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Ilthograpfrlc copy—A graphic reproduced<br />
by the lithographic precess. Also called<br />
Iltho COpy.<br />
Ilthographlc drafting—See Iuschlng.<br />
lithography—A planographlc method of<br />
printing based on the chemical repulsion<br />
between grease and waler to separate the<br />
printing from rronprinting areas. See also<br />
offset Illhogrephy;<br />
photolithography.<br />
lithosphere-The solid part of lhe Earth or<br />
other spSflal body. Distinguished from the<br />
efmosphera and the hydrosphere.<br />
local adjustment—See station<br />
ad]uatmen!.<br />
local apparent tlma—The apparant solar<br />
time for fhe meridian of the observer.<br />
local sefronomlc tlma—Mean time<br />
reckoned from the upper branch of the<br />
bcal maridian.<br />
Iocel attraction—See local magnetic<br />
anomaly.<br />
Iocsl chart-A large-scale aeronautical charf’<br />
designed tor contact fiighl in a congested<br />
area.<br />
local clvll time—See local mean time.<br />
local coordinate system—A right-handed<br />
rectangular coordinate system of which the<br />
z-esis coincides with the plumb fine through<br />
the origin<br />
local datum—The point of reference of lhe<br />
oeodetic control used exclusively in a small<br />
iirea. Usually iden(ifiad by a pro-per name.<br />
local horlzcm—See epparenl horizon.<br />
local trour angle-Anguler distance wesl 01<br />
the bcal celestial meridian; the arc of Ihe<br />
celestial equator, or the angla at the<br />
celestial POle, belween the upper branch 01<br />
the local celestial meridian and Ihe hour<br />
circle of a point on the celeslial sphere,<br />
measured westward from Ihe local celestial<br />
meridian through 360”.<br />
MIL-HDBK-850<br />
145<br />
local lunar time-The arc oj the celeslla)<br />
squalor, or the angla at Ihe celasiial pie,<br />
between the bwer branch of the kx.al<br />
calestial meridian and lhe hour clrcfe of the<br />
Moon, measured westward from the lower<br />
branch of the bcal csfestlal mertcfian<br />
through 24 hours; focal hour arrgla 0! the<br />
Moon, exprasaad in lime unffs, PIUS 12<br />
hours. See also Greenwich lunar time.<br />
IOIX31 magnatlc anomaly-Abnormal or<br />
irregular variation of the Earth’a rnegnafii<br />
field extemfing over a ralalivaly small araa,<br />
due to local magnetk inlluencas. Also<br />
called anomaloua megnetlc varlatlon;<br />
local attraction; local magnatlc<br />
disturbance; magnetic anomaly.<br />
local mean time-l. (JCS) The time<br />
interval elapsed since tha mean WI%<br />
transit of the observets amemaridian. 2.<br />
The arc of the celestial equator, or the<br />
angle at the celestial pole, between the<br />
lower branch of the local celestial meridian<br />
and fhe hour circle of the mean sun,<br />
maasured westward from the lower branch<br />
of the bcal celestial meridian through 24<br />
hours: local hour angle of fhe mean sun,<br />
expressed in time units, plus 12 hours.<br />
Called local cIvII tlmo in United stales<br />
terminology irom 1925 through 1952. See<br />
also local aawonomlc time:<br />
Universal Time.<br />
local merldlan-The meridian through any<br />
particular place or observer, serving as the<br />
reference for local time. Also called<br />
reference meridian.<br />
Iocel eldereal time-The local hour arwle<br />
of the vernal equinox, expressed in time<br />
units. Locel stiareaf lime at the Greerrwich<br />
maridlan is called Greenwich aldereal<br />
time.<br />
local tlma-1. Time based upon the local<br />
meridian as reference, as contrasted with<br />
that based upon a time zona mesidlan, or<br />
the meridian of Greenwich. 2. Any time<br />
kept locally.<br />
local vertbal—The direction of the<br />
acceleration of gravity, aa opposed to tha<br />
normal 10 a reference eurlace.<br />
Iocatlon survey-The establishment on the<br />
ground of points and fines in positions