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I<br />

. . ...4..,. . M!L.HDBK.S50<br />

glvlng the posltbn of the origin (two elements),<br />

the otiw’rtalbn of the network (one element),<br />

and the parameters of a reference elllpsokf (two<br />

efamants). More racenf definitions express lfre<br />

position and orientation as Iunclbtts of the<br />

deviations In the matian and in the prima<br />

vertical, the gaoid-ellipedd separafiin, ane the<br />

parameters of a refererwe ellipsoid. The Wortd<br />

Gaodatk System (WGS) is a gsocarrtrfc system<br />

that provides a bask reference trarne and<br />

(faomatrk figure for the earth, models the earlh<br />

grevlmatrically, and provides the means for<br />

ratallrtg positions on varioue datums to en earth.<br />

cantered, earth fkad coordinate system. Atso<br />

called horizontal detum; horizontal<br />

gaodetlc datum. See also horizontal<br />

control datum. 3. (leveling) A fevaf surface to<br />

wtrich efavatfons are referred, usually, mean sea<br />

level Imt may also include mean low water,<br />

mean bwer bcw waler, or an arbttra~ etarffrrg<br />

elevation(s). Also called vertlcel datum. See<br />

also allltude datum; Cape Canaverel<br />

datum; Department O! Da fenee World<br />

Geodetic Syetem; Europeen datum;<br />

hydrographlc datum; Indfan datum;<br />

Internatfonaf low water; local datum; low<br />

water datum; low water epringa datum;<br />

lower low watar dstum; Mercury datum;<br />

model drmrm; National Geodetic<br />

Vertical datum of 1929; North American<br />

datum o! 1927; North American detum<br />

of 1983; pfrotographlc datum; prefarred<br />

datum; Pulkovo 1932 datum; reference<br />

datum; eoundlng detum; tidal datum;<br />

Tokyo datum; vertical control datum:<br />

World Geodetic Syetem.<br />

day—The duratioir of one rotation of the Esrth,<br />

or occasionally another celestial body, on its<br />

axis. It is measured by successive transits of a<br />

reference point on the celestial sphere over the<br />

meridan, and esch type takes its name trom<br />

the reference used. See also apparent eoler<br />

dey; eetronomlc dey; calendar day; clvlf<br />

day; constituent day; Julian day; lunar<br />

day: mean eolar day; modiflad Julian<br />

day; Sidereal day; aotar day.<br />

de-integration—Definition of feafure or<br />

tfremafic singles or sets from an Infegraled data<br />

base.<br />

deadbeat compaas—See eperlodlc<br />

cortlpaee.<br />

OECCa chaI1-A cffan showing Oecca IInes of<br />

position.<br />

Decca-A trade name for a radio phase<br />

comparison ayatem which uses master and<br />

slave stations to establish a hyperbolic fettice<br />

arxt provide auxmte position fixing facifiilee.<br />

December ●aletlce-see wlnlar aolstlce.<br />

declination dlfferencs-The difference<br />

between two dactinatione, patikufariy between<br />

the declination of a cdestial body and the value<br />

used ae an argument for entering a table.<br />

decfinaflon of grid notih-see. grid<br />

declination.<br />

declfnaf Ion of the Moon-See lunar<br />

declination.<br />

declination of the Sun-See eolar<br />

declination.<br />

declination—1. In a syetem of polar or<br />

spherical coordinates, the angle at the origin<br />

between a iine to a point and the equafortal<br />

plane, meesured in a plane perpendicular to the<br />

equatorial plane. 2. me arc between the<br />

Equator and the point measured on a great<br />

citie parpendicuiar 10 the Equator. 3. (JCS)<br />

(astronomy) The snguiar distance to e body on<br />

the celestial sphere measured north or south<br />

through 90” from the ceiestial equstor along Ihe<br />

hour circle of the body. Comparable to latitude<br />

on the terrestrial sphere. 4. Dtten used as a<br />

shortened term for magnetic dacllnatlon<br />

although this uee is not prefemd. sea also grid<br />

decllnatlon; Orid magnetfc angle; lunar<br />

decfinatlon; parailei of decflnetion: solar<br />

cfeclinaflon.<br />

decllnatoire—A combined magnetic compass<br />

arvd afraighl-edge, suiiabla for use on a<br />

plantable 10 martr the magnetic merfdian. Also<br />

called box compase; trough compaas.<br />

decllnometer-A magnetic instrument similar<br />

to a surveyors compass, but arranged so that<br />

the line of sight can be rotated to conform with<br />

fhe needle or to any dasfred setting on the<br />

horizontal circle. Used in determining the<br />

magnetic declination.<br />

decompraaa-The process by which<br />

compressed dats is expanded to Its former file<br />

size.<br />

65<br />

defltrltlon-in imaoery Irrterpretetion, the<br />

. —

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