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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.

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