use and value of a geodetic reference system

by Earl F. Epstein

Publisher: University of Maine at Orono, Publisher: Federal Geodetic Control Committee, Publisher: For sale by the National Geodetic Information Center in Orono, Me, Rockville, Md, Rockville, Md

Written in English
Published: Pages: 36 Downloads: 311
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Subjects:

  • Land use -- Planning.,
  • Geodesy -- Cost effectiveness.

Edition Notes

Other articles where Geodetic Reference System is discussed: geoid: Earth dimensions—radius, mass, and density: Geodesy and Geophysics adopted the Geodetic Reference System , defining aequatorial, MG, and J2, o. Minor revisions to the numerical values were made in The revised values are as follows. Describe the coordinate system and its orientation along with its reference ellipsoid. Specify any standards with which this complies. Coordinate System. Reference Ellipsoid • Name • Semi-major axis • Flattening WGS 84 is a right-handed, Earth-fixed orthogonal System and generally conforms to IERS technical note X Y Z. Earth’s. Simplifies entering vertical observation data records into Blue Book format. The program formats the data onto a computer disk which can then be sent to NGS for further processing and incorporation of the data into the National Geodetic Reference System. PROMPTER (Version ). North American Datum (NAD) using the Clarke spheroid NAD using the Geodetic Reference System (GRS) spheroid World Geodetic System (WGS) using the WGS spheroid Newer spheroids are developed from satellite measurements and are more accurate than those developed in the 19th and early 20th centuries.

The geodetic reference system is defined as 'a complete reference system for positioning a point on the earth, including datum, co-ordinate description, co-ordinate system and possibly a projection' (CEN ). Context: Any type of map is based on such a positional reference system: each point on the Earth's surface corresponds to a point. The flattening is a small value, so usually the quantity 1/f is used instead. These are the spheroid parameters for the World Geodetic System of (WGS or WGS84): a = meters b = meters 1/f = The flattening ranges from 0 to 1. A flattening value of 0 means the two axes are equal, resulting in a sphere. Geodetic observations are necessary to characterize highly accurate spatial and temporal changes of the Earth system that relate to sea - level changes. Quantifying the long - term change in sea - level imposes stringent observation requirements that can only be addressed within the context of a stable, global reference system. coordinate values obtained by one geodetic survey method (for example, a classical line-of-sight traverse) with coordinate values obtained by another geodetic survey method (for example, a Global Positioning System geodetic control survey). Application.

Taken together, the geodetic datum (e.g, WGS84), the type of map projection (e.g., Mercator) and the parameters of the projection (e.g., location of the origin) specify a coordinate reference system, or CRS, a complete set of assumptions used to translate the latitude and longitude information into a two dimensional map. An sf object often. Reset Help Geodetic or true Reference meridian selected from a recorded deed by using the value given for one Grid line in the deed. Magnetic: Reference meridians taken from instantaneous position of Earth's pole, which Assumed wanders over time. Astronomic Reference meridian taken from current position of magnetic poles. Epstein, E.F., and T.D. Duchesneau. The Use and Value of a Geodetic Reference sity of Maine at Orono. Google Scholar. The strategy could be useful in the cases of either neglecting or having inconsistencies on height information for one (or both) geodetic system(s). References Ampatzidis, D. (), Study and data processing for the implementation of differential 3-D transformation on the Greek area.

use and value of a geodetic reference system by Earl F. Epstein Download PDF EPUB FB2

Get this from a library. The use and value of a geodetic reference system. [Earl F Epstein; Thomas D Duchesneau; University of Maine at Orono.; United States. Federal Geodetic Control Committee.]. Terrestrial Reference System Horizontal Geodetic Datum Examples of Horizontal Geodetic Datums Problems Geodetic Control in North America (and the U.S.) That is, a frame is the physical realization of the system defined by actual coordinate values of 1 1 2 3.

Terrestrial Reference System Horizontal Geodetic Datum Examples of Horizontal Geodetic Datums Problems Geodetic Control in the U.S. (and North America) International Terrestrial Reference System World Geodetic System of the U.S. Department of Defense Geometric Reference Systems 1 - 1 Jekeli, January Chapter 1 Introduction Geodesy is the science of the measurement and mapping of the Earth’s surface, and being essentially an application of mathematics it makes use of coordinates and associated reference.

A geodetic reference system is made up of two components, (1) the astronomical and geodetic constants and theories used in the establishment of geodetic positions and orientations, and (2) the reference frame in which the positions and orientations are defined. This text covers all aspects of terrestrial and celestial coordinate reference systems and frames in geodesy, from historical geodetic datums to modern (current) national and international reference systems and the transformations between them.

Assembly, has introduced a new Geodetic Reference Systemrecommends that this system be used as an official reference for geodetic work, and encourages computations of the gravity field both on the Earth's surface and in outer space based on this system".

2-!The Equipotential Ellipsoid According to the first resolution, the Geodetic Reference. The definition of the reference system, the realization by a reference frame, and the allocation of the geodetic datum have to be strictly coherent.

In traditional geodetic reference systems used in triangulation and trilateration networks, the datum was given through independent (astronomic) observations in selected fundamental stations, which. It is called the Geodetic Reference System (GRS80).

Its semimajor axis, a, is km long and is probably within a few meters of the earth’s actual equatorial radius. Its flattening, f, is 1/ and likely deviates only slightly from the true value, a considerable improvement over Newton’s calculation of a flattening ratio. Input Formats and Specifications of the National Geodetic Survey Data Base, (three-volume Blue Book set)pp., $ Use and Value of a Geodetic Reference System, by Epstein and Duchesneau,36 pp., $ Multipurpose Land Information Systems: The Guidebook, by Federal Geodetic Control Committee,pp., $ These reference ellipsoids are taken to be concentric with their coordinate system, geocentric or near geocentric, with the axis of revolution coinciding with the z-axis of the coordinate system.

The basic idea behind using the reference ellipsoids is that they fit the real shape of the earth, as described by the geoid (see Section III.B for. International Celestial Reference System (ICRS), in replacement of the FK5 (Fricke et al. The consequences of this new situation for accuracy needs more stringent than " are summarized by Feissel and Mignard ().

By Reference Systemit is meant the set of prescriptions and conventions together with the. The Geodetic Reference System (GRS 80) posited a 6 m semi-major axis and a 1 ⁄ flattening.

This system was adopted at the XVII General Assembly of the International Union of Geodesy and Geophysics (IUGG) in Canberra, Australia, considering that more appropriate values are now available, recommends a) that the Geodetic Reference System be re-placed by a new Geodetic Reference Systemalso based on the theory of the geocentric equipotential el-lipsoid, defined by the following conventional constants: • equatorial radius of the Earth: a = m.

A geodetic datum or reference frame is an abstract coordinate system with a reference surface (such as sea level) that serves to provide known locations to begin surveys and create maps.

Chapter 6. Geodetic Reference Standards Referencing systems (Obj 5 Task 1 - Identify the implement GIS-referencing system) Coordinate systems are the means of referencing geographic information to locations on the earth's surface and are the reference to standard models of the earth's surface represented as an oblate spheroid of revolution (a flattened sphere).

e A geodetic datum or geodetic system (also: geodetic reference datum or geodetic reference system) is a coordinate system, and a set of reference points, used. Geodetic datum (including coordinate datum, height datum, depth datum, gravimetry datum) and geodetic systems (including geodetic coordinate system, plane coordinate system, height system, gravimetry system) are the common foundations for every aspect of geomatics.

This course book. The Global Positioning System uses the World Geodetic System (WGS84) as its reference coordinate system.

It’s made up of a reference ellipsoid, a standard coordinate system, altitude data, and a geoid. Similar to the North American Datum of (NAD83), it uses the Earth’s center mass as the coordinate origin.

Geodetic Coordinate Reference System. The IBM Informix Geodetic DataBlade module's coordinate reference system uses geodetic latitude and longitude to describe locations relative to the Earth.

Geodetic latitude and longitude are always based on a specific datum. The geodetic latitude of a point is the angle between the datum surface normal at. erence system; a vertical network furnishes elevations in the National Geodetic Vertical Datum reference system; and a gravity network supplies gravity values in the U.S.

absolute gravity reference system. A given station may be a control point in one, two, or all three control networks. It is not feasible for all points in the control networks to. The World Geodetic System (WGS) is a standard for use in cartography, geodesy, and satellite navigation including standard includes the definition of the coordinate system's fundamental and derived constants, the ellipsoidal (normal) Earth Gravitational Model (EGM), a description of the associated World Magnetic Model (WMM), and a current list of local datum transformations.

Test Coordinate Systems. This dialog is accessed via the Test button from the Geodetic Configuration Overview Dialog.

It will take the configuration coordinate systems and put them in the Input and Output Coordinate System combo boxes. You then choose which coordinate system you want as your Input and which one you want as your Output. You will then be able to convert from one to the other.

Based on the first satellite geodetic results from early Doppler tracking and data from a few VLBI stations in the s, the NAD83 took the North American reference frame into the space age, making obsolete the older NAD27 system that was based on ground-based classical surveys.

It is essentially the basis for geodetic positioning by the Global Positioning System (GPS) and is thus also in widespread use outside the geodetic community.

The numerous systems that countries have used to create maps and charts are becoming obsolete as countries increasingly move to global, geocentric reference systems using the GRS NAD using the Geodetic Reference System (GRS) spheroid; World Geodetic System (WGS) using the WGS spheroid; Newer spheroids are developed from satellite measurements and are more accurate than those developed in the 19th and early 20th centuries.

You will find that the terms "geographic coordinate system" and "datum" are. The North American Datum of is based on both earth and satellite observations, using the Geodetic Reference System (GRS) spheroid.

The origin for this datum was the earth's center of mass. This affects the surface location of all longitude–latitude values enough to cause locations of previous control points in North America to shift. The National Geodetic Survey (NGS) is mandated by law to establish and maintain a National Geodetic Reference System (NGRS) adequate for present and future public needs.

The present NGRS is a network of close tomonumented control points whose precise geographic positions or elevations. or both, have been determined by geodetic surveys.

The geoid surface is irregular, unlike the reference ellipsoid (which is a mathematical idealized representation of the physical Earth), but is considerably smoother than Earth's physical surface.

Although the physical Earth has excursions of +8, m (Mount Everest) and −11, m (Marianas Trench), the geoid's deviation from an ellipsoid ranges from +85 m (Iceland) to − m (southern. Methods used to connect independent geodetic systems to a single world reference system are discussed, including the role of gravity data.

The edition of this publication contains an expanded discussion of satellite and related technological applications to geodesy and an updated description of the World Geodetic System. World Geodetic System (WGS), and for converting Cartesian and map projection Grid reference system 7 Map projection 7 AX, AY, AZ shift values 28 Accuracy of AX, AY, AZ shift parameters 28 Local datum distortion 29 WGS 72 to WGS 84 transformation 29 Selecting a conversion method Geodetic Tool Kit; Web Services; Process GPS Data (OPUS) Coordinate Conversion and Transformation Tool (NCAT) Vertical Conversions (VDATUM) Download PC Software; GEOID18 Computation; GPS Toolbox; HTDP; VERTCON; Surveys.

Active Geodetic Control (CORS) Adjust Leveling (LOCUS) Survey Mark Datasheets; Process GPS Data (OPUS) Calibration Base Lines.Look at other dictionaries: World Geodetic System — The World Geodetic System defines a reference frame for the earth, for use in geodesy and navigation. The latest revision is WGS 84 dating from (last revised in ), which will be valid up to about Earlier schemes included WGS .