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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.