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UAF Class GEOS 657 GEOS 657 MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks; [email protected] Lecture 7: Principles of Radar & Active Microwave Systems Image: DLR, CC-BY 3.0

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Page 1: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

UAF Class GEOS 657

GEOS 657 – MICROWAVE REMOTE SENSINGSPRING 2019

Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks; [email protected]

Lecture 7: Principles of Radar & Active Microwave Systems

Image: DLR, CC-BY 3.0

Page 2: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

Franz J Meyer, UAF

GEOS 657: Microwave RS - 2

Sentinel-1 C-band Radar monitors Dam Break in Brazil

Before dam breach: 2019-01-22

Recent “Radar in the News”

Page 3: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

Franz J Meyer, UAF

GEOS 657: Microwave RS - 3

Sentinel-1 C-band Radar monitors Dam Break in Brazil

Before dam breach: 2019-01-22After dam breach: 2019-01-28

Recent “Radar in the News”

Page 4: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

Franz J Meyer, UAF

GEOS 657: Microwave RS - 4

VS.2019-01-22

2019-01-28

Recent “Radar in the News”Se

nti

nel

-1 S

AR

O

ptical2019-01-29

2019-01-24

Planet Labs

Planet Labs

Page 5: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

Franz J Meyer, UAF

GEOS 657: Microwave RS - 5

• Some Basics and Three Types of Radar Systems

• Imaging Radars - Concepts:

– The Radar Equation

– Separating Several Range Resolution Cells within Antenna Footprint

• Imaging Radars – How it’s Really Done:

– The Concept of Pulse Compression Systems

– The Resolution-Bandwidth Duality

– Range Compression – The Matched Filter Approach

• Examples of Imaging Radar Data

Outline

5

Page 6: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

Franz J Meyer, UAF

GEOS 657: Microwave RS - 6

SOME BASICS AND THREE TYPES OF RADAR SYSTEMS

Page 7: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

Franz J Meyer, UAF

GEOS 657: Microwave RS - 77

Active Microwave Systems are called RADARs

• Radars actively transmit microwave signals (usually a radar pulse)

• Radar antenna provides directivity for transmitted signal

• A radar sensor records three different parameters: Amplitude, Phase and polarization of the reflected microwave signals (here we focus on amplitude and phase)

Detected amplitude measures surface radar cross section (RCS)

Timing of transmitted signal (radar pulse) provides information about distance between

satellite and ground

Page 8: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

Franz J Meyer, UAF

GEOS 657: Microwave RS - 88

Three Different Types of Radar Systems

• Based on measurement type, three different radar systems can be discriminated:

Non-Imaging Systems

RADAR ALTIMETERS

Measuring distance

(from travel time)

Trans-

mitted

pulses

SCATTEROMETERS

Measuring radar cross

section

Trans-

mitted

pulses

Imaging Systems

Range pixel

size ~ pulse

length

Azimuth

pixel size =

antenna

footprint (or

better when

doing SAR)

Page 9: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

Franz J Meyer, UAF

GEOS 657: Microwave RS - 9

Radar Principle

TX

RX

R

scattering

object

range

transmit

cR2

received echo:

(time)

light velocity

Page 10: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

Franz J Meyer, UAF

GEOS 657: Microwave RS - 10

• Radar altimeter emits pulses towards the Earth's surface (nadir direction)

• Signal travel time (transmission to reception) is proportional to satellite altitude.

A Short Word on Radar Altimeters

10

• Measuring Signal travel time not easy as echo signal has funny shape

Idealized altimeter echo from flat surface (e.g., smooth ocean surface

Page 11: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

Reference EllipsoidGeoid Undulations

Dynamic Topography

Barometric EffectTides SWH

Center of Mass

Instantaneous Sea Level

Orbit Height = H

Mean Sea Level = SSHmean

Geoid = Hgeoid

Sensor Geometry

Ionosphere

Dry Troposphere

Wet TroposphereHmeasured

11

Calculating Surface Height from Altimeter Measurements

Page 12: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

Mean Sea Level Height from AltimetryM

ean

Sea

Lev

el M

arch

20

06

12

Page 13: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

Franz J Meyer, UAF

GEOS 657: Microwave RS - 13

Microwave Scatterometers

• Goal: measurement of wind speed and direction over oceans

wind

ocean

surface

roughness

radar

backscatter

Example: Scatterometer on ERS

Page 14: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

Franz J Meyer, UAF

GEOS 657: Microwave RS - 14

QuikSCAT Windfield

Page 15: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

Franz J Meyer, UAF

GEOS 657: Microwave RS - 15

IMAGING RADAR CONCEPTS

Page 16: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

Franz J Meyer, UAF

GEOS 657: Microwave RS - 16

The Radar Equation – A Reminder

transmit power: WPt

224 m

W

R

GPt

power density at scatterer:

antenna gain:2

4

AG

radar cross section: 2m

WR

GPt 24

reflected power:

antenna area: 2mA

received power:

WR

GP

R

GPG

R

GPAP t

ttr

43

22

42

2

424444

242

4 m

W

R

GPt

power density at receiver:

Page 17: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

Franz J Meyer, UAF

GEOS 657: Microwave RS - 17

Pulse Waveform and Range Resolution

targets #1 and #2 easily separable, if 2cPRR (range resolution)

transmit

receive

PR R

targets:

#1 #2

Page 18: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

Franz J Meyer, UAF

GEOS 657: Microwave RS - 18

Range Resolution Example

• Insufficient Target Separation

• Sufficient Target Separation

Page 19: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

Franz J Meyer, UAF

GEOS 657: Microwave RS - 19

AN A BIT MORE ESOTERIC THINK – PAIR –SHARE

Page 20: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

Franz J Meyer, UAF

GEOS 657: Microwave RS - 20

1. Explain what the “Spectrum (Fourier Representation)” of an Image represents

2. Assign the right spectrum to the right image:

3. Based on these image relationships above, which image parameter dictates how “wide” the spectrum of the image is?

Think – Pair – ShareWhat does the Spectrum of an Image Tell Us?

Image #1 Image #2 Image #3

Spectrum #A Spectrum #B Spectrum #C

Page 21: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

Franz J Meyer, UAF

GEOS 657: Microwave RS - 21

IMAGING RADAR – HOW IT’S REALLY DONE

Page 22: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

Franz J Meyer, UAF

GEOS 657: Microwave RS - 22

Some Problems with the Radar Imaging Concept

• Power 𝑷𝒓 of returned signal reduces rapidly the distance 𝑹 to the target

𝑃𝑟 ∝1

𝑅4𝑃𝑡 𝑤𝑖𝑡ℎ 𝑃𝑡 = 𝑡𝑟𝑎𝑛𝑠𝑚𝑖𝑡 𝑝𝑜𝑤𝑒𝑟

• For satellite applications: 𝑃𝑟 ≈1

400000000000000000000000∙ 𝑃𝑡!!!!!!!

For Satellite applications:Difficult to transmit a pulse that (1) has enough power to be able to detect backscattered response AND (2) is short enough to yield sufficient range resolution

Page 23: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

Franz J Meyer, UAF

GEOS 657: Microwave RS - 23

Most Radars Replace Pulse with Linear Frequency Modulated (Chirped) Signal

• Reason: Sending sufficient power in a single short pulse is near impossible

• Radars that send chirped signal are called “Pulse Compression Systems”

• Procedure:

1. Transmit frequency coded signal of length 𝜏𝑃2. Receive frequency coded echo

3. Compress frequency coded signal using a decoding operation called matched filtering

• What is the resolution of the compressed pulse?

– Ability to compress the pulse depends on the bandwidth 𝑊𝑃 of transmitted chirp signal

– The higher the bandwidth, the narrower the compressed pulse

→ 𝜏𝑃 =1

𝑊𝑃

Page 24: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

Franz J Meyer, UAF

GEOS 657: Microwave RS - 24

Achieving Good Range ResolutionThe Airborne Case

Page 25: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

Franz J Meyer, UAF

GEOS 657: Microwave RS - 25

Achieving Good Range Resolution The Spaceborne Case

transmitted signal echo of pulses

Use a focusing process to recover the smeared targets

Send a longer “chirped” signal to increase 𝑃𝑡

Page 26: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

Franz J Meyer, UAF

GEOS 657: Microwave RS - 26

Properties of the Frequency Coded (Chirped) Signal

• Chirp signal: 𝑢 𝜏 = 𝑒𝑥𝑝 𝑗𝜋𝑘𝜏2 = 𝑐𝑜𝑠 𝜋𝑘𝜏2 + 𝑗 ∙ 𝑠𝑖𝑛 𝜋𝑘𝜏2

Frequency 𝑓

Radar center frequency 𝑓0

Chirp rate 𝑘

Pchirp pulse duration:

Time 𝜏

Time 𝜏

Band

wid

th 𝑊

𝑃

Page 27: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

Franz J Meyer, UAF

GEOS 657: Microwave RS - 27

1. Data Acquisition:

Shape of compressed pulse

Range Compression by Matched Filtering (I)

logarithmic

-10 dB

-20 dB

resolutionlinear (magnitude) sinc

resolution

Side lobes

1. Transmit chirp instead of short pulse

2. Every point target will return chirp echo

3. Final range resolution after Range Compression: 𝜌𝑅 ≅𝑐

2𝑊𝑃

2. Range Compression:Correlate received signal with replica of

transmitted chirp

Page 28: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

Franz J Meyer, UAF

GEOS 657: Microwave RS - 28

Range Compression by Matched Filtering (II)

correlation

R

Focused pulse

reference chirp

signal

Page 29: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

Franz J Meyer, UAF

GEOS 657: Microwave RS - 29

Range Compression: Resolution-Bandwidth Duality

• You see two different chirps of identical duration but different chirp rates (𝑘 = 50 & 𝑘 =100 Hz/s)

• Higher chirp rate twice the bandwidth two times better resolution after correlation

Chirp BandwidthChirp in time domain

k =

10

0 H

z/s

k

= 5

0 H

z/s

Correlation Result

Page 30: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

Franz J Meyer, UAF

GEOS 657: Microwave RS - 30

Range Compression: Matlab Example (I)

Page 31: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

Franz J Meyer, UAF

GEOS 657: Microwave RS - 31

Range Compression: Matlab Example (II)

Page 32: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

Franz J Meyer, UAF

GEOS 657: Microwave RS - 32

Range Compression: Matlab Example (III)

Page 33: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

Franz J Meyer, UAF

GEOS 657: Microwave RS - 33

Chirp-Rate Error Effects – Matlab Example

𝑘𝑠: Chirp rate of

transmitted signal

𝑘𝑓: Chirp rate used

for focusing

Chirp rate errors

→ insufficient

focusing of

scattered energy

Page 34: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

Franz J Meyer, UAF

GEOS 657: Microwave RS - 34

Where Do Side-Lobes Come From?Effect of Windowing – Matlab Example (I)

Page 35: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

Franz J Meyer, UAF

GEOS 657: Microwave RS - 35

Where Do Side-Lobes Come From?Effect of Windowing – Matlab Example (II)

Page 36: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

Franz J Meyer, UAF

GEOS 657: Microwave RS - 36

EXAMPLES OF IMAGING RADAR DATA

Page 37: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

Franz J Meyer, UAF

GEOS 657: Microwave RS - 37

Side-Looking Airborne Radars (SLARs)

• Developed in 1950s driven by military

• Key element: Long antenna transmitting narrow fan-beams sideways from the aircraft

• Resolution defined by pulse length & length of antenna

• Resolution generally fair

Side-Looking Radars Use Pulse Compression to Increase Range Resolution

Flight direction

Pixel in a SLAR image

Pulse footprint

= along-track resolution

Pulse length = range resolution

Principle of a SLAR System

Page 38: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

Franz J Meyer, UAF

GEOS 657: Microwave RS - 38

Imaged (scanned)

area

Scanning Ground-based Radar System as a SLAR Example

• Resolution defined by pulse length & length of antenna

Imaging the Surface with SLARs

Radial decrease in

resolution

scan

direction

Page 39: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

Franz J Meyer, UAF

GEOS 657: Microwave RS - 39

Example of Scanning Ground-Based Radar Acquisition

• 180 degrees scan angle – location: Fairbanks, Alaska

Sensor Location

Decre

asin

g r

eso

lution (

in s

ca

n

dire

ctio

n)

with

ran

ge

Page 40: GEOS 657 MICROWAVE REMOTE SENSING...UAF Class GEOS 657 GEOS 657 –MICROWAVE REMOTE SENSING SPRING 2019 Lecturer: F.J. Meyer, Geophysical Institute, University of Alaska Fairbanks;

Franz J Meyer, UAF

GEOS 657: Microwave RS - 40

What’s Next?

• After improving resolution in range we also want to enhance the azimuth resolution of imaging radars

• Hence, next lecture (Tuesday 20-Feb-17) we will chat about something called “Aperture Synthesis” (the basis of Synthetic Aperture Radar)

• In preparation please read in Woodhouse (2006):

– Pages 271 – 280

– Specifically think about the two different interpretations of the aperture synthesis process (we will discuss those in class)