Lecture 13 Flashcards

1
Q

Microwave region

A

1-200 GHz (0.15-30cm)

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2
Q

Characteristics of microwave radiometry

A
  • All weather (cloud penetration–longer wavelength)
  • Daily or better coverage
  • Multi-frequency/channel
  • Long record (since late 60s)
  • Large footprint
  • Hole at the pole
  • Does not rely on sun as source of illumination
  • Weak energy source so need large IFOV (bigger pixel size). Special resolution because signal is weak, so need bigger area.
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3
Q

Is radiant temperature equal to kinematic temperature?

A

NO. except for a blackbody. Almost all natural surface are gray bodies (absorb EMR).

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4
Q

Emissivity is a ratio of what?

A

Ratio of radiant emittance relative to that of a blackbody

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5
Q

Emissivity is what kind of quantity?

A

Emissivity is a spectral quantity (it varies with wavelength)

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6
Q

What is a selective radiator?

A

Materials that have variable emissivity are “selective radiators”–all natural surfaces

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7
Q

What does Planck’s Blackbody Equation do?

A

Describes the spectral distribution (wavelength) of emitted energy as a function of temperature

amount of energy at each wavelength at a given temp

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8
Q

What does Stefan-Boltzmann Law do?

A

the TOTAL power (energy) emitted from a blackbodygraybody is proportional to the 4th power of temperature (area under the Plank Law curve)

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9
Q

What does Wien’s Law do?

A

there is a maximum wavelength at which a blackbody radiates and this is determined by temperature

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10
Q

What does Rayleigh-Jeans approximation do?

A
  • Approximation of Planck’s Law
  • Works because part of Panck’s approaches zero at long wavelengths
  • valid for most microwave applications
  • MW radiometers measure brightness temperature, which when we know emissivity tells us kinematic (physical) temp
    (Brightness temp is linearly related to the kinematic temperature of the surface)
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11
Q

Dielectric constant

A

related to conductivity of material

  • measurement of how well radar energy will be moved to a depth. It therefore it measures velocity of propagating radar energy
  • 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
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12
Q

Why does moisture content affect brightness temperature

A

Dielectric constant of liquid water is very high, and wavelength and velocity reduce (speed penetrating surface)

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13
Q

Snow emissivity

A

soil vs dry snow vs wet snow–wet snow is a strong absrober/emitter

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14
Q

Atmospheric Effects and Passive Microwave

A
  • Atmospheric attenuation increases with frequency from 1 to 1000 GHz
  • 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
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15
Q

Passive Microwave Radiometry – how scan/sensors work

A
  • sensors use an antenna to detect photons * then converted to voltages in a circuit
  • mechanical rotation of antenna, or platform, or fixed antenna and oscillating mirror
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16
Q

PM sensors

A
  • ESMR (Nimbus 6 and 7)
  • SMMR (Nimbus 7)
  • SSM/I (DMSP)
  • TRMM TMI
  • AMSR
17
Q

AMSR acronym

A

Advanced Microwave Scanning Radiometer

18
Q

TRMM TMI acronym

A

Tropical Rainfall Measuring Mission (TRMM) Microwave Imager (TMI)

19
Q

SSM/I

A

DMSP Special Sensor Microwave/Imager

20
Q

Passive Microwave Applications

A
  • Soil moisture
  • Snow water equivalent
  • Sea/lake ice extent, concentration and type
  • Snowmelt
  • Sea surface temperature
  • Atmospheric water vapor
  • Surface wind speed
  • Cloud liquid water
  • Rainfall rate