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I<br />

tfrwerwtlcal gravity; Virtual gmvlty.<br />

gray ecal.-see ●top wodgs.<br />

great clrcl- cimle on the surf~e of the<br />

Eatth, the pt911s of w4tiih ~ throu@r the<br />

canter of fha Earih. Abe cafled orthodmm..<br />

great ●lllptlc ●’s-h arc defined by a pfana<br />

wllkhoontains fhatwJpdnfa and Ihacantsrof<br />

the raferanca spheroid.<br />

graet yem-Tfra parbd of one carrplete Wcle<br />

of the wquinosea around the ecfi@c, about<br />

25,S00 years. Alae called pletonk year.<br />

grwat-clmle bamlng-The inhiif diractbn of<br />

a great cirda through two terrestrial pdnts,<br />

em==~ as angufw di@a* fmm a mfarence<br />

direction. It te usually measured f- w at 1~<br />

reference duactica clockwise to 3S0°.<br />

grewt-olrote chart-A chart on wtriih a greet<br />

circle appasm as a straight Iinw ❑chart on the<br />

gnemonic prqaction.<br />

great-clink dlrectlorr-l+orfzontel direction of<br />

a great circle, expmssad as angular dkiance<br />

kern e raferanca diraclion.<br />

grwat-clrck dlctm’we-lbe length of the<br />

efrortar arc of the great circle pining two points.<br />

It is usualty azpraasad in nautical miias.<br />

gmat-wlrcle line-h land eurveying, the fine<br />

of interaadmn ef the surface of the Earth end<br />

the plane of e graat tircle of the ceiastial<br />

sphere.<br />

great4rcl* routs-(JCS) The mute which<br />

fdbwa the almrtasf arc d a great circle tefwean<br />

two pokrts.<br />

greatest ●longation-The maximum angular<br />

distance cd a bdy ef the sotar syetam hem the<br />

Sun, aB dwerved frem the Earth. The dirsdion<br />

efthebcdy eastorwastd thati Lsuaually<br />

~fiad, as the greatest dongation west.<br />

Gmwrwlch ●pparant time (GA~Local<br />

WPrent time at the Gr~nwictr nraridiin.<br />

Qreenwlch cIvII time (GC~See<br />

Unlvorsal Tlmo.<br />

Grwanwlch hour ●ngle (GHA)-Angular<br />

d~anse west of the Greenwich celestial<br />

MIL-HDBK-850<br />

111<br />

nwridii; the arc d the sa&ralii wyiator,or the<br />

angfa at the oafastii equator, or the angte at<br />

the celaatial pole, between the upper brarwh of<br />

the Greenwich ceieatial mari.iian ●rd the hour<br />

circle d a pebrf on the cdasfid sphere,<br />

rnaaaurad westward from the Greenwich<br />

oafasfid rnarirSan threugh 380°; -I hour angle<br />

at the Greenwich meridian.<br />

Graanwlch lntarvat-An interval baaed on<br />

the )Aoon’s transit of the Graa~ich -ii<br />

msridiin. as diatiiuishd frem a iccal interval<br />

based on the Moon’s transk .4 the local c9taet!!l<br />

rnatidisn.<br />

Graanwlch lunar tkna-Local lunar time at<br />

lha Greenwich rnaridiim the arc of the Aasfii<br />

equator er the angle, at tha cafaatial pole,<br />

between the lower branch of the Gmanwrs+<br />

Cataatial mwkfian and ths hour circle of the<br />

Moon, measured wesfwatd fmrn the kwer<br />

branch of tha Grwwhvich oakr.sti.slmeridian<br />

through 24 hours: Graamvkh hour angia of the<br />

Mom, expressed in time unka, p4ua 12 hours.<br />

Graanwich Mean Time (GMT)-(JCS) Also<br />

called Greenwich civil tlma; z-time: Zulu<br />

timm See ltnlveraal Tlma.<br />

Greenwtch meridian-The meridian through<br />

Greanti, England, ewving as the raferanca<br />

for Greenwich time, in centrast with tit<br />

merkfkrns. It is accepted almos4 untiersaliy as<br />

the prims meridian, or the origin d<br />

measurement of tongituda.<br />

Gmenwlch ●ldereaf data-Tha number of<br />

mean sidereai days thal have ekpaed a the<br />

Greenwich meridian since the beginning of the<br />

sidereal day that was in pmgraas at Greenwich<br />

maan neon on January 1, 4713 B.C. see also<br />

Gmanwich aldoreal day number.<br />

Gmonwich ●lderoal day number—The<br />

integral pert of the Greenwich sidereal date. It is<br />

e mearm d nurrbrirrg umsacuttidy ●uxaaaive<br />

akfereal daya beginning at the instrmts d qpr<br />

transit of the mean vernal equinox over the<br />

Greenwich nreridiin. See atao Groonwlch<br />

oldamal date.<br />

Gmwrwich sidamef tlmo (GST)-Local<br />

sidereal time at the Greenw~h meridian. Tfw am<br />

sf the celestial aquamr, or ths angie al the<br />

#astial pole, between the tqpar bmndt d the<br />

3raenwich cafeatial rneridiin end the hour side<br />

>f the varnal equinox, measured westward from<br />

ha upper trranch of the Greenwich cabstial

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