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porspectlvo chm’t-A chari on a perapacfive<br />
Pr@actiin,<br />
perspective grid-(JCS) A network of firms,<br />
drawn or superimposed on e Photograph. 10<br />
represent the pers+ecfive of a syafernrdic<br />
natwwk d fines on the ground or datum plane.<br />
~~h~~ad Canadian grid. Sea al= grid<br />
parapectlvs map projoctlon-A map<br />
project’km produced ~ efrdght fines radiiting<br />
from a aslacfad point and passing lhreugh<br />
poirrfs on the earth’s surface to the projection<br />
surface. Alee called geomctrlc map<br />
pro)actlon.<br />
parepactlvo plane-Any ptane ccmlaining<br />
the perspective canter. The intersection ef a<br />
perspective pfana and the gmurrd will ahvays<br />
-r as a straight fins on an ae~I<br />
photograph.<br />
MIL-HDBK-850<br />
parspectlva proJactlon-The projection of<br />
points by sfreighl firma drawn through them from<br />
aoma given peint to an intamaction with the<br />
plans et projection, Unless etharw.iea indicaIad,<br />
tha point of pjection is understood 10 be at a<br />
finite distarwe from the plane of projection,<br />
parspectlva ray—A line joining a perspactiva<br />
canter end e peirrt objact. See else Image ray.<br />
perapectlve apatlal modat-Crptical<br />
raconatrucfion of an area of tarmin shcwing<br />
depth by viawing a pair of aarial photographs<br />
through a atersoacapa.<br />
parspactlva view—A three-dimensional<br />
representation generated with a reference to a<br />
app~iawer location on or abeve Ore surface<br />
perspectlva-l%a appearatwe to the eye of<br />
objects in rasped to their relative distance and<br />
pesifion.<br />
perapectlvity—The corraepondence batwaen<br />
the points, lines, or pkwras of two geemelric<br />
configurations in perspective. Usually raf erred to<br />
as linear pe-ivii because the true<br />
parapdive center must be recoverable befora<br />
angular percpedvhy can be included.<br />
perturbation-in celastial mechanics,<br />
dtierencas of the actual orbii from a central<br />
188<br />
fercs odid, arising from some axlar’rd fo=<br />
such es a thkd @ altrac4ing the other two; a<br />
rasisling nrerlum (atmosphere): failure of the<br />
Parerrt bodytoad aaapdrrtmaaa, and so<br />
forth. See alse gravitational pwturbatlons;<br />
long period parkurbatlons; Iunlsolar<br />
porfurbatlone; nongravltatlonal<br />
perturbatlona; perlodlc perturbations;<br />
●ocular perturbatlona; short parlod<br />
perturbations: torrastrisl parturbetiorm.<br />
perturbed orbff-Tfra otbit of a aatelfiie<br />
differing fmm Ms norrnaf orbii due to various<br />
d=turblng affacfa such as nonaymmefrical<br />
gravltstkmal affecls, atmoapherk drag, radiil’on<br />
pressure, acd se forth. Sea alao perturbation.<br />
perfurtrlng factom (forces)-in celestial<br />
mschanii, any force that ads on lha orbi!ing<br />
body to change its ortit from a cen!ral ferce<br />
orbit.<br />
phase age—Saa ago of phase<br />
Inoquallty.<br />
phaao angle-l. Tha phase difference of two<br />
periodically recurring phenomena of the sama<br />
fr~uency, expressed in angular maasura. 2.<br />
The angle at a celestial body between the Sun<br />
and Earth.<br />
phase inequality—Variations in U-m tide or<br />
tidal currents a-iated with changes in the<br />
phase of the Meon. At new and full Mom<br />
(springs) the tide-prcducing forces ef the Sun<br />
and Meon ad in ccmjuncfion, reaulthg in greater<br />
Ihan average tide end tidal currents. At first and<br />
teat quarters of the Moon (naepa) the tideprcducing<br />
fore= cppoaa each other, resufting in<br />
smaller than everaga tide and tidal curranm.<br />
phase-l. (general) Of e petiedic quanlify, for<br />
a ~flicubr Valua of the indapendenf variable,<br />
the fradional part of a period through which the<br />
independent variebfa has advanced, measured<br />
from an arbiinwy reference. 2. (surveying) The<br />
apparent dkplacernanl of en ob)~t or s’wnal<br />
caused by ona aide being rrwre atrengfy<br />
illuminated than the other. The resuftant error in<br />
pointing is aim’iar 10 the armr cauaed by<br />
observing an accantric signaf. 3. (astronomy) A<br />
atege in e cycle of r-rring aspects, =u6A by<br />
a ~~e~tb Varieticm of the illumination of an<br />
object. The Moon passes through ifs phases,<br />
new Meon to full Moon and back to naw Moon,<br />
as its position relative to the Sun and Earth<br />
changes.