Geography 70 Basic Geodesy Map Projections Coordinate Systems Scale Locating Positions on the Earth
Geographic Data Features must be referenced to some real world location Known as georeferencing
Geographic Data & Position GOAL: To assign a location to all features Important elements must agree: – ellipsoid – datum – projection – coordinate system – scale
Position/location To determine position on the Earth, it is necessary to understand how those elements relate to one another Begin with geodesy
What is Geodesy? Geodesy “A branch of applied mathematics which determines by observation and measurement the exact positions of points and the figures and areas of large portions of Earth's surface, the shape and size of the Earth, and the variations of terrestrial gravity."
What is Geodesy? More simply, geodesy is the study of the Earth’s size and shape.
The Earth is Not Flat
Eratosthenes ( B.C.) Measured the height of an obelisk in Alexandria and determined the circumference of the earth. His measurement: 25,000 Miles Modern Measurement: 24,860 Miles
So the Earth is Round, Right?
The Earth is Irregular Not perfectly round due to: – Distortion due to the Earth’s rotation – Small irregularities on the surface such as mountains, basins, etc. – Irregularities due to variations in gravity
The Earth is Irregular Slightly flattened at the poles Equator bulges Southern Hemisphere slightly larger than Northern Hemisphere
The Earth is: A SpheroidAn Ellipsoid A Geoid
The Earth as a Sphere Geographic coordinates (latitude/longitude) used to specify locations. Treating the Earth as a sphere is accurate enough for small maps of large areas of the Earth (i.e. very small scale maps)
The Earth as a Sphere Spheroid model: – short range navigation – global distance approximations The slight flattening at the poles result in a 20 km difference at the poles from the average spherical radius
The Earth as an Ellipsoid Ellipsoid is a flattened sphere Ellipsoid is created by rotating a 2 - dimensional ellipse around an axis.
The Earth as an Ellipsoid Every ellipsoid has a semi-major (a) and semi-minor axis (b) The amount of flattening is defined as a value f, which is calculated using the semi-axes
The Earth as an Ellipsoid a = semi-major axis b= semi-minor axis f = ((a-b)/a) = flattening
The Earth as an Ellipsoid: WGS84 Ellipsoid b a f =
The Earth as an Ellipsoid
Differences in Lat / Long On a spheroid, lines of latitude (parallels) are equal distance apart On an ellipsoid, the distance between parallels slightly increases as latitude increases
The Earth as a Geoid The only thing shaped like the Earth is the Earth Geoid means “Earth Like” Shape is based on gravity field corrected by the centrifugal force of the earth’s rotation.
The Earth as a Geoid Geoid -- The surface on which gravity is the same as its strength at mean sea level Coincides with the surface to which the oceans would conform over the entire earth if it were made only of water.
The Earth as Geoid If the Earth were completely uniform in its geological composition, landforms and density, then the geoid would match the ellipsoid exactly
Interaction SpheroidEllipsoid Geoid
Relationship of Geoid to its reference ellipsoid
Geodetic Datum Datum -- n. (dat - m) \ any numerical or geometric quantity which serves as a reference or base for other quantities e
Geodetic Datum Geodetic datum – The information that ties an ellipsoid model to the geoid model – Horizontal datum (most common used) – Vertical datum
Horizontal Datum Parameters of the ellipsoid – axis length – flattening value Parameters that tie the ellipsoid to the origin point (known place on the Earth) Components
Review Sphere – The simplest 3D model of the earth Ellipsoid – A more accurate model that takes into account some of the Earth’s irregularity Geoid – The most accurate, most complex model of the Earth, taking into account the Earth’s minor variations from an ellipsoid Datum – The information that ties an ellipsoid model to a known place on the Earth
Geodetic Control Networks Geodesists and surveyors create geodetic control networks to precisely link a set of known locations to each other and to the ellipsoid/geoid at a datum origin.
Geodetic Control Networks Surveyors use these known points in the control networks for surveys and mapping. Control Points are referenced to specific datums.
Geodetic Control Network How do surveyors and others know where these points are?
Geodetic Control Network They mark it.
Common Ellipsoids, Datums
Geodetic Datums The purpose of all of this is to end up with a very, very accurate map. Not all maps need this accuracy, but some do.
Geodetic Datums
Review Sphere – The simplest 3D model of the earth Ellipsoid – A more accurate model that takes into account some of the Earth’s irregularity Geoid – The most accurate, most complex model of the Earth, taking into account the Earth’s minor variations from an ellipsoid Datum – The information that ties an ellipsoid model to a known place on the Earth