map projections
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MAP PROJECTIONS. Cartographic Design for GIS (Geog. 340) Prof. Hugh Howard American River College. MAP PROJECTION DEFINED. MAP PROJECTION. Method by which Earth’s geographic coordinates are converted to projected (Cartesian) coordinates The “flattening” of Earth onto a plane. - PowerPoint PPT PresentationTRANSCRIPT
MAP PROJECTIONS
Cartographic Design for GIS (Geog. 340)Prof. Hugh HowardAmerican River College
MAP PROJECTION DEFINED
MAP PROJECTION• Method by which Earth’s geographic
coordinates are converted to projected (Cartesian) coordinates
• The “flattening” of Earth onto a plane
Geographic Coordinates (lon,lat) Projected (Cartesian) Coordinates (x,y)
MAP PROJECTION• A great challenge faced by ancient
(and modern) cartographers– Ancient Babylonians introduced the idea
of scale, and 360 degrees in a circle– Ancient Greeks introduced the idea of
meridians and parallels (diaphragma)– Claudius Ptolemy introduced the idea of
map projections in the 2nd century AD
Claudius Ptolemy, 2nd Century AD
MAP PROJECTION• How are projections created?
– Today, most projections are created mathematically using computers
– A Reference Globe is created as a scale model of Earth
– A “rule” is derived that can be applied to every point on the globe
MAP PROJECTION• Projective Geometry has been used to
create projections, and still serves as a conceptual explanation
– A semi-transparent reference globe is fitted with a Point of Projection
– Surface of reference globe is projected onto a Developable Surface
– Surface is traced on developable surface
PROJECTION CLASSES (According to Projective Geometry)
THREE CLASSESPlanar
CylindricalConic
PROJECTION CLASSESClassification According to Projective Geometry
Good for:Polar regions
Developable Surface
THREE CLASSESPlanar
CylindricalConic
Good for:Equatorial regions
Developable Surface
PROJECTION CLASSESClassification According to Projective Geometry
THREE CLASSESPlanar
CylindricalConic
Good for:Midlatitude regions
Developable Surface
PROJECTION CLASSESClassification According to Projective Geometry
Originally developed by Claudius Ptolemy, 2nd Century AD
THREE CLASSESPlanar
CylindricalConic
Mathematical ProjectionsSome projections are developed mathematically, not according to projective geometry; developable
surfaces are not involved.Pseudocylindrical, Sinusoidal, etc.
PROJECTION CLASSESClassification According to Projective Geometry
PROJECTIONCASE and ASPECT
PROJECTION CASE• Case
– Describes how the developable surface is positioned, relative to the reference globe
– Tangent– Secant
PROJECTION CASE• Case (cont.)
– Lines of contact are Standard Lines
Standard Lines have same scale as reference globe
Distortion increases away from Standard Lines
• Aspect – The orientation of the developable
surface, relative to the reference globe
PROJECTION ASPECT
Equatorial Aspect Polar/Transverse Aspect
Oblique Aspect(Mercator) (Transverse Mercator)
(Oblique Mercator)
PROJECTION CLASSES (According to Properties Preserved)
• Distortion always results from the projection process– The larger the area of Earth projected, the
greater the distortion – Smaller areas are subject to less distortion
PROJECTION CLASSESClassification According to Properties Preserved
Smaller Area (closer to flat)Large Area
(strongly curved)
• Types of distortion:– Angle (shape)
– Area
– Distance
– Direction
PROJECTION CLASSESClassification According to Properties Preserved
• Projections can be classified according to the type of distortion they do not produce…
• Projections can be classified by the Properties They Preserve– Angle (shape)
– Area
– Distance
– Direction
PROJECTION CLASSESClassification According to Properties Preserved
• Conformal projections:– Preserve Angles (shapes of small areas)
• Equivalent (Equal Area) projections:– Preserve relative sizes of Areas
• Equidistant projections:– Preserve Distances…
• Azimuthal projections:– Preserve Directions…
PROJECTION CLASSESClassification According to Properties Preserved
Conformal: Lambert Conformal Conic
FOUR CLASSESConformalEquivalentEquidistantAzimuthal
Good for:Topographic maps
Weather mapsNavigational maps
PROJECTION CLASSESClassification According to Properties Preserved
Conformal: Mercator
FOUR CLASSESConformalEquivalentEquidistantAzimuthal
Good for:Topographic maps
Weather mapsNavigational maps
PROJECTION CLASSESClassification According to Properties Preserved
Equivalent: Eckert IV
FOUR CLASSESConformalEquivalentEquidistantAzimuthal
Good for:Thematic mapsPolitical maps
PROJECTION CLASSESClassification According to Properties Preserved
Equivalent: Sinusoidal
FOUR CLASSESConformalEquivalentEquidistantAzimuthal
Good for:Thematic mapsPolitical maps
PROJECTION CLASSESClassification According to Properties Preserved
FOUR CLASSESConformalEquivalentEquidistantAzimuthal
Conformal and Equal Area projections are mutually exclusive
No projection can be both conformal and Equal Area
!
PROJECTION CLASSESClassification According to Properties Preserved
FOUR CLASSESConformalEquivalentEquidistantAzimuthal
Conformal and Equivalent projections are mutually exclusive
No projection can be both conformal and Equivalent
PROJECTION CLASSESClassification According to Properties Preserved
Equidistant: Azimuthal Equidistant
FOUR CLASSESConformalEquivalentEquidistantAzimuthal
Good for:Airline distance maps
Seismic maps
PROJECTION CLASSESClassification According to Properties Preserved
Distances are correct from the center of the projection, to all other locations(and along standard lines)
Azimuthal: Loximuthal
FOUR CLASSESConformalEquivalentEquidistantAzimuthal
Good for:Navigational maps
PROJECTION CLASSESClassification According to Properties Preserved
Directions are correct from the center of the projection, to all other locations(and along standard lines)
Robinson
FOUR CLASSESConformalEquivalentEquidistantAzimuthal
Compromise ProjectionsDistort shape, size, distance, and direction,
but distribute distortion in a way that looks natural
Good for:Non-critical applications
PROJECTION CLASSESClassification According to Properties Preserved
FOUR CLASSESConformalEquivalentEquidistantAzimuthal
Compromise ProjectionsDistort shape, size, distance, and direction,
but distribute distortion in a way that looks natural
Good for:General, non-critical
applications
PROJECTION CLASSESClassification According to Properties Preserved
Van der Grinten
Winkel Tripel
SELECTING an APPROPRIATE PROJECTION
SELECTING A PROJECTION• Selection of an appropriate projection
requires consideration of– Data– Symbolization method– Intended audience– Region of Earth– Map scale– Level of generalization, etc.
SELECTING A PROJECTION• John Snyder’s Guidelines provide a
hierarchical mechanism for choosing projections, based on
– Region to be mapped (world, hemisphere, continent or smaller)
– Desired projection property (conformal, equivalent, azimuthal, equidistant)
– Desired projection characteristic (class, case, aspect)
SELECTING A PROJECTION• World Map of Literacy Rates (choropleth)
Preserves relative areas of enumeration units
SELECTING A PROJECTION
SELECTING A PROJECTION• Map of Russian Population (proportional
symbol and dot)
Preserves relative areas of enumeration units
SELECTING A PROJECTION
Standard Parallels located ~1/6 from top, and ~1/6 from bottom
Central Meridian located midway of E-W extent
SELECTING A PROJECTION• Map of Kansas Tornado Paths (flow)
Angular relationships of paths are important
No need to preserve relative areas of
enumeration units
SELECTING A PROJECTION
Lambert Conformal Conic
SELECTING A PROJECTION
Albers Equal Area Conic
Virtually no difference!
The smaller the area, the less important the projection!
SELECTING A PROJECTION
Lambert Conformal Conic
Lambert Conformal Conic would be the correct
choice…
MAP PROJECTIONS
Cartographic Design for GIS (Geog. 340)Prof. Hugh HowardAmerican River College