the longitude of the horizontal center of a coordinate system (this longitude value is often the longitude origin of the coordinate system); in the case of the transverse Mercator projection, ...
The meridian that passes through the poles and origin of an ellipsoid/sphere representing the earth and is used in calculations of a specific projection.
Central Processing Unit (CPU) ...
Central meridian and lines perpendicular to it
The line of longitude that defines the center and often the x-origin of a projected coordinate system. In planar rectangular coordinate systems of limited extent, such as state plane, grid north coincides with true north at the central meridian.
the central meridian is straight, half as long as the Equator, and a standard line in odd-numbered projections
poles are flat, half as long as the Equator
even-numbered projections are equal-area
odd-numbered projections have equally spaced parallels ...
the central meridian is the meridian where the cylinder touches the sphere
theoretically, the central meridian is the line of zero distortion
by rotating the cylinder around the poles
the central meridian (and area of least distortion) can be moved around the earth ...
Distances are only correct along parallels and central meridian. Shapes become more distorted away from the central meridian and close to the poles. Slaking See wetting and drying.
Select the Projection Lambert_Azimuthal_Equal_Area. Alter the Central Meridian and Latitude of Origin.
It is also necessary to select a datum (Geographic Coordinate System). Click Select and find North America > North American Datum 1927.prj.
Map makers have technical terms to describe the line of latitude or longitude where this imaginary 'piece of paper' touches the Earth. These are:
for a line of latitude - standard parallel
for a line of longitude - central meridian
Azimuthal Projections ...
Other projection mathods are based on more complicated flattenable projection surfaces, and instead of points of tangency, spacial cases of these projections can be made by adjusting their Standard Paraslells or Central Meridians ...
Just as the normal aspect Mercator projection has low distortion of scale near the equator, so does a transverse Mercator projection have low scale distortion near its central meridian. With the UTM system, the earth is divided into 60 zones of longitude, each 6 degrees of longitude wide.
The origin of each UTM zone is the intersection of its central meridian and the equator, and the parameters are applied to this origin to make it convenient to work with making all x and y values positive, or reducing their range.
The UTM easting coordinate (the X coordinate) for a feature is the distance in meters east or west from the central meridian of the UTM zone. The central meridian for UTM zone 10 (with boundaries at 120° west longitude and 126° west longitude) is 123° west longitude.
and is the longitude from the central meridian, and is the latitude.
The Mollweide is a pseudocylindrical projection in which the equator is represented as a straight horizontal line perpendicular to a central meridian one-half its length.
There is a false origin defined at 400,000, -100,000 such that the central meridian is the Zero easting of the National Grid - which is also aligned to the 2 degree West meridian of Longitude. Additionally, the scale along the central meridian is 0.
To eliminate the necessity for using negative numbers to describe a location, the east-west origin is placed 500,000 meters west of the central meridian. This is referred to as the zone's ‘false origin'. The zone doesn't extend all the way to the false origin.
Within each zone the central meridian is given an Easting value of 500,000 metres. The equator is designated as having a Northing value of 0 for northern hemisphere coordinates. Coordinates are recorded relative to the central meridian in metres in a particular zone.
Put another way: UTM projection is used to define horizontal positions world-wide by dividing the surface of the Earth into 6 degree zones, each mapped by the Transverse Mercator projection with a central meridian in the center of the zone.
Enter Central Parallel: 0 if you want the Equator as the central parallel
Enter Central Meridian: 0 if you want the Greenwich meridian as central meridian
Enter Scale Factor at the Central Meridian
Enter plural form of map units: for example, meters ...
Transverse Mercator projections result from projecting the sphere onto a cylinder tangent to a central meridian. Transverse Mercator maps are often used to portray areas with larger north-south than east-west extent.
UTM zones have an origin on the equator at the point where the central meridian of the zone intersects. Coordinates are measured in meters from the false origin followed by the zone number and the hemisphere.
The projection is true to scale along the central meridian and along each parallel. It is neither conformal nor equal-area, and it is only free of distortion along the central meridian. Therefore, it should only be used for regions of predominant north-south extent.
UTM easting coordinates are referenced to the center line of the zone known as the central meridian. The central meridian is assigned an easting value of 500,000 meters East. Since this 500,000m value is arbitrarily assigned, eastings are sometimes referred to as "false eastings" ...
The easting coordinates are measured from an artificial reference line drawn parallel and 500,000 meters to the west of the zone's central meridian. (Thus each central meridian is numbered 500,000.) The third figure shows the ten UTM zones spanning the United States.
Using Spatial Analyst this tile was clipped, warped with an order-three polynomial to approximate an Equidistant Conic projection (Clarke 1866 spheroid, central meridian 71 degrees west, reference latitude 19 degrees north, standard parallels at 21 and 17 degrees north), ...
A coordinate system is usually defined by a map projection, a spheroid of reference, a datum, one or more standard parallels, a central meridian, and possible shifts in the x- and y-directions to locate x,y positions of point, line, and area features.
A class of map projections in which the parallels are represented by a system of non-concentric circular arcs with centers lying on the straight line representing the central meridian (Lee 1944). The term was first applied by Hunt, and later extended by Tissot (1881).
The UTM divides the world into 60 zones of 6 degrees longitude. Each zone extends 3 degrees east and west from its central meridian and are numbered consecutively west to east from the 180-degree meridian. Transverse Mercator projections may then be applied to each zone.
There are two geoprocessing tools available from the Data Driven Pages toolset in the Cartography toolbox to help you populate a spatial reference field: Calculate Central Meridian and Parallels and Calculate UTM Zone.
into an AutoCAD Map 3D drawings Cartesian coordinate system, and accounts for the curvature of the surface of the Earth with a projection. A coordinate system is usually defined by a projection, an ellipsoid definition, a datum definition, one or more standard parallels, and a central meridian.
Eastings are in meters with respect to a central meridian drawn through the center of each grid zone (and given an arbitrary easting of 500,000 meters). In the northern hemisphere, northings are read in meters from the equator (0 meters).
A transverse cylindric projection uses a meridian of longitude as its central meridian. travelling salesman problem p. 203 given a graph connecting a set of nodes, devise a route that visits each node in the graph exactly once and minimizes the total cost accumulated. trend surface p.