map projection properties Flashcards

1
Q

Refrence globe

A

a model of the Earth at some chosen scale

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2
Q

Developable surface

A

a mathematically definable surface onto which the land masses and graticule are projected from the reference globe

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3
Q

List the 3 developable surfaces/ classes

A

cone - concical class
plane - planar class
cylinder - cylindrical class

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4
Q

Case

A

tangent
secant

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5
Q

Aspects

A

polar
equatorial
obligue

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6
Q

why does distortion occur?

A

There isn’t a constant scale on the earth’s surface because it is obligate ellipsoid. Distortion is inevitable.

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7
Q

scale factor

A

local scale / princicple scale

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8
Q

Tissot’s indicatrix

A

Provides a visual means of showing how distortion varies at point locations across a projection.
A quantitative analysis of distortion that describes the amount and type of distortion that occurs at points across the map

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9
Q

Azimuthal projections

A

preserve directions, only from centre of map to any other point along a great circle.
e.g Lambert equivalent

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10
Q

conformal projections

A

preserve angular relationships around a point
e.g Lambert conformal conic projection

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11
Q

Compromise projections

A

preserve no specific property, but rather strike a balance among various projection properties.
SF can be manipulated so that the extreme angular and aerial distortion found on equivalent and conformal.
e.g Robinson projection

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12
Q

equidistant projections

A

Preserving the principle scale between 2 points on a map. Distance can only be preserved in one direction.
e.g equirectangular cylindrical and Euler equidistant conic

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13
Q

What is distortion?

A

is the alteration of the size of the earth’s landmasses and the
arrangement of the earth’s graticule when they are projected to a 2D flat map

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14
Q

VIsual approach to distortion

A

visual comparison of the sizes of landmasses and the arrangement of the graticule on a projected map

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15
Q

Scale factor to analyse distortion

A

SF=is a numerical assessment of how the map scale at a location on the map compares with the principal map scale.
Compute how much deviation exists between the local scale and the principal scale at any location on a given projection. Variation in SF can be used to
quantify the distortion on the map for
different locations

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16
Q

Tissots indicatrix to analyse distortion

A

based on a unit circle
r-1.0, where all spatial relationships are preserved.
a=b=1
when a=b there is no distortion
when a=/b but a=1 then there is angular distortion
when a=b but a=/ 1 then aerial distortion takes place
when a=/b and a=/1 angular and aerial distortion occurs

17
Q

list the 4 projection properties

A

Areas
angles
distances
direction

18
Q

equivalent projections

A

preserves areas
e.g Albers equal area