Basic Geodesy (Cartographic Fundamentals) Flashcards
Geodesy
Science of Earth measurement
Pythagoras (6th Century B.C.)
Humans live on a perfect sphere
Aristotle (4th Century B.C.)
Sailing ships disappeared hull first and mast last..
Late 1600’s
Conclusion : the Earth is not a perfect sphere, but rather a prolate spheroid
Issac Newton (1687)
Oblate spheroid
The Graticule (Geographic Grid)
Combination of latitude and longitude
Lines of Latitude (parallels)
Run east to west but are labeled north or south of the Equator
Lines of Longitude(Meridians)
Run North to South but are labeled east or west of the prime meridian
Reference Ellipsoid
a mathematically defined surface that approximates the geoid
Worldwide used Ellipsoids
Geodetic reference System (GRS)1980
World Geodetic System 1984 (WGS84)
Geoid model
Most precise shape of Earth, approximates mean sea level, is the shape that the surface of the oceans would take under the influence of Earth gravitation and rotation alone(no current, wind, tides, waves)
Datums
Defines the size and shape of the Earth(reference ellipsoid) and some tie point that fixes the ellipsoid on the surface of Earth or the the center of Earth
(A datum also describe the origin and orientation of the coordinate system used)
Horizontal datum
Specifies locations in terms of geodetic latitude and longitude computed from a reference ellipsoid
Vertical Datum
determines elevation regarding the mean sea level>relates to the geoid
NAD
North American Datum