Lecture 2 Flashcards

1
Q

what are the components of electromagnetic radiation

A

source / Atmospheric interaction / interaction with the earth’s surface / sensor

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2
Q

What are the sources of electromagnetic radiation

A

Natural radiation(1) sun - only in the day (2) any object on the earths surface above 0 kelvin emits energy. day or night Artificial radiation(3) the instrument itself, it fires a pulse and measures its return. day and night as not reliant on the sun

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3
Q

What is wavelength?

A

The distance between wave crests

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4
Q

What wavelength is blue

A

0.4-0.5 micro metres 400-500 nm

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5
Q

what wavelength is green

A

0.5 - 0.6 µm or 500 – 600 nm

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6
Q

what wavelength is red

A

0.6 - 0.7 µm or 600 – 700 nm

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7
Q

give examples of how The colour of objects is related to the way the reflect and absorb energy. Dark/light surface

A

A white surface reflects most of the light – reflect red/green and blue in equal parts ▪ A dark surface absorbs most of the light

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8
Q

explain the infrared wavelengths

A

(0.7 µm) to the microwave spectrum (1mm)
Near infrared (NIR) 0.7 – 1.0 µm
Shortwave IR (SWIR) 1.0 - 3.0 µm
Mid infrared (MIR) 3.0 – 5.0 µm
Far infrared (FIR) 5 µm – 1 mm

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9
Q

what is far infrared also known as

A

thermal infrared (radiation emitted from warm surfaces)

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10
Q

microwaves - wavelength

A

Wavelengths longer than Infra red (>1mm)

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11
Q

what are passive sensors (microwaves)

A

detect and respond to natural input from the physical environment-measure emitted energy ▪ related to the temperature and moisture properties of the surface

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12
Q

What are active sensors (microwaves)

A

generate their own energy ▪ backscatter related to the surface roughness

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13
Q

Why are microwaves useful

A

▪ All-weather capability ▪ can see through clouds ▪ not reliant on energy from the sun ▪ can operate at night – good for tropical regions as often cloudy.

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14
Q

Give two types of Natural radiation

A

solar radiation and Terrestrial radiation

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15
Q

Describe artificial radiation

A
  • Send its own source of energy pulse
  • Record the back scattered energy
    *Time taken by the pulse – can calculate height of objects on the surface.
  • Strength of echo received from the object
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16
Q

what are the two types of natural radiation and which wavelenfths are they

A

Reflected - visible, IR and MIR
Emitted - MIR and FIR

17
Q

All radiation used for remote sensing passes through the atmosphere before and after it has interacted with Earth surface. This alters the radiations…

A

▪ Speed
▪ Frequency
▪ Intensity
▪ Direction

18
Q

Give examples of Aerosols and gases in the atmosphere. what happens to them

A

dust, soot emitted from combustion processes or cars – concentration varies by time of day. some energy absorbed, some scattered and some passes through and measured by sensor.

19
Q

Amount of Atmospheric scattering depends on…

A
  • Size of the particle
  • Abundance of the particle – time of year for example
  • Wavelength of EMR – longer the wavelength the less impacted by atmospheric scattering
  • Depth of the atmosphere – elevation of sun in sky varies – energy passes through different depths of atmosphere.
20
Q

List 3 types of scattering

A
  1. Rayleigh Scattering
  2. Mie scattering
  3. Non-selective scttering
21
Q

Raleigh scattering

A

1890’s caused by gas molecules in the upper atmosphere
smaller than radiation wavelength.
as wavelength gets shorter scattering increases
Graph – blue part is more effected by Raleigh scattering than the red
This is why the sky is blue - in the day where the observer sees the scattered radiation
▪ also causes the red sky at sunset where red wavelengths are scattered due to the angle of the sun in the sky

22
Q

Mie Scattering

A

Larger particles. Can be emitted from anthropogenic activities like combustion.
Caused by water vapour, pollen, smoke particles & dust in lower atmosphere (troposhphere) – larger particle cannot rise so high in the atmosphere.
Mie scattering occurs when the diameter of atmospheric particulates are similar to or larger than the wavelengths of the scattered light

Scattering influences the wavelengths from the blue to middle infrared
▪ has a greater effect on radiation of longer wavelengths than Rayleigh scattering
Haze/pollution in the atmosphere causes scattering = worse in urban environments

23
Q

Non-selective

A

Particles much larger than incident radiation (e.g. water droplets and large dust particles)
▪ Takes place in lower atmosphere
▪ Not wavelength dependent as all wavelengths scattered equally
▪ E.g. clouds contain water droplets which scatter all visible wavelengths equally
▪ therefore clouds appear white – always when above them.

24
Q

The type of scattering occurs because of? (2)

A

The wavelength of the incident radiant energy. The size of the gas molecule, dust particle and or water vapour droplet encountered.

25
Q

What’s the difference between scattering and absorption?

A

Absorption = loss of energy, scattering is just moved

26
Q

Describe absorption in the atmosphere

A

Due to gasses in the atmosphere. Affects wavelengths that are shorter or longer than visible light. Energy absorbed in the atmosphere emitted at longer wavelengths (greenhouse gases). there is a loss of energy

27
Q

Give three common examples of gasses absorbed int he atmosphere

A

1) Ozone - high in the atmosphere - absorbed by Ultra Violet
2) Carbon Dioxide - lower in the atmosphere - absorbed by Mid and far/thermal infrared)
3) Water vapour - lower in the atmosphere - absorbed by far infrared.

28
Q

What are atmospheric windows?

A

Areas that are not absorbed - appear white on the graph. satellites make measurements in these areas.

29
Q

What wavelength range does the sun emit the most energy?

A

Visible light – 0.4um to 0.7um

30
Q

Name 3 sources of EMR?

A

Natural 1)The sun – only in the day
2) Terrestrial (objects on the earth’s surface and the earths surface itself) because some energy is absorbed and then reemitted – causing urban heat islands.
Artificial: 3) Active sensor - from satellites etc.

31
Q

Name 3 types of atmospheric scattering?

A

Raleigh, Mie and non-selective
Scattering is removed from the data (atmospheric correction)