reflectance Flashcards

1
Q

incident energy

A

energy from the sun that reaches the earth’s surface. It can be:
- absorbed
- reflected
- transmitted

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2
Q

incident energy equation

A

incident energy (Ei) = reflected energy (Er) + absorbed energy (Ea) + transmitted energy (Et)

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3
Q

what satellites measure

A

reflected energy in W/m^-2
- Er depends on the amount of incident radiation + reflection properties of surfaces
Er = Ei - (Ea + Et)

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4
Q

Reflectance curve

A

X-axis: wavelength
Y-axis: reflectance
- shows what wavelengths are getting reflected back depending on the band/item

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5
Q

what percent of energy is reflected by an object

A

Reflected energy / incident energy

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6
Q

red edge

A

Transition of absorption between green to IR can be used to identify plants

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7
Q

in plants: when moisture content is high, there’s ____ absorption

A

more
- May be helpful in measuring leaf status

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8
Q

how to distinguish clouds vs snow

A

clouds: reflect high in all wavelengths
snow: reflect high in visible to near IR, absorb more in mid-IR and beyond

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9
Q

what affects spec. curves in plants

A
  • height of plant
  • time of year
  • if it’s been watered recently
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10
Q

reflectance vs radiance

A

radiance: total energy measured at the satellite
- highest in blue b/c it scatters the most
reflectance: % of incident energy reflected
- because of differences in magnitude of EM radiation across wavelengths, these curves look very diff

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11
Q

specular reflection

A

angle of reflection = angle of incidence
- mirror like reflections
- Usually happens equally across wavelengths
i. Doesn’t contain information about the color of what you’re looking at
1) When you’re looking at a mirror, you can’t tell what it’s made of just by looking at it; you’re only looking at your reflection

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12
Q

difuse reflection

A
  • reflect uniformly in all directions
  • contains spectral information about the reflecting surface
    !! what we want to measure in remote sensing !!
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13
Q

types of reflectors

A
  • ideal specular reflector
  • near perfect specular reflector
  • near-perfect diffuse reflector
  • ideal diffuse reflector
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14
Q

ideal specular reflector

A

one to one; angle of incidence is exactly angle of reflection

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15
Q

near perfect specular reflector

A

angle of incidence is angle of reflection, but some diffusion occurs

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16
Q

near-perfect diffuse reflector

A

almost perfect equal reflectance in all directions, but small angle of reflection

17
Q

ideal diffuse reflector

A

perfectly equal reflection in all directions

18
Q

Something that’s more textured relative to the wavelength will cause __ reflectance

A

Something that’s more textured relative to the wavelength will cause more reflectance

19
Q

sun-sensor geometry

A
  • affects reflectance measured by a remote sensing instrument
  • this relative positions of the sun, sensor, and object cause geometric effects on irradiance
20
Q

sun sensor geometry: angles

A

solar elevation angle: angle between sunlight and ground
viewing angle: between camera and object
azimuth angle: ground angle between camera and sun

21
Q

differential shading

A

the sensor receives more info from one side of an object than the other bc that’s where the sun is hitting it

22
Q

differential scattering

A

a. When light is preferentially scattered in a certain direction
b. Often in mie scattering
c. Can mean light is inconsistent across angles
i. The magnitude of haze can affect the imaging

23
Q

specular reflection

A

Different distortion across different parts of the image based on the viewing angle
- i.e. a bright spot in a body of water

24
Q

bidirectional reflectance distribution function

A

mathematical function that predicts for a given object, what reflectance will be at any viewing angle and sun elevation angle
- If you’re looking at something from a particular angle and if the light source is coming from a particular angle, it predicts the reflectance
- Property of a feature
Calculated with light and viewing angle

25
BRDF and spheres example
each sphere's BRDF describes its reflectance in terms of wavelength, illumination, and viewing angle - They look different because they're made of different things, and thus have different BRDFs ○ They reflect differently and have different wavelengths Specular and diffuse reflection also depends on the type of material
26
BRDF in remote sensing: example
If amazonian rainforest get greener during the dry season § The first group; looked greener because they weren't correcting for the BRDF § Gave the illusion that it was greener during the dry season ○ THUS: correcting for the BRDF can affect findings § Most satellite data we collect is corrected for already
27
satellites and reflectance
Reflectance: what a satellite is seeing - reflected light must travel twice thru the atmosphere - Some scattering happens as light returns to the sensor - Sensor picks up path radiance
28
path radiance
scattered light that the sensor is seeing that's not reflected off of whatever the sensor is focused on
29
TOA vs surface energy
TOA: top of atmosphere - to understand surface features, need to convert energy measured at the satellite to energy measured at the surface
30
gamma and x-rays
almost fully blocked by the atmosphere, therefore of no use in satellite remote sensing - Cant make it thru atmosphere so not used in satellite, but used in outer space analysis
31
UV wavelengths
0.01 - 0.4 nm - mostly blocked by the earth's atmosphere - some applications for mapping oil spills
32
visible wavelengths
0.4-0.7 nm - atmospheric windows allow most visible light through - panchromatic imagery - measures reflectance in all visible wavelengths
33
infrared
near IR - many applications: vegetation monitoring; delineating water bodies shortwave IR - 1.4 - 3nm - applications: soil moisture; vegetation water content; geology - can penetrate clouds
34
far infrared
3-10,000 nm - emitted by warm objects - used to measure earth surface temperatures, detect fires
35
microwave
- 0.1-3.0 cm - RADAR wavelengths - little solar radiation in this range, so typically requires active sensors - influenced by soil moisture, 3d structures of earth surface features - can penetrate clouds