transmit lossI La is the atmospheric lossI Lr is the receiver lossI Lsp is the signal processing loss

with the resulting system-loss SNR (an additional factor np canaccount for multiple pulses signal processing gain, see later slides)

SNR =PtGtGrλ

(4π)3R4kT0FBLs

The various factors are discussed in the following slides.21 / 62

Page 24: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Transmit loss

Typically waveguides, cables, circulator, directional coupler, andswitch add losses on the order of Lt ≈ 3− 4 dB.

The antenna gain G may include some losses, depending ondefinition. Always consult datasheets!

22 / 62

Page 25: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Atmospheric loss

Atmospheric losses depend on frequency, weather conditions,altitude, etc. Typically measured in dB/km, and limits the range ofthe radar.

23 / 62

Page 26: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Atmospheric loss

Typical atmospheric losses as function of frequency, at two differentaltitudes. Note the peaks corresponding to resonant interactionwith atmosphere molecules. Further losses are due to rain, fog etc.

Long range radar systems tend to operate in frequency regionswith low loss, but short-range systems may use losses for isolation. 24 / 62

Page 27: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Receive loss

Similar to transmit losses: waveguides, cables, circulator, switch,filters etc. Include losses up to the point where the noise figure Fis specified (F = SNRin

SNRout).

25 / 62

Page 28: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Signal processing loss

Even though the signal processor usually provides gain (typically onthe order of np), the imperfections also provide some loss.

26 / 62

Page 29: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Signal processing loss: beam scanning

Loss due to the target not being intercepted by the maximum gainof the beam. While tracking, beam can be kept on target.

27 / 62

Page 30: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Signal processing loss: straddle loss

Discretization of range and Doppler frequencies in differentprocessing bins may introduce loss around 1 dB in both range andDoppler. The dips can be reduced by increasing bin overlap(oversampling).

28 / 62

Page 31: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Outline

1 Radar Range EquationReceived powerSignal to noise ratioLossesMultiple pulsesApplication oriented RRE:s

2 Radar Search and DetectionSearch mode fundamentalsDetection fundamentals

3 Conclusions

29 / 62

Page 32: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Multiple pulses

The SNR can be improved by using data from several pulses. Thesignal processing gain from this can be estimated as (assumingwhite noise)

I Coherent processing (both phase and amplitude):

SNR(np) = np SNR(1)

I Noncoherent processing (only amplitude):

SNR(np) ≈ √np SNR(1)

Typically, the processing gain by using multiple pulses can beestimated as

√np SNR(1) ≤ SNR(np) ≤ np SNR(1)

Using many pulses increases the measurement time.

30 / 62

Page 33: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Average power, coherent processing

We use np pulses, each with duration τ and repeated at PulseRepetition Frequency (PRF=1/PRI, Pulse Repetition Interval).

t

τ

PRI

Td = np · PRI

I Dwell time Td = np · PRI = np/PRF.

I Peak pulse power Pt =PavgTdnpτ

=PavgTdB

np

The coherent processing SNR is then

SNRc =

(PavgTdB

np

)︸ ︷︷ ︸

= peak Pt per pulse

GtGrλ2σnp

(4π)3R4kT0FBLs=PavgTdGtGrλ

(4π)3R4kT0FLs

31 / 62

Page 34: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Pulse compression

There seems to be two conflicting requirements:

I High resolution requires short pulse time τ (or rather, highbandwidth)

I High SNR requires long pulse time τ

These requirements can be combined using pulse compression,explained in Chapter 20. The average power form of the RREremains the same,

SNRpc =PavgTdGtGrλ

(4π)3R4kT0FLs

where

I PavgTd is the energy in one pulse train

I kT0F is the noise energy from the receiver

Discussion question

32 / 62

Page 35: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Outline

1 Radar Range EquationReceived powerSignal to noise ratioLossesMultiple pulsesApplication oriented RRE:s

2 Radar Search and DetectionSearch mode fundamentalsDetection fundamentals

3 Conclusions

33 / 62

Page 36: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Case study: hypothetical radar system SNR

Transmitter: 150 kilowatt peak powerFrequency: 9.4 GHzPulse width: 1.2 microsecondsPRF: 2 kilohertzAntenna: 2.5 meter diameter circular antenna (an

efficiency η = 0.6 is used to determineantenna gain.)

Processing dwell time: 18.3 millisecondsReceiver noise figure: 2.5 dBTransmit losses: 3.1 dBReceive losses: 2.4 dBSignal processing losses: 3.2 dBAtmospheric losses: 0.16 dB/km (one way)Target RCS: 0 dBsm, –10 dBsm (1.0 and 0.1 m 2 )Target range: 5 to 105 km

34 / 62

Page 37: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Case study, graphical form

Different detection ranges for the two different targets.

35 / 62

Page 38: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Search application

A solid angle Ω is being scanned for targets at M beam positions withdwell time Td. The total time to scan is then

Tfs = MTd ≈Ω

θ3φ3Td

where θ3 and φ3 are the azimuth and elevation 3 dB beamwidths. Usingθ3φ3 ≈ λ2/Ae and G = 4πAe/λ

2, the average power RRE can be written

PavgAe

4πkT0FLs≥ SNRmin

(R4

σ

)(Ω

Tfs

)where “user terms” are on the right and “system designer terms” on theleft. This shows that the power-aperture product PavgAe has to bemaximized in order to search a big solid angle Ω at small time Tfs. 36 / 62

Page 39: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Track application

When tracking one or several targets, important parameters areI Tracking precision σθ ∼ 1/

√SNR

I Number of tracked targets Nt

I Updates per second r37 / 62

Page 40: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

RRE for track application

The RRE can be rewritten in terms of the tracking parameters as(see derivation in the book, Section 2.16)

PavgA3ek

2m

λ4kT0FLs=

(π2

2

)(rNtR

4

σ · σ2θ

)(1

cos5(θscan)

)where km ∈ [1, 2] is a tracking system parameter, and the factorcos5(θscan) accounts for gain loss and beam broadening whenscanning a phased array. This shows the strong dependence onantenna aperture for efficient tracking.

With known SNR rather than σθ, we could also write

PavgA2e

LsFλ2=

SNR · 4πR4kT0 · PRF

σ

which also demonstrates a strong dependence on Ae.38 / 62

Page 41: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Some trade-offs

SNR =PavgTdGtGrλ

(4π)3R4kT0FLs=PavgTdAetAerσ/λ

2

4πR4kT0FLs

I Stealth technology: SNR ∼ σ/R4 shows that σ needs to bereduced significantly in order to affect detection range R.This implies high costs.

I SNR increases with increased dwell time Td, at the expense oflonger measurement times.

I For fixed Ae and σ (antenna and scatterer large compared towavelength), smaller wavelength increases SNR.

Discussion question

39 / 62

Page 42: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Outline

1 Radar Range EquationReceived powerSignal to noise ratioLossesMultiple pulsesApplication oriented RRE:s

2 Radar Search and DetectionSearch mode fundamentalsDetection fundamentals

3 Conclusions

40 / 62

Page 43: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Outline

1 Radar Range EquationReceived powerSignal to noise ratioLossesMultiple pulsesApplication oriented RRE:s

2 Radar Search and DetectionSearch mode fundamentalsDetection fundamentals

3 Conclusions

41 / 62

Page 44: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Task of the search mode

The task of the search mode is to scan through a certain volume,and detect the presence of targets with no a priori knowledge oftheir existence.

The radar beam is directed at different angles, mechanically orelectrically, and measurements are taken at each position. Thescan has to be fast enough, so targets do not have too much timeto move.

42 / 62

Page 45: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Mechanical vs electrical scanning

Mechanical

I Rotating turret.

I Typically scans in azimuth.

I Continuous movement 360

one direction or finite sectorback-and-forth.

I Rotation speed needs toalign with dwell time andrange delay.

Electrical

I Phased array.

I Scans quickly in alldirections.

I Beam width changes withangle.

I Scan loss can becompensated by increasingdwell time at large angles.

Search can be combined with track either bytracking-while-scanning (slow update), or search-and-track(interleaving track function, only ESA).

43 / 62

Page 46: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Outline

1 Radar Range EquationReceived powerSignal to noise ratioLossesMultiple pulsesApplication oriented RRE:s

2 Radar Search and DetectionSearch mode fundamentalsDetection fundamentals

3 Conclusions

44 / 62

Page 47: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Threshold concept

A detection is registered when a signal is registered above athreshold, giving some margin to the noise floor. The signal needsto be considered as a random variable.

45 / 62

Page 48: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Probability

Probability of False Alarm: PFA =

∫ ∞Vt

pi(v) dv

Probability of Detection: PD =

∫ ∞Vt

ps+i(v) dv

The probability density function (PDF) is denoted p, index “i” forinterference and index “s+i” for signal in the presence ofinterference.

46 / 62

Page 49: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Noise probability distribution: Rayleigh distribution

When measuring both amplitude and phase, v = I + jQ, the I andQ signals due to noise are zero mean Gaussian. This implies theamplitude r =

√I2 +Q2 is Rayleigh distributed, that is,

pi(r) =r

σ2nexp

(− r2

2σ2n

)where σ2n is the mean square voltage, or variance of the noise,called noise power. In the figure below, σ2n = 0.04.

47 / 62

Page 50: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Probability of false alarm

Using the Rayleigh distribution, the probability of false alarm canbe computed explicitly (a truly rare case!):

PFA =

∫ ∞Vt

r

σ2nexp

(− r2

2σ2n

)dr = exp

(− V

2t

2σ2n

)For a desired PFA, this provides the required threshold:

Vt =√

2σ2n ln(1/PFA)

To further reduce the PFA, it is common to make confirmationmeasurements of a detection. With n confirmations, we get

PFA(n) = [PFA(1)]n

for a false alarm in all dwells, which quickly reduces the PFA.

48 / 62

Page 51: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Signal + noise PDF: Rician distribution

For a non-fluctuating target signal embedded in Gaussian noise, weobtain the Rice distribution:

ps+i(v) =v

σ2nexp

(−v2 + v2s+i

2σ2n

)I0(vvs+i/σ

2n)

where vs+i is the mean amplitude, and I0 is the modified Besselfunction of the first kind and second order. For vs+i = 0 this is theRayleigh distribution. The probability of detection is

PD =

∫ ∞Vt

ps+i(v) dv =

∫ ∞Vt

v

σ2nexp

(−v2 + v2s+i

2σ2n

)I0(vvs+i/σ

2n) dv

Not surprisingly, this does not have a closed solution, but can beimplemented numerically (Marcum’s Q-function).

49 / 62

Page 52: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

50 / 62

Page 53: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Receiver operating curves, ROC

To investigate the trade-off between PFA, PD, and SNR, a curve oftwo with varying values of the third can be plotted.

Higher level system requirements determine desired PFA and PD

which can vary a lot. Typical values could be PD around50%− 90% for a PFA in the order of 10−4 − 10−6. In the curvesabove, this requires SNR around 10 dB− 13 dB.

51 / 62

Page 54: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Fluctuating targets: motivation

Big, real life targets have very complicated RCS, dependingstrongly on angle. A statistical description is necessary.

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Page 55: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

The Swerling models

Two different PDF:s (different target characteristics), combinedwith two different fluctuation rates: dwell-to-dwell orpulse-to-pulse.

For fixed PFA and PD, a fluctuating target (SW1-4) requires higherSNR than a non-fluctuating target (SW0).

Further details in Chapter 7.53 / 62

Page 56: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Receiver operation curves

For high PD the required SNR for fluctuating targets issignificantly higher than for non-fluctuating. For low PD

fluctuating targets may require lower SNR than fluctuating, butthis is seldom an interesting region.

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Page 57: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Closed-form solutions

Chapter 3.3.8 presents some closed form solutions for computingprobabilities. These can be convenient in specific cases, but pleasealways check carefully the region of applicability of theformulas!

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Page 58: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Multiple dwells

The single-dwell detection probability can be improved usingmultiple dwells with only a small penalty in cumulative false alarm:

PD(n) = 1− [1− PD(1)]n

PFA(n) = nPFA(1)

Requiring m-of-n detections can further improve both probabilities:

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Page 59: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Outline

1 Radar Range EquationReceived powerSignal to noise ratioLossesMultiple pulsesApplication oriented RRE:s

2 Radar Search and DetectionSearch mode fundamentalsDetection fundamentals

3 Conclusions

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Page 60: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Conclusions

I The radar range equation estimates the received power orSNR.

I An overview of losses have been presented.

I The use of multiple pulses to strengthen SNR has beendemonstrated.

I The RRE can be adapted to various specific applications, likesearch or track, with parameters specific for the application.

I Fundamentals of detection theory have been treated,introducing PD and PFA.

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Page 61: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Discussion

Based on the radar range equation

Pr =PtGtGrλ

(4π)3R4

should we go for long or short wavelengths to maximize Pr?

Answer:With Gt and Gr fixed, long wavelengths are preferred.Using G = 4πAe

λ2, the RRE is

Pr =PtAteAreσ

4πλ2R4

With Ate and Are fixed, short wavelengths are preferred!

Go back

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Page 62: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Discussion

Based on the radar range equation

Pr =PtGtGrλ

(4π)3R4

should we go for long or short wavelengths to maximize Pr?Answer:With Gt and Gr fixed, long wavelengths are preferred.

Using G = 4πAeλ2

, the RRE is

Pr =PtAteAreσ

4πλ2R4

With Ate and Are fixed, short wavelengths are preferred!

Go back

59 / 62

Page 63: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Discussion

Based on the radar range equation

Pr =PtGtGrλ

(4π)3R4

should we go for long or short wavelengths to maximize Pr?Answer:With Gt and Gr fixed, long wavelengths are preferred.Using G = 4πAe

λ2, the RRE is

Pr =PtAteAreσ

4πλ2R4

With Ate and Are fixed, short wavelengths are preferred!

Go back

59 / 62

Page 64: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Discussion

Based on the radar range equation

Pr =PtGtGrλ

(4π)3R4

should we go for long or short wavelengths to maximize Pr?Answer:With Gt and Gr fixed, long wavelengths are preferred.Using G = 4πAe

λ2, the RRE is

Pr =PtAteAreσ

4πλ2R4

With Ate and Are fixed, short wavelengths are preferred!Go back

59 / 62

Page 65: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Discussion

Give some examples of scatterers giving rise to clutter!

Answer:Surface clutter: rocks, grass, sea waves, bushes, sand dunes. . .Volume clutter: rain, hail, insect swarms, forest, sand storm. . .

Go back

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Page 66: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Discussion

Give some examples of scatterers giving rise to clutter!

Answer:Surface clutter: rocks, grass, sea waves, bushes, sand dunes. . .Volume clutter: rain, hail, insect swarms, forest, sand storm. . .

Go back

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Page 67: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Discussion

With the average power form of the radar range equation

SNR =PavgTdGtGrλ

(4π)3R4kT0FLs

things only get better with large dwell time Td. Are there anydisadvantages?

Answer: yes, longer measurement time implies slower reaction.

Go back

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Page 68: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Discussion

With the average power form of the radar range equation

SNR =PavgTdGtGrλ

(4π)3R4kT0FLs

things only get better with large dwell time Td. Are there anydisadvantages?

Answer: yes, longer measurement time implies slower reaction.Go back

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Page 69: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Discussion

How do you think the radar cross section of a scatterer can bereduced?

Answer:

1. Shaping the scatterer to divert reflection away frommonostatic direction.

2. Absorbing the incoming wave.

3. Active cancellation: send out a signal that cancels thereflection signal (very difficult).

Go back

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Page 70: EITN90 Radar and Remote Sensing Lecture 2: The Radar Range ... · Typical atmospheric losses as function of frequency, at two di erent altitudes. Note the peaks corresponding to resonant

Discussion

How do you think the radar cross section of a scatterer can bereduced?

Answer:

1. Shaping the scatterer to divert reflection away frommonostatic direction.

2. Absorbing the incoming wave.

3. Active cancellation: send out a signal that cancels thereflection signal (very difficult).

Go back

62 / 62