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i<br />
Intercardlnal polnl—Any of the four<br />
diractkms midway between the cardinal poims;<br />
norfhaast. soufheasl, southwest, or northwest.<br />
MIL-HDBK-850<br />
Interferometer-An apparatus used to<br />
pmducs and measura interference from hvo or<br />
more coherent wave trains from the same<br />
source. Used to measure wavelengths, to<br />
measure an@sr width of sources, to determine<br />
the angular positkm of sources (as in satellite<br />
tracMng), snd for other purposes. See also<br />
radio Interferometer.<br />
Interim Terrain Data (ITD)-A DMA digital<br />
producf consisting of oomiguous data eels<br />
comprised of attributed and urraymbolizad<br />
feature Information in six thematic files (Surlace<br />
Configuration, Vegetation, Surface Materials,<br />
Surface Drainage, Transportation, and<br />
Obstaclea) and a sevemh file of Digital Terrain<br />
Elevation Data (DTED) Level 1. The data content<br />
is equivalent to the content of either Tactical<br />
Terrain Analysis Data Bases (7TADBe) or<br />
Planning Terrain Analyais Dala Bases (PTADBs).<br />
An enhanced Iranspafat!on file consisting of<br />
attributed roads (afl-waaf her fhrough Carl track),<br />
bridges, and tunnels was added to the data set,<br />
See Plannfng Tarraln Analysls Data<br />
Base; Tactical Terreln Analysls Date<br />
Baae.<br />
Interior angle trrsverse-in surveying, a<br />
closed lravarae wherein distances are maasured<br />
and only Inlerlor angle measurements are used.<br />
Intarlor orlantatlon-The determining<br />
(anafyiicalfy or in a photogrammetric instrument)<br />
of the intarior perspective of the photograph as<br />
it was at the instant of exposure. Elements of<br />
imerbr Orfemation are the calibrated focal<br />
Iangth, bcatbn of the calibrated principal point,<br />
and the calibrated lens distortion. Also called<br />
Inner orlantation.<br />
Intertor perapactlve canter—See<br />
parapectlve center.<br />
Interior to a curtre-That area lying toward<br />
the Conceva sfde of a curva and incfuded within<br />
the area of the circle of which the curve Is a part<br />
of fhe circumterenca.<br />
lnterlocklrtg angle-in till analysis of oblique<br />
photographs, the angle betwesn the optical<br />
axea of Ihe varflcal and oblkfue cameraa. Ttte<br />
dihedral angle betwaan lhe planes of the<br />
vert!cal and oblique photographs.<br />
. .<br />
intermediate contour Urse-A conlour line<br />
drawn bahveen index contours. (@ending on<br />
the wnfour interval, there are thrae or four<br />
imerrndale contours between the irrfex<br />
contours.<br />
Intermediate orbft-A cemnsf force orbft that<br />
Is tangent to the real orbii al some poim. A<br />
fictitious aatellile traveling in the kdermadiefe<br />
orbit would hava the sama position, but not the<br />
same velocity, as tha real salellita af the poim of<br />
tangency.<br />
Internal data structure-The organization<br />
within a ayslem of data and particularly, the<br />
reference linkages among data rslarrwnts. Sae<br />
also Data structure.<br />
International Gravity Standardlzatlon<br />
Net 1971 (IGSN 71)—An adiusted worldwide<br />
network of gravity measurements consisting of<br />
absolula, pendulum, and gravimeter<br />
observations. The IGSN 71 was approved and<br />
adopted by fhe International Union of Geodesy<br />
and Geophysics in 197t, and replaces the<br />
Potsdam datum as fhe international graviiy<br />
standard.<br />
International date llnS-(JCS) The line<br />
coinciding approximately with the amemerfdian<br />
Of Greenwich, modified to avoid certain<br />
habitable land. In crossing fhis line there is a<br />
date change 01 one day. Also called date Ifna.<br />
International eliipaold—A refarence elffpsoid<br />
defined by Hayiord in 1924 with samimajor<br />
axis(a) as 6,378,388.0 reefers, and flattening of<br />
li297.<br />
Internatlonaf gravity formula—A<br />
devalopmem of the formula for theoretical<br />
gravity, based on the aasumptfone thal the<br />
spheroid of raference is an exact ellipsoid of<br />
revolution having the dimensions of the<br />
international ellipsoid of reference (Madrid,<br />
1924), rotating about its minor axia once in a<br />
sidereal day; fhaf the surface of the ellipsoid is a<br />
level surface: and that gravity al the Equator<br />
equals 978.049 gals.<br />
Intarnatlonal low watar (ILW)—A plane of<br />
reference bafow maan sea Iavef; half the range<br />
between mean Iowar low water and mean<br />
higher high water multiplied by 1.5.<br />
Internetfonal ayatam of Unlt9 (Sf)-The<br />
practical international metric system of unlls