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MIL-HDBK-850<br />

notices, chart updale manuals, target material<br />

bulletins, etc.) utilised 10 Imnemit correction data<br />

tiich the user apfiiis 10 an existing MC&G<br />

product.<br />

corracflon overlay—A transparent material<br />

on which edil cmrecfbns are noted. The method<br />

permits an Immediate bcation ot leaturas to be<br />

revised without the necessity o! marldng the<br />

drawing Or MSP.<br />

corractlon-A quantity, equal in absoluta<br />

magnitude but o~stte in sign to the error,<br />

added to a calculated or observed value to<br />

obta”m the true or adjusted value. See also erc<br />

correction; ●rgmentatlon corractlon;<br />

Bouguar corraotlon; clock correction;<br />

Corlolla correcflon; curvatura correction;<br />

dynamic correction,; dynamic<br />

temperature corractlon; eccentric<br />

reduction; E8tv6a csrrrectlon; fletd<br />

correction; free-elr correction; grade<br />

correction; height-of-eye correction;<br />

Index correction; Ionospheric Correction;<br />

Iatltude correction; Iangth correction:<br />

level correction; orrhometrlc correction;<br />

Polerls correction; rod correction; eag<br />

corractlon; aemldlamaler corracllon;<br />

slope correction; eurfaca corrections;<br />

tape corrections; temperet ure<br />

correction; tension correction; terrain<br />

corractlon; tidal correction; tlmlng<br />

correction; trensll micrometer contact<br />

correction; velocity correction.<br />

correlate aquatlon-An equstion derived<br />

horn an observation or rendition equation, using<br />

undetermined multipliers, and expressing the<br />

rendition that the sum 01 the squares ot the<br />

residuals (or oorrecfiins) reeufting trom the<br />

appliition of these muttipliira to the<br />

observation or conditiqn equstions shall be a<br />

minimum See also condlllon equal Ion;<br />

normel equatton.<br />

Correlarlon Tracking and Trlangulatlon<br />

(COTAT)-A trajectory measuring syslem<br />

Cowssd of several antenna base lines, aach<br />

separated by large distances, used to measure<br />

direction cosines to an object. From thesa<br />

measurements its apace position is computed<br />

by triangulation.<br />

correlation-1. (general) The statistical<br />

interdeperrde~e between two quantities (a.g.,<br />

in gsodasy, gravity enomalies are correlated<br />

with olher gravity anomafies, with elevation, with<br />

58<br />

elevation dtierences, and with geology, etc.). 2.<br />

(aurvaying) The removal of discrepancies thal<br />

axiet among survey dala so that all pane are<br />

interrelated without apparent error. Tha terms<br />

coordination @nd corralatlon are usually<br />

apptied to the harmonizing of auweys of<br />

adjacent areas or of dlffarenf surveys over the<br />

same eraa. Two or more such surveys are<br />

coordinated when they are computed on the<br />

same datum; they are correhted when they are<br />

adjusted Iogether.<br />

correspondence-( steraosmpy) The wndition<br />

that exists when mrrespotilng images on<br />

a pair of photographs lie in the same epipolsr<br />

plane: the absence of y-parallax.<br />

correapondlng Imege polnta-The ImaQes<br />

on two or more overlapping photographs ot a<br />

single ob]ect point. Sometimes incorrectly celled<br />

conjugate Image polnta.<br />

corresponding Image rays—Rays catnecting<br />

each 01 a set of corresfmrding Image<br />

points with its patlicuiar perspective cenlar.<br />

corresponding lmagea—A point or fhre in<br />

one system o! points or tines homologous to a<br />

point or line in another system. Sorrwimas<br />

incorrectly called conJugate potnts.<br />

cotldal charr-A chafl of cotidal Iinas that<br />

show approximate locations of high waler at<br />

hourly imervale measured from a reference<br />

merid! an, usually Greenwich.<br />

cotlsfal hour—The average interval expressed<br />

in solar or lunar hours between the Moon’s<br />

passage over the merictiin of Greerrwich and<br />

Ihe Iollowing high waler at a specified place.<br />

cotldal llnS-A line on a chart passing thruugh<br />

all points where high water occurs et tha same<br />

lime. The lines show the lapse of time, usually in<br />

lunar hour intervals, between the Moon’s transit<br />

over a reference meridian (usually Greenwich)<br />

and the occurrence of high water for any point<br />

lying along the line.<br />

counter-etch—To remove, with certain diluted<br />

acids, Impurities from a Iimographk p!ate,<br />

making if receptive to an image.<br />

countarclockwlss angla-A horizontal angle<br />

measured In a countembckwlse direction: used<br />

primarily for the measurement of deflection<br />

engles.

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