Lecture 3 - Georeferencing I Flashcards

1
Q

What is a map?

A

A to-scale representation (on a flat medium) of a selection of materials or abstract features on the earth’s surface.

  • shows more than just earth’s surface b/c it is loosely used to refer to the visual display of info
  • don’t always have to be fully accurate
  • geometric distortion is unavoidable in representation
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2
Q

What is the process of map making?

A
  1. Selection of few features that need to be included
  2. Simplification: involving elimination, aggregation, and smoothing (ex. of a jagged coastline)
  3. Exaggeration/displacement of included features that are too small to show at scale (ex. highways)
  4. Classification/attribute data manipulation to reduce complexity
  5. Symbolization: to represent different classes of features chosen
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3
Q

How are maps and GIS related?

A
  • maps are main data source for GIS
  • maps are analogue databases
  • GIS’ roots are in map analysis
  • GIS overcomes many limitations of paper maps
  • ex. London Underground map is distorted because we don’t care about actual distances, but the stop orders and interchanges (good use here)
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4
Q

What are the 2 broad classes of maps?

A
  1. Topographic map

2. Thematic map

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5
Q

What is a topographic map?

A
  • a reference map tool showing many natural/cultural geo features (ex. roads, water, elevation, vegetation, toponomy (labels))
  • ex. contour lines
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6
Q

What is a thematic map?

A
  • displays spatial patterns of one theme or set of attributes (communicates geographical concepts)
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7
Q

What are the 3 types of thematic maps?

A
  1. Choropleth map: uses zone to show data, like income, education, etc. (boundaries usually human imposed)
  2. Area class map: shows zones of constant attributes, like vegetation and soil types (boundaries are mixed and messy because they’re natural)
  3. Isoline map: shows imaginary surface by means of lines joining points of equal value (contours) - used for phenomena smoothly varying across a map (ex. air pressure, temperature)
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8
Q

What is map scale?

A

Scale: ratio b/w distances on map and corresponding distances in the real world (ground distance)

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9
Q

How can scale be represented?

A
  • verbally: 1 cm = 1 km
  • fraction: 1:100,000 (proportion)
  • graphic scale: line bar scale
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10
Q

Describe the difference between large-scale and small-scale maps

A

Large-scale: shows a small area in great detail (ex. 1:1,000)
Small-scale: shows large area in little detail (ex. 1:250,000)
To tell difference, 1/1,000 is bigger than 1/250,000

Deciding what is large or small is subjective and based on comparisons b/w maps

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11
Q

What is map generalization?

A
  • uses judgement in the elimination of detail/reduction of features
  • scale controls the degree of generalization (influences features shown and simplification)
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12
Q

What is the geometric process of map making?

A
  • methods of mapping ellipsoidal or spherical surfaces that are used to represent the earth
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13
Q

What is required to locate phenomena on earth?

A
  • a location system through a grid of lines
  • geographic coordinate system: specifies positions on the globe through latitude and longitude (E-W)
  • expressed in degrees, minutes, and seconds, or in decimal degrees
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14
Q

Explain latitude

A

It measures angular deviation north or south from the equator along a meridian.

  • equator is a reference plane used to define longitude (0 degrees latitude)
  • parallels are lines of equal latitude
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15
Q

Explain longitude

A

It measures the angle on the equatorial plane east to west b/w the meridian of the point and the central meridian through Greenwich, England

  • prime meridian is reference plane used to define latitude (0 degrees longitude)
  • meridians are lines of equal longitude
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16
Q

Explain the prime meridian

A
  • arbitrarily assigned by humans
  • division b/w E and W hemispheres
  • passes through Greenwich
17
Q

What is a graticule?

A
  • network of lines on a globe or map that represents lat and long
  • origin is at equator and prime meridian (0,0)
18
Q

Explain how lat and long are measured.

A
  • in: degrees° minutes’ seconds”
  • 60”=1’ and 60’=1°
  • 1 second is approx 100 ft
  • decimal degrees is best for GIS
19
Q

How do you convert from degrees, minutes, and seconds to decimal degrees?

A

dd = d° + m’/60 + s”/3600

  • make sure to use appropriate sign!
  • NE: ++ SE: -+ SW: – NW: +-
  • always carry at least 6 decimal places
20
Q

What is a grid?

A

a set of uniformly spaced straight lines intersecting at 90° angles
- use a grid where graticule is not high enough resolution (ex. small countries)

21
Q

What is the shape of the earth?

A
  • not a sphere, but a biaxial ellipsoid/spheroid (irregular)
  • not uniform (ocean is smooth while topography varies
  • it is a geoid (physical figure of the earth)
22
Q

What is the geoid?

A

Mathematical figure of the earth’s surface based on gravitational measurements/calculations

  • if the earth stopped spinning and everything settled it would look like this
  • can’t see it visually, so it is theoretical and modelled
23
Q

What is the surface composition of the earth?

A
  • topographic surface is the interface b/w the land and air and is complex/difficult to model (sharp and bumpy, like mountains and valleys)
  • the 3D best fit smooth surface of the geoid is the ellipsoid
  • the geoid goes above and below the idealized ellipsoid in certain places
24
Q

Which spheroid do we use?

A
  • wide variety depending on purpose

- ex. WGS84, Everest, etc.

25
Q

What is geodesy?

A

Process of measuring position (horizontal control) and elevation (vertical control) of points on earth’s surface (spheroid)

26
Q

What is geodetic surveying?

A
  • used to establish location of survey monuments
  • incorporates earth’s shape/curvature
  • good for large areas (ex. world)
27
Q

What is plane surveying?

A
  • assumes earth is flat
  • good for small geographic locations
  • uses survey monuments as starting points
28
Q

What is a datum?

A
  • reference mathematical model used for projection to geoid
  • formula that combines ellipsoid and its geoid to surveyed control points
  • basically, a reference point from which we measure something
29
Q

What is the difference between a horizontal and vertical datum?

A

Horizontal: precise location known and used as reference point
- make sure selected ellipsoid fits area of interest
Vertical: surface to which elevations are referenced
- ex. point that is 17m below sea level is reference for other buildings

30
Q

What is the difference b/w local and global datums?

A

Local: designed to fit specific area
Global: origin at centre of mass of earth; shape and size best possible approximation for geoid

31
Q

Briefly describe the history of North American Datums

A
  • 1900: first nationwide datum in US with 2,500 points (centre in Meades Ranch, Kansas)
  • NAD27: 25,000 stations
  • NAD83: uses satellites and 275,000 stations withe origin at the centre of the mass of the earth
  • CANNOT convert from NAD27 to NAD83
32
Q

Briefly describe the history of global datums

A
  • demand for global reference ellipsoids

- World Geodetic System 1984 (WGS84) most recent

33
Q

What equation is used to calculate orthometric heights?

A

Orthometric Heights = Ellipsoid Height +/- Geoid Undulation

H = h +/- N