Unit 8 Flashcards

1
Q

How is hyperspectral remote sensing different from multispectral?

A

It has 100s of bands that range spectral resolutions. Can estimate the relative abundance of certain features not just their presence or absence.

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2
Q

What is the benefit of imaging spectroscopy

A

Can use the full spectrum for analysis giving higher resolutions
= determine vegetation health, water content, types of vegetation etc.

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3
Q

How does a spectral sample from imaging spectroscopy differ from multispectral such as landsat

A

Instead of inferring the spectral signature from about 5 bands per pixel we have contiguous spectral bands giving a more accurate view of the signature

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4
Q

Where does the best spectroscopy occur currently?

A

Airborne, but increasing interest in spaceborne

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5
Q

Why is imaging spectroscopy area-based?

A

Since it flies over numerous targets there is gridded data that allow for formation of images based on the spectral bands

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6
Q

What are examples of airborne imaging spectrometers?

A

AVIRIS, AVIRIS-NG, CASI/SASI

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7
Q

How can we use a library of vegetation spectra?

A

TO map vegetation types and conditions

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8
Q

What are examples of space borne imaging spectrometers?

A

Hyperion, Hyspiri, ENMAP

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9
Q

What is the challenge of imaging spectroscopy and being area-based?

A

Have to tease out individual objects from the mixed pixels (spectral mixing) through unmixing methods

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10
Q

What is linear spectral unmixing?

A

Using information to determine the fraction or percentage of each feature from known/expected spectral signatures that they have

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11
Q

What is an endmember?

A

A pixel that is assumed to have a pure spectral signature for a given land cover class (Ie. open water)

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12
Q

What is a common method of unmixing in land use/land cover studies?

A

Sub-pixel fractions: applied to optical multi-spectral imagery to derive fractions of specific land cover types

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13
Q

What radiation does thermal remote sensing use?

A

emitted longwave radiation from emitted the earth’s surface (terrestrial)

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14
Q

What are the major uses of thermal remote sensing?

A

To monitor surface temp changes (dirunal, seaonal, interannual) + the earth’s energy budget

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15
Q

the internal true temperature of an object from the molecular vibrations

A

Kinetic temperature

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16
Q

define radiant temperature

A

result of emitted energy from an object also called the apparent or brightness temperature

17
Q

How does wein’s displacement law relate to thermal remote sensing?

A

All objects emit EM energy and the amount/wavelength is based on the temperature of the object. Hotter objects have smaller wavelengths (inverse relationship).

Therefore we can use this to distinguish features in thermal remote sensing

18
Q

What is a blackbody?

A

A theoretical object that is a perfect emitter and absorbs all energy = does not reflect anything

19
Q

What happens to emissivity if the radiant temperature is lower than the actual kinetic temperature of an object?

A

The emissivity will be low

20
Q

What example increases the emissivity?

A

Water content

21
Q

Are most thermal sensors imaging sensors?

A

Yes, in comparison LIDAR is not

22
Q

What are some examples of thermal imaging sensor missions?

A

Landsat, MODIS, ASTER, GOES, ECOSTRESS

23
Q

How can evaporation be used with thermal imaging?

A

Evaporation causes a slight decrease in temperature so we can infer water stress