1. Passive Microwave Remote Sensing

2. Passive Microwave Radiometry Microwave region: 1-200 GHz (0.15-30cm) Uses the same principles as thermal remote sensing Multi-frequency/multi-polarization sensing Weak energy source so need large IFOV and wide bands

3. Microwave Brightness Temperature Microwave radiometers can measure the emitted spectral radiance received (L  This is called the brightness temperature and is linearly related to the kinetic temperature of the surface The Rayleigh-Jeans approximation provides a simple linear relationship between measured spectral radiance temperature and emissivity

4. At long wavelengths, such as in the microwave region, the relationship between spectral emittance and wavelength can be approximated by a straight line.

5. Rayleigh-Jeans Approximation k is Planck’s constant, c is the speed of light,  is emissivity, T is kinetic temperature This approximation only holds for >> max (e.g. > 2.57mm @300 K) spectral radiance is a linear function of kinetic temperature a constant

6. Brightness Temperature  T is also called the “brightness temperature” typically shown as T B

7. Brightness temperature can be related to kinetic temperature through emissivity Thus, passive microwave brightness temperatures can be used to monitor temperature as well as properties related to emissivity

8. Microwave Radiometers Advanced Microwave Sounding Unit (AMSU) 1978-present Scanning Multichannel Microwave Radiometer (SMMR) 1981- 1987 Special Sensor Microwave/Imager (SSM/I) 1987-present Tropical Rainfall Measuring Mission (TRMM) 1997-present Advanced Microwave Scanning Radiometer (AMSR-E) 2002- present

9. Passive Microwave Radiometry Passive microwave sensors use an antenna (“horn”) to detect photons at microwave frequencies which are then converted to voltages in a circuit Scanning microwave radiometers –mechanical rotation of mirror focuses microwave energy onto horns

11. Passive Microwave Applications Soil moisture Snow water equivalent Sea/lake ice extent, concentration and type Sea surface temperature Atmospheric water vapor Surface wind speed Cloud liquid water Rainfall rate only over the oceans

12. Monitoring Temperatures with Passive Microwave Sea surface temperature Land surface temperature

13. Passive Microwave Sensing of Land Surface Emissivity Differences Microwave emissivity is a function of the “dielectric constant” Most earth materials have a dielectric constant in the range of 1 to 4 (air=1, veg=3, ice=3.2) Dielectric constant of liquid water is 80 Thus, moisture content affects brightness temperature Surface roughness also influences emissivity

14. Atmospheric Effects At frequencies less than 50 GHz, there’s little effect of clouds and fog on brightness temperature (it “sees through” clouds) Thus, PM can be used to monitor the land surface under cloudy conditions In atmospheric absorption bands, PM is used to map water vapor, rain rates, clouds

15. Atmospheric Mapping Mapping global water vapor 85 GHz

16. Passive Microwave Sensing of Rain Over the ocean: –Microwave emissivity of rain (liquid water) is about 0.9 –Emissivity of the ocean is much lower (0.5) –Changes in emissivity (as seen by the measured brightness temperature) provide and estimate of surface rain rate Over the land surface: –Microwave scattering by frozen hydrometeors is used as a measure of rain rate –Physical or empirical models relate the scattering signature to surface rain rates

17. Rainfall from passive microwave sensors: Accumulated precipitation from the Tropical Rainfall Measuring Mission (TRMM) Similar to SSM/I

18. Passive Microwave Remote Sensing from Space Penetration through non- precipitating clouds Radiance is linearly related to temperature (i.e. the retrieval is nearly linear) Highly stable instrument calibration Global coverage and wide swath Larger field of views (10-50 km) compared to VIS/IR sensors Variable emissivity over land Polar orbiting satellites provide discontinuous temporal coverage at low latitudes (need to create weekly composites) AdvantagesDisadvantages

19. Passive and Active Systems Passive remote sensing systems record electromagnetic energy that is reflected or emitted from the Earth’s surface and atmosphere. Active sensors create their own electromagnetic energy that 1) is transmitted from the sensor toward the terrain, 2) interacts with the terrain producing a backscatter of energy, and 3) is recorded by the remote sensor’s receiver.

20. Active Microwave Remote Sensing

21. Radar=Radio Detection and Ranging Radar system components

22. Radar: How it Works A directed beam of microwave pulses are transmitted from an antenna The energy interacts with the terrain and is scattered The backscattered microwave energy is measured by the antenna Radar determines the direction and distance of the target from the instrument as well as the backscattering properties of the target

23. Radar Parameters Azimuth Direction –direction of travel of aircraft or orbital track of satellite Range angle –direction of radar illumination, usually perpendicular to azimuth direction Depression angle –angle between horizontal plane and microwave pulse (near range depression angle > far range depression angle) Incident angle –angle between microwave pulse and a line perpendicular to the local surface slope Polarization –linearly polarized microwave energy emitted/received by the sensor (HH, VV, HV, VH)

24. Radar Nomenclature Nadir Nadir azimuth flight direction azimuth flight direction look direction look direction range (near and far) range (near and far) depression angle (  ) depression angle (  ) incidence angle (  ) incidence angle (  ) altitude above-ground-level, H altitude above-ground-level, H polarization polarization Radar Nomenclature Nadir Nadir azimuth flight direction azimuth flight direction look direction look direction range (near and far) range (near and far) depression angle (  ) depression angle (  ) incidence angle (  ) incidence angle (  ) altitude above-ground-level, H altitude above-ground-level, H polarization polarization

25. RADARlogicRADARlogic

26. Radar Pulse Length

27. Synthetic Aperture Radar Antenna “length” is increased synthetically by building up a history of backscattered signals from the landscape along the track of the sensor Implemented by keeping track of the Doppler shift of the reflected signal (frequency of the transmitted signal is known)

28. Doppler Offset A target's position along the flight path determines the doppler frequency of its echoes: targets ahead of the aircraft produce a positive doppler offset targets behind the aircraft produce a negative offset As the aircraft flies a distance (the synthetic aperture), echoes are resolved into a number of doppler frequencies. The target's doppler frequency determines its azimuth position.

30. Creation of the RADAR Image

31. Image Foreshortening Slopes that are facing the radar appear compressed (and bright) in the resulting image

33. Layover Layover occurs when the incidence angle (  ) is smaller than the foreslope (  + ) i.e.,  <  +. i.e.,  <  +. This distortion cannot be corrected!

35. Radar Shadowing Radar shadowing can be useful for interpreting geomorphological features

37. Radar Backscatter Power received = Power per unit area at target x Effective scattering area of the target x Spreading loss of reradiated signal x Effective receiving area of antenna

38. Radar Backscatter Coefficient The efficiency the terrain to reflect the radar pulse is termed the “radar cross-section”,  The radar cross-section per unit area, (A) is called the “radar backscatter coefficient” (  ˚) and is computed as : The radar backscatter coefficient determines the percentage of electro- magnetic energy reflected back to the radar from within a radar pixel This is similar to the reflectance in optical remote sensing

39. Radar Backscattering

40. Depends on the properties of the target: –roughness –dielectric constant Depends on characteristics of the radar: –depression angle –frequency/wavelength –polarization

41. Electrical (E) and magnetic field (B) are orthogonal to each other Direction of each field is perpendicular to the direction of wave propagation.

42. PolarizationPolarization

43. Polarization Plane polarized light can be either –vertically polarized (E 0 is perpendicular to the plane of incidence) –horizontally polarized (E 0 is parallel to the plane of incidence) Solar radiation is unpolarized (random) but can become polarized by reflection, scattering, etc. Lasers and radars produce polarized radiation

44. Radar Polarization Cinder cone and basalt lava flow in north-central Arizona. Strong return in the HH polarized image and weak HV polarization indicates that the lava is not depolarizing the radar pulse (it is composed of large blocks with smooth faces)

45. Rayleigh Criterion for Roughness A surface is considered smooth at or below a height, h, if: [ cm ] h = the vertical relief (average height of surface irregularities) = the radar wavelength (measured in cm)  = the depression angle

46. Surface Roughness in RADAR Imagery

47. Nile River Sudan SIR-C Color Composite: Red = C-band HV Green = L-band HV Blue = L-band HH Space Shuttle Color- Infrared Photograph C-band,  = 6cm L-band,  = 24cm

48. Radar and the Dielectric Constant Dielectric constant depends on the type of material as well as its moisture state –it is analogous to the refractive index of the material –it is primarily a function of moisture content –also depends on chemical properties such as salinity Dielectric constant is the ratio of the capacitance of a material to that of a vacuum. Also known as the “relative permittivity”

49. Dielectric Constant dielectric constant of liquid water is 80; dry soil is 2-4.

50. Radar frequency and backscatter Depth of radar penetration through the vegetation canopy varies directly with

51. Types of Active Microwave Surface and Volume Scattering that Take Place in a Hypothetical Pine Forest Stand

52. Response of A Pine Forest Stand to X-, C- and L-band Microwave Energy

53. SIR-C/X-SAR Images of a Portion of Rondonia, Brazil, Obtained on April 10, 1994

54. Cardinal Effect: High radar backscatter occurs when planar features or slopes are oriented perpendicular to the radar beam SIR-C/X-SAR radar image collected over the greater Los Angeles area on October 3, 1994.

55. Cloud Penetration C-, L-, and P- band radars are defined as “all weather” X-band radar does not penetrate heavy precipitation Only Ka band (0.8 - 1.1 cm) has some cloud mapping capability

56. Commonly Used Radar Frequencies