Coordinate Reference Systems and Positioning
A Wikibookian believes this page should be split into smaller pages with a narrower subtopic. You can help by splitting this big page into smaller ones. Please make sure to follow the naming policy. Dividing books into smaller sections can provide more focus and allow each one to do one thing well, which benefits everyone. |
A reader requests expansion of this book to include more material. You can help by adding new material (learn how) or ask for assistance in the reading room. |
Introduction
[edit | edit source]This book is intended to develop content for a new chapter on Coordinate Reference Systems and GNSS Surveying for the Spatial Data Infrastructure Cookbook developed through the Global Spatial Data Infrastructure (GSDI) initiative. The purpose of the chapter is to provide high level information for a basic understanding of global coordinate reference systems (e.g., WGS 84, ITRFxx/GRS80) and case studies from different regions and countries of the world about the challenges of tying their datums to global coordinate reference systems. As the final product will be incorporated in a Portable Document Format (PDF) document, it is important that sufficient information be extracted from open sources so that the user does not have to jump from article to article to get high level information about Global Coordinate Reference Systems and Positioning. Content will be condensed into a chapter covering 15-20 pages.
The Wikibooks approach is being used to foster international collaboration and to quickly develop content. Anyone can contribute and change existing content, and one does not need to register. If, however, you want attribution for your contribution, you are encouraged to register. If you decide to contribute, it is recommended that you familiarize yourself with Wiki markup. The Wikibooks approach is not for people who do not want their masterpiece altered!
As of 2005-01-26, our wish list for contributions is as follows:
- Extraction of information from open sources for inclusion in this chapter
- Graphics and figures
- Case studies from various regions and countries of the world for tying into global coordinate reference systems such as WGS 84 and ITRFxx/GRS80
- Anything marked as TBSL (To Be Supplied Later)
Context and rationale
[edit | edit source]Consistent with the SDI Cookbook, this section establishes the background, context, and rationale for the subject suitable as general orientation for all readers, but targeted for managers and end-users.
Geodetic datum
[edit | edit source]Ellipsoid
[edit | edit source]In geodesy, a reference ellipsoid is a mathematically defined surface that approximates the true figure of the Earth or geoid. It is used as the surface on which geodetic network computations are performed and [geographic] point co-ordinates calculated.
Mathematically, the reference ellipsoid is an oblate (flattened) ellipsoid of revolution with two different axes, an equatorial semi-major axis and a polar semi-minor axis . The ellipsoid of revolution is obtained by rotating the ellipse about the semi-minor axis (refer to Reference ellipsoid)
The flattening is defined as
- from Reference ellipsoid
GRS80 was adopted by the International Union of Geodesy and Geophysics (IUGG) at its XVII General Assembly in Canberra, Australia, December 1979.
For GRS80, = 6 378 137 m and = 0.003 352 810 681 18
External links
Geoid
[edit | edit source]A geoid is a close representation of the shape of the Earth. According to C.F. Gauss, it is the "mathematical figure of the Earth", in fact, of the Earth's gravity field. The geoid is that equipotential surface which coincides on average with mean sea level. - adapted from Geoid
The geoid has an irregular surface and unlike the ellipsoid, cannot be expressed by a mathematical formula.
Height
[edit | edit source]In geodesy, height is the distance of a point (usually on the terrain surface, such as a mountain top) vertically above or below a reference surface - adapted from Height
An ellipsoidal height uses the reference ellipsoid as its reference surface. A geodetic height uses the geoid as its reference surface.
Coordinate systems
[edit | edit source]Cartesian coordinate systems
[edit | edit source]Geographic coordinate systems
[edit | edit source]Geographic coordinate systems
Latitude
Longitude
Grid/Image coordinate systems
[edit | edit source]Unrectified image CRS
Georectified image CRS
w:Image georeferencing TransformationImage georeferencing Transformation
Global Coordinate Reference Systems
[edit | edit source]Geocentric XYZ (TBSL)
[edit | edit source]International Terrestrial Reference System(ITRS)
[edit | edit source]International Terrestrial Reference System (ITRS)
International Terrestrial Reference Frame(ITRF)
[edit | edit source]The International Terrestrial Reference Frame - The International Terrestrial Reference Frame (ITRF) is a set of points with their 3-dimensional Cartesian coordinates which realize an ideal reference system, the International Terrestrial Reference System (ITRS)
Epoch (TBSL)
[edit | edit source]World Geodetic System of 1984 (WGS 84)
[edit | edit source]Plate tectonics and positioning
[edit | edit source]Global Navigational Satellite Systems (GNSS)
[edit | edit source]Concepts
[edit | edit source]How positions are determined
[edit | edit source]GNSS determine positions on the earth through trilateration.
Ellipsoidal and geodetic heights
[edit | edit source]Satellite constellations
[edit | edit source]Global Positioning System (GPS)
GLONASS
Galileo positioning system
Organizational issues
[edit | edit source]Consistent with the SDI Cookbook, this section addresses the design architecture of organisations, roles, and software systems that are intended to interact.
This section will provide case studies on how various regions and countries of the world are tying into Global Spatial Reference Systems.
Regional reference frames
[edit | edit source]IAG Subcommission 1.3: Regional Reference Frames
Europe (TBSL)
[edit | edit source]South and Central America (TBSL)
[edit | edit source]North America (TBSL)
[edit | edit source]Africa (TBSL)
[edit | edit source]Asia-Pacific (TBSL)
[edit | edit source]IAG SC1.3e: Regional Reference Frame - Asia-Pacific
Permanent Committee on GIS Infrastructure for Asia and the Pacific (PCGIAP) Working Group 1: Regional Geodesy
Antartica (TBSL)
[edit | edit source]National datums
[edit | edit source]Australia
[edit | edit source]Geocentric Datum of Australia
Reference Frame: ITRF92(International Terrestrial Reference Frame 1992), Epoch 1994.0, Ellipsoid: GRS80
New Zealand
[edit | edit source]New Zealand Geodetic Datum 2000 (NZGD2000)
Reference Frame: ITRF96 (International Terrestrial Reference Frame 1996), Epoch 2000.0, Ellipsoid: GRS80
New Zealand lies along the boundary of the Australian Plate and Pacific Plate and therefore, is a geophysically active area. The effects of slow crustal deformation (plate tectonics) amount to about 5 cm per year. These changes will be managed through the use of a velocity model to generate NZGD2000 coordinates from observations made at times other than the datum reference epoch. This will allow specialised users to generate coordinates for times other than the reference epoch.
United Kingdom
[edit | edit source]OSGB36 (Ordnance Survey Great Britain 1936)
Reference Frame: OSGB36, Ellipsoid: Airy 1830
Other countries (TBSL)
[edit | edit source]Implementation issues (TBSL)
[edit | edit source]Standards and specifications
[edit | edit source]ISO 19111:2003, Geographic information - Spatial Referencing by Coordinates - scope only; ISO standard carries a copyright
ISO 19127, Geographic information - Geodetic Codes and Parameters - scope only; ISO standard carries a copyright
OpenGIS Implementation Specification: Coordinate Transformation Services, Revision 1.00
OGC Abstract Specification: Topic 2 - Spatial Referencing by Coordinates
OGC Web Coordinate Transformation Service (WCTS)
Recommended XML/GML 3.1.1 encoding of common CRS definitions (XML for CRS)
Recommended XML/GML 3.1.1 encoding of image CRS definitions (ImageCRS)