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,/<br />
I<br />
d-y C’$Ndialdata.<br />
Gsogmphk Nsrw*s Procosslng Syskm<br />
(GNPS)-Ths DMA system which includes the<br />
hardware, cmffwsre srsj eras to nminfain<br />
the geographic nsmee data requirsd for digital<br />
maps ad gsztmeam.<br />
MIL-HDBK-850<br />
gsogm hlc (~oogrephbel)-Signify ing<br />
bade MRfbnehpto the Eartfrcxmddamd asa<br />
gbbe-ahapad body. The term geographic is<br />
applied dike to dsta bad on ths geeid and on<br />
othw spheroids.<br />
geographic coordlnat@a-(JCS) The<br />
qusnfitbe c4 fatituda and Iengituda wlriih ds&ne<br />
the~indapnfonffnswf~ efm.s<br />
Edh with respect to thtr rsferenca spheroid.<br />
Also called astronomic coordlnetes:<br />
gravimetrlc coordlnatea; tormotrial<br />
coordinates. See also coordlnatas;<br />
geodetic coordinates.<br />
geographic lstltude-A general term,<br />
aPPbinjl afike to asfrancsnic 181iidBs ~~<br />
geodetc latitudes.<br />
geographic llmlta-The lines heving Istirude<br />
and Iongkde values bounding the area of a<br />
mm or chart: that eras exclusive of overlao<br />
areas. See siseneatlh-rsis.<br />
geographic location-see geographic<br />
pooltlon.<br />
geographic longltude-A general term,<br />
a@Yin9 afike to astronomk and to geodetic<br />
longitudes<br />
geographic merldlan—A general temf<br />
;~~~~,atike to an as!ronomio or gsodetrc<br />
geogmphlc nama-Aleo called place<br />
name and toponym. sea also Board of<br />
Geographic Names.<br />
geographic nonllnoarlty—The error<br />
introduced by digitization and subsequent<br />
processing 10 Ihe total error of both abdute<br />
ard reletfie positioning of any Ieature on the<br />
gmphk.<br />
geographic perallef-A general term,<br />
applying atike to an eafronomic parallel or e<br />
geodetic parallel .<br />
gaographlc posltlo~Tha position of a point<br />
Ontheaurfea c4the Earfhuupmeed krmrrtw<br />
of latiiuda end bngitude, either geodetic or<br />
astronomic.<br />
gaographlc ●urv*y-A general term. mt<br />
~pfibk & defined Iirritsfion, covering a wide<br />
mWe & Wweye fying between and merging<br />
into axpbmfory wrvaye on the one hand and<br />
bsdc topogmphii eurvays on the cdher.<br />
Gaographk etevays WJ.4y cover kwga areas,<br />
are based on coordinated control, end am uaad<br />
to record ptryskal and statistical ctssmcferfsrks<br />
of the area surveyed.<br />
geographic vertical-See vertical.<br />
googrephlcaf ●ma claaWtcatlon<br />
eyatern-A fogicsl snd orderfy gaographksl<br />
division of the world using nufirs, Iattem! and<br />
ccmbinaticms of the same for the deeignakxr of<br />
areas and subsraas.<br />
goographlcef ●xploretlon trmrome-A<br />
route followed scross some parts of the Earth,<br />
approximate positions ebng whmh are<br />
determined by surveying or nevigslional<br />
methods.<br />
gaographlcel mile-The length of 1 minute<br />
of erc at the Equator, or 6,067.08 feel (on the<br />
Clarke cpheroid of 1666).<br />
gaographbrd pofe-Eiiher of the two points<br />
cd intersection of the sudece of the Earth tih its<br />
axis, where all meridtans meet.<br />
geoidaf contour-A line on the suriace of the<br />
geoid of mnstant elwation with reference to the<br />
surface of the spheroid of reference. Geoidd<br />
contours depend on the surta of reference as<br />
wellaeon lheahapedthegeoid. Theeama<br />
gecid referred to different surfeoes of refemnos<br />
will give different sets of gaoirhl contours.<br />
geoldel holght profile-See<br />
●strogoodetlc Ieveflng.<br />
gooidal height—The distence of the gaoid<br />
above fpodive) er bebw (nagative) the<br />
methemalicsl reference spheroid. Also celled<br />
geold separstlon; undulation of the<br />
geold. See alw sstrogeodetic<br />
undulations.<br />
geoldd horlzors-llat circle of the celestial<br />
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