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In these Lecture Slides, the primary aim of the Lecturer is to illustrate the following key points : Scale Factor, Map Projections, Mathematical Expression, Projection Termsa, Scale Factor, Principal Scale, Scale Factor, Projection Terms, Cylindrical, Azimuthal
Typology: Slides
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Map projection: a mathematical expression representing the 3D surface of the earth on a 2D map.
This processalways results in distortion to map properties: such as area, shape, or direction.
….hundreds of projections have been developed to best suit a particular type of map.
the distortion, flattening or stretching needs to be done systematically. (Watch video 3.5 min)
Literally projecting the globe onto a map … 3 of the earliest projections (by the ancient Greeks)
[Gnomon = pagan sundial]
For example, in any projection, where every line of latitude is equal in length (whereas the relative lengths on the globe are 1 at the equator, 0.5 at 60 latitude and 0 at the Poles),
The SF in the other direction (along meridians) may not be the same.
Conic Cylindrical Azimuthal (planar)
Distortion increases with distance between the ‘globe’ and the surface
c. Standard Line: The standard line is a line along which the scale factor equals 1 (often the point / line of contact)
Lines of latitude are 'parallel' and evenly spaced.
Meridians converge at the poles, half at 60 degrees.
All grid lines cross at right angles.
Scale factor is 1 in all directions.
‘Great circles’ are straight lines e.g. meridians, equator, 'straight' flight lines
Projections may preserve shape or area, … but NOT both area and shape.
A projection that maintains 'area' is equal area (or equivalent).
This is achieved by sacrificing shape: stretching in one direction to counter for earth curvature must be compensated by compaction in the other.
In other words, the product of the two Scale factors at any point in the two directions (N-S and E-W) is 1.0 (e.g 1 x 1, 2 x 0.5 etc..)
A projection that maintains shape is conformal or orthomorphic.
For example a 2x2 square becomes a 1x1 or 4x4 square. Stretching in one direction is matched by stretching in the other: that is, the scale factors are equal at a point in the two directions (i.e. there is 'equal-stretching').
Distances can be correct in one direction from a line, usually a standard line … or distances can be correct in all directions from a point.
In these cases, the projection is termed equidistant (but only N-S)
Plate Carrée projection Docsity.com
Conic Cylindrical Planar (azimuthal)
Sub-groups based on projection orientation ( normal , transverse, oblique)