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Radar Mapping. Electromagnetic EM Radiation Electric Field & Magnetic Field –Perpendicular to direction of propagation Explains light but is absolutely.

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Presentation on theme: "Radar Mapping. Electromagnetic EM Radiation Electric Field & Magnetic Field –Perpendicular to direction of propagation Explains light but is absolutely."— Presentation transcript:

1 Radar Mapping

2 Electromagnetic EM Radiation Electric Field & Magnetic Field –Perpendicular to direction of propagation Explains light but is absolutely fundamental for radio spectrum

3 Typical Radar System 1.A pulse generator that discharges timed pulses of microwave/radio energy 2.A transmitter 3.A duplexer that alternates the signals involved between transmitted and received 4.A directional antenna that shapes and focuses each pulse into a stream 5.Receiving Antenna

4 Radar Bands 1.Ka Band: Frequency 40,000-26,000 MHz; Wavelength (0.8-1.1 cm) 2.K Band: 26,500-18,500 MHz; (1.1-1.7 cm) = Weather Radar 3.X Band: 12,500-8,000 MHz; (2.4-3.8 cm) 4.C Band: 8,000-4,000 MHz; (3.8-7.5 cm) 5.L Band: 2,000-1,000 MHz; (15.0-30.0 cm) 6.P Band: 1,000- 300 MHz; (30.0-100.0 cm) These are all in the Microwave part of the spectrum

5 About Radar RADAR = RAdio Detection And Ranging Typically radar transmitters send and receive 1500 pulses per second Pulses last about.1 microsecond Pulses send 100-1000 waves What a radar actually measures is time (between transmission and reception) What a radar actually receives when it’s pointed in a certain direction isn’t always in that direction

6 Some Radar Effects

7 Bright = rough, Dark = smooth Metal reflects brightly Metal corners or edges reflect especially brightly –A truck has same size radar signature as a bomber –Stealth = eliminate sharp edges and conductive materials Look direction = Illumination on Image

8 What Determines Radar Echo Electrical properties of material (Dielectric Constant) –Conductive = High Dielectric Constant = Reflective –Non-conductive = Low Dielectric Constant = Non-Reflective Roughness –Can’t “see” things smaller than wavelength –Corners are effective for scattering

9 Some Dielectric Constants Air: 1 Teflon: 2 Glass: 5-10 Water: 80

10 Radar Image of ISS

11 Radar and Optical

12 Stereoscopic SLAR

13 Radar Stereoscopy Although radar images can be viewed to give a 3-dimensional appearance, true photogrammetry is far more complex than with optical imaging. It can be done, although when NASA began radar mapping of Venus they didn’t yet have the ability.

14 Light and Radar

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16 Light Vs. Radar

17 How Time = Illusion

18 Radar Foreshortening With optical foreshortening, the facing side of a mountain looks normal and the back side looks compressed With radar foreshortening, the facing side of a mountain looks normal and the back side looks longer Layover: On steep slopes objects may appear to overlap because they’re the same distance (time) away.

19 Light vs. Radar

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21 Layover

22 Radar Foreshortening

23 Layover and Foreshortening

24 Underwater Radar?

25 Sonar View

26 How Time = Illusion

27 Sonar Views of Shipwrecks

28 German Bomber

29 Polarization Radar signals are polarized parallel to their transmitting antenna H (horizontal) polarization = parallel to bottom of plane When signals scatter, some of the polarization is lost What we see depends on the orientation of the receiving antenna

30 Polarization Imagine a signal from a perfectly horizontal antenna It bounces off a perfectly flat surface perpendicular to the beam A receiver parallel to the transmitting antenna will get 100% return A receiver perpendicular to the transmitting antenna will get 0% return

31 HV vs. HH

32 Multiband Color Composite

33 Alaska Coast

34 Reflectivity and Penetration, Florida

35 Reflectivity, Southern California

36 IR + Radar

37 Radar Penetration of Sand, Sudan

38 Ground Penetrating Radar

39 Optical and Radar Imagery

40 TOPEX/Poseidon

41 The Sea Is Not Flat

42 Pacific Ocean Sea Surface Changes

43 Sea Surface Radar Mapping

44 2004 Tsunami

45 Global Wind Speed and Wave Heights

46 Radar Image of Hawaii

47 Lidar LIght Detection And Ranging Uses laser pulses to measure distance Anything that affects light affects Lidar –Blocked by clouds, smoke, aerosols –Can monitor clouds, smoke, aerosols Records distance and direction Depending on processing, can image vegetation canopy or ground

48 Lidar

49 Mount St. Helens

50 Neolithic Mound, Slovakia

51 Hopewell Mounds, Ohio

52 Hopewell Mounds Ground View

53 Caracol, Belize

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56 Caracol, Belize, Point Cloud

57 Bainbridge Island, WA

58 Tacoma Fault and Glacial Troughs


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