Lec 12 - Introduction to Thermal Infrared Flashcards

1
Q

Also known as longwave infrared (LWIR)

A

Thermal Infrared

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2
Q

It is the sensing of emissive energy or “temperature” energy

A

Thermal Infrared

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3
Q

Remote Sensing Measures (4)

A

(1) Land and Ocean Surface Temperature
(2) Atmospheric
(3) Radiation Balance
(4) Emissivity

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4
Q

It is the parameter indicating the energy and water exchange between the surface and the atmosphere.

A

Land and Ocean Surface Temperature

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5
Q

It measures temperature and amount of water vapor at different levels of the atmosphere

A

Temperature and humidity

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6
Q

Other gasses present in small amounts within the atmosphere.

A

Trace Gas Concentration

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7
Q

The balance between the radiant energy received by the Earth from the Sun and that returned by Earth to space

A

Radiation Balance

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8
Q

The ratio of the energy radiated from a material’s surface to that radiated from a perfect emitter (blackbody)

A

Emissivity

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9
Q

The measure of the motion of atoms and molecules in a substance

A

Temperature

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10
Q

Energy of particles of matter in random motion

A

Kinetic Heat

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11
Q

It can be measured using a thermometer

A

True Kinetic Temperature (Tkin)

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12
Q

The emitted EM radiation caused by the collision of particles with kinetic heat

A

Radiant Flux (Watts)

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13
Q

The amount of radiant flux emitted from an object

A

Radiant Temperature (Trad)

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14
Q

Relationship between Tkin and Trad

A

There is usually a high positive correlation between the true kinetic temperature of an object (Tkin) and the amount of radiant flux radiated from the object (Trad)

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15
Q

The most obvious source of EM radiation for remote sensing

A

Sun

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16
Q

The ratio of radiance spectrum of a non-perfect emitter over that of a perfect emitter (blackbody) at the same temperature.

A

Emissivity spectrum

17
Q

The perfect absorber and emitter

A

Blackbody

18
Q

The law states that, “The total energy emitted/radiated per unit surface area of a blackbody across all wavelengths per unit time is directly proportional to the fourth power of the black body’s thermodynamic temperature.

A

Stefan-Boltzmann Law

19
Q

This law states that black body radiation has different peaks of temperature at wavelengths that are inversely proportional to temperatures.

A

Wien’s Displacement Law

20
Q

This means reflectivity and emissivity has an inverse relationship; “good absorbers are good emitters” and “good reflectors are poor emitters”

A

Kirchoff’s Radiation Law

21
Q

The most commonly used method for land surface temperature (LST) retrieval from satellite data (Wang et. al, 2019)

A

Split-window algorithm

22
Q

The measure of the increase in thermal energy content (Q) per degree of temperature rise

A

Thermal/heat capacity (C)

23
Q

The rate at which heat will pass through a material

A

Thermal conductivity (K)

24
Q

The rate at which temperature can change within a body (energy loss / gain characteristics)

A

Thermal diffusivity (k)

25
Q

It is a measure of a substance’s ability to transfer heat in and out of that portion that received solar heating during the day and cools at night (cm^2/s)

A

Thermal diffusivity (k)

26
Q

The thermal response, delay in reaching ambient temperature following exposure to energy

A

Thermal inertia (P)

27
Q

The measure of the heat transfer rate across a boundary between two materials

A

Thermal inertia (P)

28
Q

Any pattern that recurs every 24 hours as a result of one full rotation of the planet Earth around its axis.

A

Diurnal cycle (or diel cycle)

29
Q

Thermal Properties of Water

A

(1) Cooler in the day and warmer in the night relative to other materials in the scene
(2) High thermal inertia, relative to typical land surfaces, as controlled largely by water’s high specific heat.

30
Q

A device designed to measure and detect thermal (heat) energy.

A

Thermal energy detector

31
Q

The basic principle is the conversion of heat into a measurable signal.

A

Thermal energy detector

32
Q

This produces a voltage when heated

A

Thermocouple

33
Q

It undergoes a change in electrical resistance when heated

A

Bolometer

34
Q

It is much more complex and expensive and is not used on the best-selling thermal camera models for various applications

A

Quantum detector

35
Q

It is sensitive to infrared radiation, which is a form of thermal energy.

A

Infrared (IR) Detectors

36
Q

It is temperature-sensitive resistors whose resistance changes significantly with temperature

A

Thermistors

37
Q

Common Satellite Sensors in Thermal IR

A

(1) Landsat 8
(2) NOAA AVHRR Band 4
(3) GOES, GMS, MOS 1, SeaWiFs, Nimbus CZCS (1 thermal), SeaSat, HCMM
(4) Ceres

38
Q

Thermal Infrared (TIR) Applications

A

(1) provide accurate distributions of surface spectral emittance and temperature
(2) Heat and moisture fluxes (exchanges)
(3) Climatological processes
(4) Evapo-transpiration
(5) Soil moisture variation
(6) Hydrology, oceanography and ocean currents
(7) Biomass distribution
(8) Vegetation monitoring
(9) Lithology & geology
(10) Urban land use
(11) Natural disaster monitoring
(12) Thermal pollution