Chapter 1 - Remote Sensing Flashcards

1
Q

Advantages of Remote Sensing

A

unobtrusive
systematic data collection - helps with sampling bias that is inherent in lots of GIS
provides fundamental information, unlike lots of GIScience

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2
Q

Limitations of Remote Sensing

A

Oversold sometimes
Human error introduced in design specifications
Active remote sensing that emits EMR (LIDAR, RADAR, SONAR) can be obtrusive
Can be expensive (greatest expense is a well trained analyst)
Machines can become uncalibrated

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3
Q

Remote sensing process

A
  1. Hypothesis to be tested is defined using a specific type of logic and appropriate processing model
  2. In situ data & collateral data necessary to calibrate remote sensor is collected
  3. Remote sensor data are collected (ideally at the same time as calibration data)
  4. In situ and remote sensor data are processed using analog, digital image processing, modelling, and n-dimensional visualization
  5. Metadata, processing lineage, and accuracy are provided & results communicated
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4
Q

Biophysical variables

A

Some can be measured with remote sensing such as:
water vapor in air
soil moisture
normalized difference vegetation index (nvdi)
etc.

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5
Q

Hybrid variables

A

modeled by combining other variables together

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6
Q

Active remote sensing (and what it’s input is a function of)

A

emit EMR, and reabsorb as L = f(lamba, sxyz, t, theta, P, omega)
where lamba = wavelength
sxyz = location of pixel and its size
t = temporal info
theta = angle between radiation source & terrain target of interest
P = polarization of back-scattered energy
omega = radiometric resolution

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7
Q

Spectral resolution

A

number and dimension of specific wavelength intervals (bands)

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8
Q

Nominal Spectral Resolution

A

What we call certain bands. Bands follow a gaussian distribution curve and are nominally defined/ separated at Full Width at Half Maximum of intensity

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9
Q

Hyperspectral

A

records hundreds of bands

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10
Q

Ultraspectral

A

records many hundreds of bands

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11
Q

Spatial resolution

A

smallest angular or linear separation between two objects that can be resolved by a remote sensing system.
Can be calibrated by placing black and white tarps on the ground, obtaining areal photography, computing # of resolvable line pairs per millimeter

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12
Q

Nominal Spatial Resolution

A

D = beta* H
diameter = instantaneous field of view * height above the ground
smaller = greater spatial resolving power
- historical landsat MSS data not useful for urban applications because of large spatial resolution
- rule of thumb: to detect a feature, resolution should be smaller than 1/2 of the smallest part of the feature

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13
Q

Sampling density

A

Some systems such as LIDAR use pulses of EMR at various time intervals - the spatial resolution applies to the pulse and reception of the pulse, but the sampling density is more important for analysis & has to do with interval/ frequency of observations

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14
Q

Temporal Resolution

A

How often samples of 1 location are taken

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15
Q

Nadir

A

The point directly below a satellite. Some satellites can sample off-nadir, which introduces Bidirectional Reflectance Distribution Function issues

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16
Q

Pulse length

A

length of time required to emit a pulse -> short = more precise distance measurement

17
Q

Radiometric resolution

A

Ability of a sensor to discern between greyscale levels, defined in bits

18
Q

Polarization

A

when waves aren’t distributed uniformly across all 360 degrees perpendicular to direction of propagation. Sunlight is weakly polarized, but becomes depolarized when it hits nonmetal objects.

19
Q

geniometer

A

documents changes in sensor radiance, L, caused by changing position of sensor & or source of illumination

20
Q

Pros/ Cons of suborbital viewing

A

Available on demand, higher resolution, available on demand

atmospheric turbulence can distort images & be difficult to correct for, expensive

21
Q

Analogue image processing pros/ cons

A

humans are great at compiling lots of info when looking at an image

precise measurement isn’t as easy, analysis isn’t repeatable, can’t store data,

22
Q

Radiometric correction of remote sensor data

A

noise or error introduced by the sensor may be able to be corrected for

23
Q

Geometric correction of remote sensor data

A

processes information so images are in proper place for GIS applications

24
Q

Hard vs. Fuzzy classification

A
hard = discrete mutually exclusive classes 
fuzzy = blend together
25
Q

Scene modeling components

A

1) scene model -> form & nature of energy & matter within scene & their spatial and temporal order
2) Atmospheric model -> relationship between atmosphere and energy entering & leaving
3) Sensor model -> behavior of sensor in response to energy influxes