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i<br />

MIL-HDBK-850<br />

sphorfcal ●xcosa-l%e amount by which the<br />

sum of the three arrgfes of a triangle on a<br />

sphere axoeade 180”. In gaodatk work, in the<br />

co~yfafbn of trisngbs, the difference between<br />

s@r3rrd angfas and sphamidal angles is<br />

generally nagfecfsd: Sph- angles are used,<br />

and Lagarrdm’s thsorem ki applii to the<br />

dsribution of the spherical excess. That is,<br />

a~roximatefy ona-thd of the @mrical axcaaa<br />

of a given spherical triangle is subtracted from<br />

each angle of the triangle.<br />

spharlcal hsrrnonks-Trigonometric terms<br />

of an infhife .saries used to approximate a W*<br />

or thraedkrransiortd furrcfbrr of ~t~ns w or<br />

abeve the Earlh.<br />

spherkal Ion- lens in whmh .s11euriacas<br />

are segments of spheres.<br />

spherical trlangk-The cbsed figure formed<br />

when any three points on the surfece of e<br />

s+rhare am ~kred by ems of great circles.<br />

ctpherold junctlorr-An eccentuatsd line on e<br />

VP or chart, separating Wo or more major<br />

,.- grids which ere. based on d~eran! spheroids,<br />

spheroid of referonc~See refarence<br />

spheroid.<br />

spheroidal angle-An angle between two<br />

curves on e spheroid; meesured by the angle<br />

between their tangents at the point of<br />

intereeXiin.<br />

spheroidal axcess—Tha amount by which<br />

the sun of the three engbs of a O’iangle on a<br />

spherokf exceeds 180”. see also spherical<br />

excess.<br />

spheroldsf trlangl*A triangle on tha<br />

surlece of e sphamid.<br />

rtphorold-1. (genetal) Any figure differing<br />

slightly from a sphere. 2, (geodesy) A<br />

mathematical figure cbsaly approaching the<br />

geoid in form and size end used as a surface of<br />

reference for geodetic surveys. In geodesy<br />

spheroid and elf!!sokf are synonymous terms.<br />

See ebu Afry ●pherold (afllpaold);<br />

Australian Nstlonal apherold; Eaasel<br />

sphorold (slllpsofd); Clarko spheroid<br />

(olllpsold) of 1868; Cfarko cphorold<br />

(olllpsold) of 16S0; ●flipsofd of rotetlon:<br />

equilibrium ●pherofd; Everest spheroid<br />

(ellipsoid); Hayford sphorold (ellipsoid);<br />

za8<br />

Intorrmtlorml ●phoroid (alllpsold);<br />

Kraaovaky sphtsrold (alllpaold); oblato<br />

●pherold: prolsto ●pharold; roferanco<br />

●pharold.<br />

●phoropotm!tlal surtaca-See apharop.<br />

●pharop-An aqu”~tential surface in the<br />

normal gravily field of lhe Earlh. Also celled<br />

●phoropotmtlal ●urtaca.<br />

spldor tempfet—A mechanical templet which<br />

is fwmed by afteching skoftad steal arms,<br />

representing radiifs, to a central sore. The<br />

spider tenqdet san be d~ernblad ard the<br />

parts used agein. Also called mechanical arm<br />

templet.<br />

spider-tomplmt p}ot-See spldcr-tomplot<br />

triangulation.<br />

spldar-tamplet trienguletlon—A grephicsl<br />

rad!al triangulation made by the uss of spider<br />

Iempbts. Also called spider-tempfet plot.<br />

spiral curve-(mufe surveying) A cutve of<br />

uniformly vsrying radius mnnacfing a circuler<br />

curve and e tangent, or two circular curves<br />

whose rsdii sm. rqtiivaty, bngar and ahorler<br />

than its own extreme radii. Afso called<br />

easamont curve; tranaltlon curve,<br />

spiral to spiral (SS)-A common point<br />

between two spirals.<br />

splrlt Iavel axis—The fine tangent to the<br />

surfece of a spiril Ieval tube (vial) egainsf which<br />

the bubble forms, at the center of the gmduetad<br />

scale of the level, and in the plane of the<br />

bngiwdinsl axis of the tube (vie!) and its center<br />

of curvature. Also called axis of lava~ axle<br />

of Iho level bubble; bubble ●xk.<br />

splrft Ieval wind-Lack of parallelism<br />

between the axis of a spirit Iavel vial and the fine<br />

joining the centets of its suppals. When wind<br />

(pronounced to rhyme with find) is prasant, the<br />

bubble will respoti with a bngitudinal<br />

movemenl Wren the spirit level is rocked on ifs<br />

Suppotis.<br />

nplrlt bvallng—The determination of<br />

Islevetions<br />

of points wfih respect to each otfwr or<br />

\ with respect to e cumrnorr datum, by use of a<br />

Ileveling<br />

rod end en instrument using a spiril<br />

level to esteblish e horizontal fine et sight.

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