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vacuum box-The frame, wrrfeinirrg ils own<br />

Vssuum unit, Whfch encfmes the rrmkf fer the<br />

fermktg d pfeafii refid maps.<br />

Vaia81a Comp*retor-A precise dbtarrce<br />

measuring Inatrumsrrt thel uses c@icel<br />

imarferometry for making masauremsnfs. h can<br />

reassure distensas ss grast as MM meters with<br />

Ofr===Ydl Wfmlo7.<br />

value-Sas abaoluto VShlO; ●d]usted<br />

valrm; most probablo value: obaanmd<br />

valrm; tru. value.<br />

vanlshlrrg llna-The straight fine on a<br />

photograph t@n which lie 811the vanishing<br />

points of all aystema ot psrellel lines psrallsl to<br />

one plane.<br />

vanlshlng paint-l%e knege, in the pfane of<br />

a ~~~h. of the peint towmd whish a<br />

system of parallel firrEs in ths .3@ect spsce<br />

mnvergas.<br />

varlablo contour interval-A nonuniform<br />

mrrtour intsrvsf. ft msy rssuft tmm the U6S of<br />

cartogrsphk source me!erkrls which do not<br />

so~in a constant sentour interval er from<br />

ade@ng the oortteur interval to specifii types of<br />

Wrmfn for the optimum perfrsyal of diet<br />

fsstures.<br />

varfabfa Iongth field-A field WIWSS length is<br />

determined by the amount ef sforege needed 10<br />

atom ifs contents. Useful for chsresfer strings and<br />

ceotdhs:e atrfnga, both of wh~h are huhty<br />

vsriabfa in length.<br />

variable fanrnh recorde—These remrds may<br />

heve a variabl-e number of fiefds (dele elemantsj<br />

or the fields msy be of varying fsngfh, or both.<br />

Verieble-fmgth mmrde typiilly hsve defimifsd<br />

fiekls atior &yie murrts to fediiate pmcsseing.<br />

Sss also fixed-length records.<br />

varlabfe perspective camera system— A<br />

system whti, in its simpfsst fwrn, mnsisfs of a<br />

rAemJard+pa view camsrs, a Isrge eparture<br />

front-surface mirror of spherical mnfigumfiin.<br />

end en eesal used in tfrs recfifiiticm of highfy<br />

tifted bng focal-length phetegrephs, and the<br />

trsnaformstion of maps and charts fmm one ,<br />

projecflmr to another. When the csmera<br />

MIL-HDBK-850<br />

v<br />

2 74<br />

mnponeM krqkced wifhapm@fOr, if<br />

~ possibk 10 expedite the recfifkationof<br />

Iuner pt@Ogmpfy tekan by terrsetriel<br />

observatori8a.<br />

variable ratio pantograp&S e e<br />

pantograph.<br />

verWrco(u2~Tha most SornmOnly used<br />

measure of d- or error In atstiatkef<br />

ansfyeia. ffieefao oelfsdthe mesnaquered<br />

davietii. Vaderroe is cdctdsrd by ri tddng<br />

fhaeumof thaaqusM davWonshomtha<br />

mean fof each of n cbaervetiens. Then the sum<br />

is dii”tied by n-l.<br />

varlatlorr of coerdlnato rrmthod- A<br />

malhcd et e@a~mg massursrrrants in wtriih the<br />

mordinetas of geodstk points ere varied so as<br />

fo bsst fit the obaarvstiorm snd retain<br />

msthemstlcel Ivwmrgeneity. Sea obaawatlon<br />

equationa; varlatlon of perametera.<br />

variation of latftude-A 6MsII dwmge in the<br />

astronomic isthude of points on the Eerfh, due<br />

to V.srfet)orl d fhe @es.<br />

varletlon of pamrneter-1. An interactive<br />

msthcd to edvii mm@ex equations by<br />

successively cJeam epproxirn=dkms of tha<br />

variables, usuelfy arnpl@ng the more rrignifiint<br />

terms of the rust dsrivatiwes c4 msthemstioelty<br />

prsciss funcfiens thst must equal zero cdy<br />

when the correct vefuas 64 the variables sre<br />

uti to compute the funcliorw. 2. The<br />

okmrvsfksr eqlaMona method of beef squares<br />

adjustment is eemafhnss referred to as the<br />

varfation of parameter mctiod of Iosat<br />

●quaras sdjuatment bmausa the<br />

peremetam of ebservat”km equetlmrs era<br />

determined by varietion of perametem.<br />

varletlon of tha poles-A small variation of<br />

the Imetkrn et the irr.stantanseus exis of rotation<br />

of the Eerth with rseuecf to the ohvsicsl surface<br />

thereof. Also called “polar motion. see elso<br />

conventional Intarnatlonaf origin.<br />

varlstlonal lnaquallty-An Inequality in the<br />

Mean’s rnetien, due msinly to the tangential<br />

m~nent of fhe Sun’s attraction.<br />

varlstIon—See magnatlc varlatlon.

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