Map Basics, partII GEOG 370 Christine Erlien, Instructor.
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Transcript of Map Basics, partII GEOG 370 Christine Erlien, Instructor.
![Page 1: Map Basics, partII GEOG 370 Christine Erlien, Instructor.](https://reader036.fdocuments.us/reader036/viewer/2022062409/56649f1b5503460f94c300bb/html5/thumbnails/1.jpg)
Map Basics, partII
GEOG 370
Christine Erlien, Instructor
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Previously in Ch. 3 Symbolization Simplification/generalization Classification Scale Reference & Thematic Maps Major Map Elements
Wrapping up with: Projections Grid systems
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Geographic Data
Features must be referenced to some real world location Georeferencing
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Geographic Data & Position
Important elements must agree:– scale
– ellipsoid
– datum
– projection
– coordinate system
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Geographic Data & Position: Scale
When is this is an issue?– When data created for use at a particular
scale are used at another Why is this an issue?
– All features are stored with precise coordinates, regardless of the precision of the original source data
– What does this mean?• Data from a mixture of scales can be displayed
& analyzed in the same GIS project this can lead to erroneous or inaccurate conclusions
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Geographic Data & Position: Scale
Example:– Location of same feature at different scales– (-114.875, 45.675)
(-114.000, 45.000) • Zoomed out look like same point• Zoomed in look like separate points
Take-home message:– Be aware of the scale at which data were
collected metadata– Measurements will only be as good as
least accurate data source
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Geodesy
Study of the Earth’s – Size
– Shape
– Gravitational fields
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Geographic Data & Position: Ellipsoid The earth is not flat
it must be round?! Not perfectly round:
– Small irregularities on the surface such as mountains, basins, etc.
– Distortion due to the Earth’s rotation
– Irregularities due to variations in gravity
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Geographic Data & Position: Ellipsoid The earth’s shape is irregular
– Slightly flattened at the poles– Equator bulges– Southern Hemisphere slightly larger than
Northern Hemisphere
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Geographic Data & Position: Ellipsoid
Ellipsoid: Hypothetical, non-spherical shape of earth– Note: Earth’s ellipsoid is only 1/300 off
from sphere
– Basis for datums • Datum: Reference for elevation on the earth’s
surface
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Reference Ellipsoids
Earth's surface not perfectly symmetrical, so ellipsoid fitting one geographical region may not fit another– Reason for different reference ellipsoids
– Examples:• Clarke 1866: Used for N. America until recently• GRS80: Geodetic Reference System of 1980• WGS84: Developed by US military, refined
version of GRS80
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Ellipsoids & Datums: Importance
Differences exist between different ellipsoids & datums– Coordinates different in each can be
significant distance
– Elevation can be major differences at large scales
Note: Be aware of the ellipsoid & datum for datasets you are working with
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Geographic Data & Position: Projection
Projection: Process by which the round earth is portrayed on a flat map
To project– Think of a light inside the globe, projecting
outlines of continents onto a piece of paper wrapped around globe
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Process of Map Projection
1. Scale change– Actual globe reference globe based on
desired scale (e.g. 1:1,000,000)
2. Reference globe mathematically projected onto flat surface
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Families of Projections
Planar/Azimuthal
Cylindrical
Conical
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Cylindrical projections
http://www.progonos.com/furuti/MapProj/Normal/ProjCyl/projCyl.html
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Cylindrical projections
General properties:– Meridians equally spaced– Spacing between parallels of latitude
increases toward poles– On globe, longitude lines converge at poles
cylindrical projection forces them to be parallel
– The farther away a point is from the tangent line (where cylinder contacts the globe), the greater the distortion
– Useful for sailing (No direction distortion)
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Cylindrical projections: Distortion
http://www.fes.uwaterloo.ca/crs/geog165/cylproj.htm
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Conic Projections
Conic projections are created by setting a cone over a globe and projecting light from the center of the globe onto the cone.
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Conic Projections General properties:
– Contact with globe along either 1 or 2 lines of latitude
– Longitude lines projected onto the conical surface, meeting at its apex
– Latitude lines projected onto the cone as rings
– Distance between longitude lines widens as their distance from the apex increases
– Typically used for mid-latitude zones with an east-to-west orientation
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From Getting Started with Geographic Information Systems, Keith C. Clarke
Conic Projections
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Conic Projections: Distortion
http://www.fes.uwaterloo.ca/crs/geog165/conproj.htm
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Azimuthal/Planar ProjectionsPlanar projections, also called azimuthal projections, project map data onto a flat surface.
When the plane touches the earth at either the north or south poles latitude lines appear as concentric circles and longitude lines radiate from the pole at their true angle like the spokes on a wheel. This particular map projection's light source originates at the center of the earth but this is not true for all planar map projections. (ESRI Press)
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Azimuthal/Planar Projections
General properties:– Tangent to the globe at one point – North & South Poles most common
contact points • Longitude lines converge at the pole • Distance between longitude lines increases as
the distance from the pole increases• Latitude lines appear as a series of concentric
circles.
– Used most often to map polar regions
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Azimuthal/Planar Projections:Distortion
http://www.fes.uwaterloo.ca/crs/geog165/azproj.htm
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Map projections: Distortion
Converting from 3-D globe to flat surface causes distortion
Types of distortion– Shape– Area– Distance– Direction
No projection can preserve all four of these spatial properties
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Map projections: Distortion Shape
– The ability of a map projection to maintain shape of geographic features
– Conformal projections: Map projections that maintain shapes/angles, scale factor locally
• Best used on small areas difficult to maintain true angles for large areas
• Distorts area • Application: Marine or air navigation
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Conformal projections
Example: Mercator
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Map projections: Distortion
Area– The ability of a map projection to maintain
equal area for geographic features (e.g., correct area relative to one another)
– Equal area projections: Map projections that maintain this property • Application: Instruction & small-scale
general reference maps
– No map projection can preserve both conformality and equal area
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Equal area projections
Example: Mollweide
Distortion minimal near the intersection of Equator & central meridian, increases toward the edges of the map
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Map projections: Distortion
Distance– Map projection's ability to maintain true
distance• Maintained for only certain parallels or
meridians OR• Maintained in all directions around 1 or 2 points
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Equidistant projections
http://www.fes.uwaterloo.ca/crs/geog165/cylproj.htm#Equidistant%20Projections
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Map projections: Distortion
Direction– Map projection's ability to maintain true
direction between geographic locations– Azimuthal map projections: Maintain
direction with respect to 1 or 2 points • Angle of a line drawn between any two
locations on the projection gives the correct direction with respect to true north
• Application: Navigation
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Azimuthal projections
Lambert azimuthal
Tangent to North Pole
http://www.warnercnr.colostate.edu/class_info/nr502/lg2/projection_descriptions/lambert_azimuthal.html