map projections

42
MAP PROJECTIONS Cartographic Design for GIS (Geog. 340) Prof. Hugh Howard American River College

Upload: zaynah

Post on 14-Jan-2016

76 views

Category:

Documents


0 download

DESCRIPTION

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 Presentation

TRANSCRIPT

Page 1: MAP PROJECTIONS

MAP PROJECTIONS

Cartographic Design for GIS (Geog. 340)Prof. Hugh HowardAmerican River College

Page 2: MAP PROJECTIONS

MAP PROJECTION DEFINED

Page 3: MAP PROJECTIONS

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)

Page 4: MAP PROJECTIONS

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

Page 5: MAP PROJECTIONS

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

Page 6: MAP PROJECTIONS

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

Page 7: MAP PROJECTIONS

PROJECTION CLASSES (According to Projective Geometry)

Page 8: MAP PROJECTIONS

THREE CLASSESPlanar

CylindricalConic

PROJECTION CLASSESClassification According to Projective Geometry

Good for:Polar regions

Developable Surface

Page 9: MAP PROJECTIONS

THREE CLASSESPlanar

CylindricalConic

Good for:Equatorial regions

Developable Surface

PROJECTION CLASSESClassification According to Projective Geometry

Page 10: MAP PROJECTIONS

THREE CLASSESPlanar

CylindricalConic

Good for:Midlatitude regions

Developable Surface

PROJECTION CLASSESClassification According to Projective Geometry

Originally developed by Claudius Ptolemy, 2nd Century AD

Page 11: MAP PROJECTIONS

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

Page 12: MAP PROJECTIONS

PROJECTIONCASE and ASPECT

Page 13: MAP PROJECTIONS

PROJECTION CASE• Case

– Describes how the developable surface is positioned, relative to the reference globe

– Tangent– Secant

Page 14: MAP PROJECTIONS

PROJECTION CASE• Case (cont.)

– Lines of contact are Standard Lines

Standard Lines have same scale as reference globe

Distortion increases away from Standard Lines

Page 15: MAP PROJECTIONS

• 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)

Page 16: MAP PROJECTIONS

PROJECTION CLASSES (According to Properties Preserved)

Page 17: MAP PROJECTIONS

• 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)

Page 18: MAP PROJECTIONS

• Types of distortion:– Angle (shape)

– Area

– Distance

– Direction

PROJECTION CLASSESClassification According to Properties Preserved

Page 19: MAP PROJECTIONS

• 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

Page 20: MAP PROJECTIONS

• 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

Page 21: MAP PROJECTIONS

Conformal: Lambert Conformal Conic

FOUR CLASSESConformalEquivalentEquidistantAzimuthal

Good for:Topographic maps

Weather mapsNavigational maps

PROJECTION CLASSESClassification According to Properties Preserved

Page 22: MAP PROJECTIONS

Conformal: Mercator

FOUR CLASSESConformalEquivalentEquidistantAzimuthal

Good for:Topographic maps

Weather mapsNavigational maps

PROJECTION CLASSESClassification According to Properties Preserved

Page 23: MAP PROJECTIONS

Equivalent: Eckert IV

FOUR CLASSESConformalEquivalentEquidistantAzimuthal

Good for:Thematic mapsPolitical maps

PROJECTION CLASSESClassification According to Properties Preserved

Page 24: MAP PROJECTIONS

Equivalent: Sinusoidal

FOUR CLASSESConformalEquivalentEquidistantAzimuthal

Good for:Thematic mapsPolitical maps

PROJECTION CLASSESClassification According to Properties Preserved

Page 25: MAP PROJECTIONS

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

Page 26: MAP PROJECTIONS

FOUR CLASSESConformalEquivalentEquidistantAzimuthal

Conformal and Equivalent projections are mutually exclusive

No projection can be both conformal and Equivalent

PROJECTION CLASSESClassification According to Properties Preserved

Page 27: MAP PROJECTIONS

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)

Page 28: MAP PROJECTIONS

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)

Page 29: MAP PROJECTIONS

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

Page 30: MAP PROJECTIONS

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

Page 31: MAP PROJECTIONS

SELECTING an APPROPRIATE PROJECTION

Page 32: MAP PROJECTIONS

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.

Page 33: MAP PROJECTIONS

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)

Page 34: MAP PROJECTIONS

SELECTING A PROJECTION• World Map of Literacy Rates (choropleth)

Preserves relative areas of enumeration units

Page 35: MAP PROJECTIONS

SELECTING A PROJECTION

Page 36: MAP PROJECTIONS

SELECTING A PROJECTION• Map of Russian Population (proportional

symbol and dot)

Preserves relative areas of enumeration units

Page 37: MAP PROJECTIONS

SELECTING A PROJECTION

Standard Parallels located ~1/6 from top, and ~1/6 from bottom

Central Meridian located midway of E-W extent

Page 38: MAP PROJECTIONS

SELECTING A PROJECTION• Map of Kansas Tornado Paths (flow)

Angular relationships of paths are important

No need to preserve relative areas of

enumeration units

Page 39: MAP PROJECTIONS

SELECTING A PROJECTION

Lambert Conformal Conic

Page 40: MAP PROJECTIONS

SELECTING A PROJECTION

Albers Equal Area Conic

Virtually no difference!

The smaller the area, the less important the projection!

Page 41: MAP PROJECTIONS

SELECTING A PROJECTION

Lambert Conformal Conic

Lambert Conformal Conic would be the correct

choice…

Page 42: MAP PROJECTIONS

MAP PROJECTIONS

Cartographic Design for GIS (Geog. 340)Prof. Hugh HowardAmerican River College