Home (Central Meridian)

 GIS 

Home  
 
 
Home » GIS » Central Meridian


 

Central Meridian

GIS  Centerline  Central Processing Unit

Central Meridian
central meridian - [coordinate systems] The line of longitude that defines the center and often the x-origin of a projected coordinate system.



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, ...

Central Meridian
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) ...


A is a meridian that passes through the center of a projection. The is often a straight line that is an axis of symmetry of the projection.
...

Central meridian and lines perpendicular to it
Central Clindrical
Classification: ...

- A line running North and South, at the center of a graticule, along which all points have the same longitude. See also Meridian.
...

central meridian
The line of longitude that defines the center and often the x-origin of a projected coordinate system.

the 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 ...

the central meridian is the meridian where the cylinder touches the sphere
theoretically, the central meridian is the line of zero distortion ...

Distances are only correct along parallels and . Shapes become more distorted away from the 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.

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 - ...

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 .

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 of the UTM zone.

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 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 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'.

Within each zone the is given an Easting value of 500,000 metres. The equator is designated as having a Northing value of 0 for northern hemisphere coordinates.

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 : 0 if you want the Greenwich meridian as
Enter Scale Factor at the ...

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 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.

UTM easting coordinates are referenced to the center line of the zone known as the . The is assigned an easting value of 500,000 meters East.

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.

Using Spatial Analyst this tile was clipped, warped with an order-three polynomial to approximate an Equidistant Conic projection (Clarke 1866 spheroid, 71 degrees west, reference latitude 19 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, ...

[ESRI software] In Survey Analyst for field measurements, any meridian that is parallel to the , used when computing points in planar rectangular coordinate systems of limited extent.

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).

Each zone extends 3 degrees east and west from its 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.

Eastings are in meters with respect to a 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.

See also: See also: Meridian, Map, Projection, Area, Parallel

GIS  Centerline  Central Processing Unit

 
RSS Mobile