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I<br />

meridian through 24 hours; Greenwich hcur<br />

s@e d the VWIMd F@nOX. =W- ~ t“~<br />

units.<br />

Grwenwlch time-llna basal upon the<br />

GM* marktisn as mferenm, as mnfrssed<br />

*thstbaa edWor reMof - meridian.<br />

grid smplltud~rrpfiiude relative to grid<br />

east or wwt. See also smplltudo.<br />

grfd azhntrth-The angle in the plans of<br />

P@tibn rnaaaumd cbdrwbe between a<br />

straight fiie and the central rneridiin of a ptane<br />

mcfingufar coordhale system.<br />

grid fmering-(JCS) searing measured ftom<br />

grid north.<br />

MIL-HDBK-850<br />

grfd computation-The detamrinaticm fmm<br />

a set of fables derived from formulas, of the true<br />

shape and dlmene’brrs of a grid, for the purpose<br />

of constructing such a grfd. The grid is<br />

mstherrmlimlly coordinated with its related map<br />

projacfiom they are usually compulsd<br />

corrW-renfty<br />

grid convergence-(JCS) The horizontal<br />

angle at a place between Irue north and gr”d<br />

ninth. It is pmporliinsl to the longitude<br />

difference between the pfsca and the central<br />

meridiin. See elsa convcrgenca.<br />

grid coordinate system-(JCS) A pfane<br />

rectangular oeordhale system ususlly bessd on,<br />

end rnathematbally adjusted to, a map<br />

prc@fion in order that gwgraphic p.aeifibns<br />

(fatitudes and longitudes) msY be ras~y<br />

tmrraformed into plane coordhslea and the<br />

rnmpUl~fiifrS refafing 10 them may be msde by<br />

the ordmsry mahrts of plane aurvayirrg.<br />

grid coordhratea-(JCS) Coordheles of a<br />

grid mordinste system to wtrich numbers ardor<br />

letters ●m assigned for use in designating e<br />

point on e gr)dded map, photograph, or chart.<br />

Sss also coordlneten.<br />

grid daaIlnatlon-The angular difference in<br />

dirscfion between grid rrorlh end hue north. II is<br />

measured ess or west fmm true north, Also<br />

called declination of grid north;<br />

gls.msnt.<br />

grid dhectlor@-foffxonfsJ dimctkin expreeaed<br />

as angular distance fmm grid north.<br />

112<br />

grid dlstanm-See grid Iarrgfh.<br />

grid equMOr-A fine pwpendhdar 10 a prime<br />

grid fnaridian, et the tiln.<br />

grid lntsrvaf-(JCS) The d~tsiwe represented<br />

be4ween the fines d a grid.<br />

grid Inverse-1’he computatbn d grid length<br />

and gr”idazimuths from grid coodinsks.<br />

grid JunctIona-Those Iirms daikreeting the<br />

jokringoftwoorrn ora@daY*emsmam$Por<br />

chart.<br />

grid Iatltuds-+ngular diatarrce from a grid<br />

equator. Sea else flctftloua Iatltudo.<br />

grid fangth-The dis$rmce between tw pdnts<br />

obtained by amputation from grid oocdrrdee<br />

of the points. It dtiera from the geodetic kengfh<br />

by the amount d a small correction besad on<br />

the acsfe factor for Ihs Iins. Also calfed grid<br />

dlstanca.<br />

grid lln@-CXre of the lines d e grid.<br />

grid longftude-Angular distance bstween e<br />

prime grid meridiin and sny given grid meridiin.<br />

See also ?ictltlous Iongltudo.<br />

grid magnotlc ●ngle-(JCS) Angular<br />

dtiere~e in diracfbn between grid mxfh and<br />

myr9nsfm nofih. It is rmmsured east or wasr fmrn<br />

gnd north. Afao called grlvatlon; grid<br />

varlatlon.<br />

grid merldlatine of the grid fines<br />

aslending in a grid north-south dkcfion. The<br />

reference grid meridiin is called prima grid<br />

marldlan. In polar mgicms the prims grid<br />

msridlan is usually the 180”4” geographic<br />

meriden. See also flctltkmm rn.rldlan.<br />

grid mathod+pktogremmetry) A method of<br />

pbrting ~il from oMque photogmp~ fV<br />

SWdW@sm9 e Wmpact&e C4 e map grid on a<br />

photograph ❑nd Imnsferring the detail by eye,<br />

thst is, by using the corr-ng lines of the<br />

msp grid and itrl pemp=tw e rmi plemment<br />

guides. See elm parspectlvs grid.<br />

grid north-(JCS) The rrorfherfy or zem<br />

direction Indutad by the grid datum of<br />

dirsct.ksrsl reference.

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