2. Horizontal Positioning
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Undulating
Surface
Earth Mathematical Surface
Reference Ellipsoid
Reference Frame &
Datum
Best fit surface of Earth
Coordinate System
Horizontal Position
3. Process of Projection
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2. Project undulating geoid
to regular oblate spheroid
1. Defining Surface
topography wrt geoid
3. Projecting spherical into
map coordinate syetem
4. Projection System
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Physical model
Cylindrical Projection (Cylinder)
Tangent case
Secant case
Conic Projection (Cone)
Tangent case
Secant case
Azimuthal Projection (Plane)
Tangent case
Secant case
Distortion Properties
Conformal Projection (preserve
local angles and shape)
Equal Area or Equivalent (Area)
Equidistant (Scale along center
line)
Azimuthal (Directions)
6. Mapping Plane
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Plane in which the surface of earth
is projected.
Distortion is minimum at the point
of contact
Mapping involves transformation
of geographic coordinates
(∅, 𝛌) 𝐢𝐧𝐭𝐨 (𝐱, 𝐲) in terms of
easting and northing.
7. Conformal Projection
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Properties
Preserve Shape
(only for small areas)
Preserve Angles
Used for Large Scale Mapping
Distortion increases outwards from the
central meridian and standard parallel
Fig. Lambert conformal conic
projection
8. Distortion
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Conformal projection best suits for large scale map or
small area also scale remains moreover constant.
For small scale map, scale gets distorted.
Meridians and Parallels intersect at right angle.
Area and Length are affected due to conformal projection.
9. Lambert Conformal Conic Projection
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North Standard
Parallel
South Standard
Parallel
Parallel of
Grid Origin
(Base Parallel)
Central Meridian
Polar Axis
On development
Type: Conic & Secant
Property: Conformal
10. Transformation
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The coordinates from spherical datum can
be transformed to Lambert Conformal
Conic Projection by the following formulas,
where
λis longitude λ0 is reference longitude
ϕ1 and ϕ2 are reference parallels
ϕ0 is reference latitude.
ϕ is latitude.
11. Features
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Distances are true only along the standard parallels.
Other regions have reasonable accurate length.
Directions are reasonably accurate.
Distortions of shape is minimal at standard parallels
eg. Used for maps of North America with standard parallel 33N
and 45N with scale error of 2.5% for topographic maps.
12. Scale Error
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Map projection without distortions
would correctly represent shape, angle,
area, distance, direction anywhere on
the map.
Hence a map projection is associated
with scale distortions.
It depends on the size of area being
mapped and type of map projection
selected.
Fig. Scale distortion after
flattening
13. Singularity
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It is error encountered in
conformal map (at least one
point)
Green circle on map
represents 254 ° 33´.
The opposite pole is second
singularity which is absent on
map.
It can be mapped at infinity.
Fig. conic conformal map
Fig. Earth
15. Country using Lambert
Conformal Conic Projection
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USA
Belgium
France
Ireland
Fig. Map projection of International Map series
Source: Map projections for Europe (European Commission Joint
Research Center) Edited by A. Annoni, C. Luzet, E. Gubler, J. Ihde 2001
16. Advantage
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Angles and small shapes are preserved.
Minimum area distortion around standard parallel.
Accurate distance over standard parallel.
Best suited over middle latitudes and those having east-west
extent.
Limitation
Increase in distortions (shape, size and area) away form
standard parallels.
It cannot be used for thematic and statistical mapping.
Error due to Singularity.