Thermal Remote Sensing Flashcards

1
Q

Sources of shortwave Radiation

A

The sun
Reflections of EMR off the Earth

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2
Q

Sources of Longwave Radiation

A

Emission off the Earth

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3
Q

Relationship between longwave and shortwave

A

Blackbody Radiation Curves
Higher temp = shorter wavelength

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4
Q

Thermal Radiation definiton

A

Heat
Kinetic energy within an object due to random motion of particles then converted to EMR
Generally long wave

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5
Q

Temperature definiton

A

The measure of the average kinetic energy of particles in a substance
higher temp = higher velocity

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6
Q

Thermal specrum

A

3 - 14 um

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7
Q

Lowest temp on record

A

-89.2 c in Antartica

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8
Q

Highest temp on record

A

56.7 c in Death Valley CA

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9
Q

Why do TIR bands have lower spatial res than visible bands

A

Q = (hc)/v
Longer wavelengths have lower energy, they dont travel as far
TIR sensors have bigger IFOV to reliable catch enough energy

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10
Q

Air temp vs Surface temp in RS

A

RS measures surface temperature while weather stations measure air temp

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11
Q

Finding Temp with RS

A

Convert DNs to Top of Atmos (TOA) radiance
Convert TOA radiance to brightness temperature
Calculate emissivity
Calculate Land Surface Temperature (LST)

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12
Q

Emissivity definition

A

A surface materials effectiveness in emitting energy as thermal radiation
measured 0 to 1
Opposite Albedo

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13
Q

Types of Urban Heat Island effects

A

Surface Layer UHI
Canopy Layer
Surface
Boundary

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14
Q

Blackbody emissivity and problem

A

e=1
This is a theoretical entity, nothing we know of absorbs all EMR (except maybe the sun)

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15
Q

Graybodies

A

real objects that radiate less thermal energy than a blackbody

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16
Q

Urbanization definiton

A

population increase in proportion of people living in urban areas

17
Q

Land Use Land Cover Change (LULCC)

A

general term for the human modification of the Earth’s surface

18
Q

Impacts of Urbanization on Urban Climate

A

Increased air and surface temp
Increased surface run off
Decreased biodiversity
Downgraded air quality

19
Q

Urban Heat Island Effect definiton

A

Urban areas have higher temperature in comparison to surrounding rural areas

20
Q

Consequences of UHI effect

A

Increased energy and water consumption
Compromised human health and comfort
Downgraded air quality
Increased duration and magnitude of heat waves

21
Q

Boundary Layer UHI

A

Lowest part of the atmos
100 - 2000m above surface
Measured by weather baloons

22
Q

Surface layer UHI

A

Highest altitude of all the buildings and structures within a city
Measured by rooftop station or eddy-covariance flux tower

23
Q

Canopy layer UHI

A

Layer of air beneath the mean height of the buildings and trees
measured by weather stations 2m above ground

24
Q

Surface UHI

A

Remotely Sensed
Land Surface Temperature (LST)