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Projections 2011

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    Map Projections andCoordinate Systems

    Jan-Van Sickle

    Khang-tsung Chang

    ESRI Using ArcMap

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    Basic Map projection Types Conformal: preserves local shapes and angles

    Equivalent/equal area: represents areas in correctrelative size (shapes not preserved)

    Equidistant: preserves consistency of scale along

    certain lines Azimuthal: preserves accurate directions (e.g.,

    angles preserved, but length of lines is not)

    Property is often included in name (e.g., Lambertconformal conic projection)

    Map can have more than one property, but conformaland equivalent are mutually exclusive

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    Conformal projections

    Conformal projections preserve local shape.

    To preserve individual angles describingthe spatial relationships, a conformal

    projection must show the perpendicular

    graticule lines intersecting at 90-degree

    angles on the map.

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    Equal area projections

    Equal area projections preserve the area

    of displayed features. To do this, the otherpropertiesshape, angle, and scalearedistorted. In equal area projections, the

    meridians and parallels may not intersectat right angles.

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    Equidistant projections

    Scale is not maintained correctly by any

    projection throughout an entire map;however, there are, in most cases, one or

    more lines on a map along which scale is

    maintained correctly. Most equidistant

    projections have one or more lines for

    which the length of the line on a map is thesame length (at map scale) as the same

    line on the globe.

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    True-direction or Azimuthal

    projections

    True-direction,orazimuthal, projections give the

    directions or azimuths of all points on the mapcorrectly with respect to the center. Some true-direction projections are also conformal, equalarea, or equidistant.

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    Examples

    Planer Projections

    Polar Map Projections

    Secant Map Projections

    Simple Conic Projections Lambert Conic Projection

    Cylindrical Projections

    Universe Transverse Mercator

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    Planar Projections

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    Plane Polar Map Projections

    One tangent plane

    A plane touching the globe at a single

    point

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    Question

    Is the Polar Projection an Azimuthal

    Projection?

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    Answer

    YES:

    Direction of any line from the central tangent

    point on the map to any other point

    represents the actual direction of the line.Preserves accurate directions (e.g., angles

    preserved, but length of lines is not)

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    1 - Stereographic

    Imaginary light source

    on the opposite pointof tangency

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    Question

    Is the stereographic projection a Conformal

    projection (i.e., preserves shapes)?

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    AnswerConformal: preserves

    local shapes andangles

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    Question

    Where is the no distortion (of scale) zone

    on the map?

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    Answer

    Center of map

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    Question

    Where on the map does distortion increase?

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    Answer

    Away from the Center

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    Rule

    The point (standard point) or the line

    (standard line) where a map & a globetouch are the only locations on the map

    where there are no distortions

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    2 - Gnomonic Imaginary light source

    at the center of theglobe

    Conformal: preserveslocal shapes and

    angles

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    Modifications to Decrease

    Distortions

    Basis: Decrease the distance between the

    map projection surface and the ellipsoidal

    surface

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    Surface cuts theellipsoid

    The area where

    distortion is inacceptable range is

    increased

    Secant Projection

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    Simple Conic Projections

    The most simple conic projection is tangent to the

    globe along a line of latitude. This line is called the

    standard parallel.Straight converging lines (meridians) and concentric

    circular arcs (parallels). Central meridian center of

    map.

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    QuestionFor Simple Conic Projections

    Distortion increases as you move

    away (E or W) from the Central Meridian

    away from the standard parallel (approach pole)

    Conic projections are used for mid-latitude

    zones that have an EW orientation (True or False)

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    Answer Distortion increases as you approach the

    poles

    Conic projections are used for midlatitudezones that have an EW orientation

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    Secant Conic Projections

    More complex conic projections that contact the

    global surface at two locations.

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    Cylindrical Projections

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    Universe Transverse Mercator

    Projection

    Cartesian coordinates

    For each zone, the enclosing cylinder is

    rotated so that a particular centralmeridian (longitude) is touched.

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    Universal Transverse Mercator

    (UTM)

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    Special Case: State Plane Really a meta-projection

    Each state has one or more projections,with one or more zones.

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    Data from maps of varying

    projections can not be integrated

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    Solution: Projection and

    Reprojection

    Projection: Converts from a geographic

    coordinate system to projectedcoordinate system

    Re-projection: Projects from one type of

    projected coordinates to another type


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