1 - NGA
1 - NGA
1 - NGA
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1<br />
MI L-HDBK-850<br />
g80d0dc fine-A tine of SfWfSd d-nctt<br />
bafween my fvm pdnta en any !nafhenmticelFy<br />
dafinad surface. Agaodadclkmfcfan aU@ecid,<br />
in ganerat, h a Ens & rbtble curvature, and<br />
usuauy Iii bafwaan the two ncirmsl sectibn fines<br />
wttikh the two pohte determine. tf the M<br />
t-1 pdnts are in naarfy the wna fslfiude,<br />
the gacdaeb fbta may cross owe of the normal<br />
eactbn lines. n should be nofed that, except<br />
abng lhe Equator and abng the marfdtane, the<br />
gaodesic llnalenot eptanacrsve end cennc4<br />
Lw dghfed over directly. Hewcwer, for<br />
conventkmal trfangulatkm the lengths and<br />
dtiicna of gacdasic lines dtiar kmppreciabty<br />
fmrn cm-responding pek’s d norrnel ~ion lines.<br />
Also called gaodealc; geodetic Ilrm.<br />
geodealc-sae geodesic line.<br />
geodesy—lle science whkh deals with the<br />
fb~inalion d the size and figure of the<br />
Geodotlc Reterenco Systsim 1960 (GRS<br />
BO)-Thta gaodatic reference systam was<br />
ado@d by the XVII General Assembly of the<br />
international Union ef &odesy and Geophysics<br />
at Canberra, Australia in 1979. The GRS SO is<br />
defined by the four fundamental mnetents:<br />
aerni-mejor axis 6,378,137m, gravitatiomd<br />
constent d the Earih (including Ihe atmosphere)<br />
3,9S6.005 x 108 n# S-2, -nd degrae zonal<br />
coaffiiienl 108,263 x l@, and anguler<br />
relational velocii 7,292,115 x 10-11 radkms.<br />
geodotlc ●td geophysical data (G6G)-<br />
Infcrmat”mn or earth data, pertaining to the<br />
sciences of geodesy and geophysics. Typicalfy<br />
includes gravity infomralkm, geodetic peinf<br />
posifiining data, datum definition, etc.<br />
gciodotlc ●nd goophyslcal data<br />
roductlo*The process of enhancing the<br />
value of geodetii and geophysical data by<br />
anefyais, evefuatien, computation, and<br />
adjuatmant. The pmcaea includes (1)<br />
transforming unadjusted survey data and<br />
ebservafiona into an adjuafed form with reliability<br />
afatemanfs; (2) establishing basic frameworks of<br />
horizontal and va.ttiil cantml in advance of<br />
-P. Chad, ad fargat rrwleriels pmducfion, snd<br />
publiihmg d trig Iiita; and (3) arbsfyais,<br />
evaluation, and campufalicn of geodetic and<br />
!W@Yabl data obtained by awface, ahboma,<br />
or tmteffife hschniquee to establish, exiend,<br />
connect, and transform daturns and to relets<br />
datum to the Dapamrranf of Defenea Workt<br />
Geodetic System.<br />
geodetic ●nomaly-Sea ●nomaly,<br />
definiiicn 2.<br />
geodetic ●dronomy-The branch of<br />
gecdesy which Ufifiiee astronomic Obearvsfbns<br />
to asfracf gecdatb Irkmnafiin.<br />
goodetlc aztmuth mark-A rwked potnt<br />
astsbfished in connection with a friengufatbn (or<br />
tmverae) station to provide n starting azimuth for<br />
dependent euwaya.<br />
gaodetic ●zimuth-l%a angle between the<br />
gacdefii meridian turd the tangent to the<br />
geodesic fins at the chsarvar, measured in the<br />
pklne peqmndiculet 10 Ihe allipaoid rrc.rmal of<br />
the observer preferably cJockwiae from north.<br />
Although older suweys, particularly by the Coasl<br />
and Gaodatic Suwey (now National Geodetic<br />
Survey), used sculh, the Daparfment of<br />
Defense now uaas north.<br />
geodatlc control data-information<br />
concerning the pracise horizontal and vertical<br />
geodetic bcetion of pints on the surface d the<br />
Earth end ceiestkl bodies, includ@ points<br />
obtained by phc.!ogmmmetric techniques.<br />
geodatlc control—A system of horizontal<br />
rmdlor vefiicsl mntrol statione that have been<br />
esfeblishad and edjuslad by geodetic meihode<br />
❑nd in which the shape and size of the Earth<br />
(geeid) have baen considered in position<br />
computat”mns.<br />
geodatic coordinator—Tha quantities of<br />
latitude, bngifude, and height (ellipse”@, which<br />
define lhe posifiin of a point en the surface of<br />
tha Earth with respect to tha raferance spheruid.<br />
Also imprecisely called googrttphlc<br />
coordinate.<br />
gaodatlc<br />
card.<br />
geodetic<br />
data sheet—See control data<br />
datum—See datum, definition 2.<br />
gaodatic equatOr-Tha line of zero geodetic<br />
ktifude the uraaf circle described ly tb<br />
semimejor asis d the reference alliisdd ea if ie<br />
roteted about<br />
aatronomlc<br />
the minor asis.<br />
●quator.<br />
See also<br />
103<br />
geodetic he4ght-See ●lllpsoldel holght.