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vcrlical ●xaggoratlon-1. The change in a<br />
rrrcdel aurfeca Crelted by pqerthafly raising<br />
lhe~rarrr heighrof alfpoitissbeve the b9sa<br />
~.<br />
level tie mkdning<br />
Urcmea90ftha<br />
the same base scale.<br />
vartksl scafernferthe<br />
2.<br />
herizontd<br />
retiaf map.<br />
scale ef ● Iermrn model or plssfii<br />
vortlcal ●xtenslo~ ●xtenslon,<br />
defsitii 2.<br />
vortlcal geodotlc drrtu~ee vwtkd<br />
control datum.<br />
VWUCSI lntonslty-The magnatk intens”~ of<br />
the vertical ~rrent of the Earth’s msgnetic<br />
field. rtrckened positive if dewnwsrd, negative it<br />
upward,<br />
vertical parallax—see y-parallax.<br />
vertical pass point-ses supplemental<br />
olevatlon.<br />
vertical photogmph—An eerisl photograph<br />
takerr with the axis of the earners being<br />
tintsined as okxdy as possible 10 a truly<br />
vertical posbion with the rssuftsnt photograph<br />
laying a~roxirrralefy in a horizerrtal plane.<br />
vertical ptana-1. Any plane psssing<br />
Ihmugh a point on the Earth end containing the<br />
zerdth and mdir of thst pdnt; else a plsne<br />
containing a plumb line. 2 (surveying) A plsne<br />
at right angles to a horizontal pfsne and within<br />
whkh angtes and dMmcee are observed.<br />
vertical sketchmeatar-A type of<br />
sketchrnaater in tilch verfiosl phoregmphs are<br />
Ufifiied.<br />
vortlcal etoreotriangulatlO*That perlien<br />
I OfStWSOtriSr@Morl &ncemed with lb<br />
eatabfiimanf of vedikot data. Varkal<br />
stersotriangulation is etten Iirnfted er prscluded<br />
aa an cparatkrn due to the more rigid scarmcy<br />
starxtards established for vertical pesitiens thsn<br />
for fwfzorrtal pcMorrs.<br />
vertical-anglo bench mark (VABM)—A<br />
bench mark with ef.evalion estsbliihed by<br />
vertksl angle me!hak. See alse bench mark.<br />
varllcel-anglfr station—See<br />
aupplamantal etation.<br />
MIL-HDBK-850<br />
Z77<br />
vOrtlc~f-The fine perparxliidsr to the gsoid at<br />
~Y~*.tktid~rn~ UWfCSCeaf<br />
grawry sch. sea UJsobed Vartkal; mass<br />
●ttmctfon vortkal: normal, rlefinltion 3.<br />
vfbmtiOrr-4 eingfa rnovemanf of a pendulum<br />
irrahher dbctbn,toorfro.sea Stso<br />
osclllstlon.<br />
Wdeo Point Posltionlng Data Baa.<br />
(VPPDB)-A DMA analofj VkfeO dac prodrrd<br />
rhii pmvkiaa ● mmmrxpk precise positiiing<br />
ca@@yniriihi amoreversattia rrdeaeLarfe<br />
uaa fhn the Anstyiiil Photogramotrk<br />
Peaitiing System (APPS). VPPOB was a<br />
WmOMl COIWJfw to Mow reel time aordinate<br />
rasdouK designed for ease of use arxl m“nirnsl<br />
Imining time.<br />
video disc [MCGTJ-A 30.5 cm (12”)<br />
Cmstont Angrisr VaJcdy (CAV) ansbg video<br />
discca#rle ofstorir# video imeges ones~<br />
aide (equkwlerd 10 spproxirdely 200 everag-<br />
Si2ed map chests at m dflemrrr kids of view).<br />
See also CD-ROM.<br />
vldao rrrop-hy one of a - of<br />
cartogrsphk preduds thst are *umd, stored,<br />
m-d d~yed using anslog video signals.<br />
vlewfltrder-(aerial camera) An atmiliiry devica<br />
which show the fiikt d view of a camera. tt is<br />
used in the takingd VOrticsl.9arkIpfrotqephy<br />
to con-act cmb angle and rrmintnin fonvmd Isp<br />
(end Iep).<br />
vlgnatthrg-t. (photogmphy) A gradual<br />
reductiorr hdenaity ofpafla ofephetegmphii<br />
image due to the stopping of some of the mys<br />
errtering the lens. Thus, a kms nmurrting rrmy<br />
Inlerfam with the sxtrems oblii mys. An<br />
ant”~netting fitter is one thst gmdrmlty<br />
decmsses in density frerrr the cs’ttw teward the<br />
adge$ it la used with msny wide-angle lenses to<br />
procfuce a photograph of uniform den.shy by<br />
cuiting down the overexposure d the center of<br />
the photograph. 2. (fiihography) A photographic<br />
IXOCeSS wfriih portrays a soiii cmlor in a soreen<br />
vdkh shsdes oft gredudiy inlo Ihe unprinted<br />
paper. @xr water is often ahown by this<br />
methed.<br />
vlrtuel gravity-The forca of gravity on an<br />
etmmspheric parcel, reduced by cerrtrrfugat hrce<br />
due to rhe rrmtk.n of the parcel ralalive to the<br />
Earth.