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I<br />

trmtcpondor-@CS) A mcafvar.tmmsmtlter<br />

which will ganerafe n rqfy al@nal w pqer<br />

irrlarrogatiorr. Sea aleo rsspcmaor.<br />

transvorsa asla-l%a distanoe between the<br />

apeidas. If IS kfenfkal to the aemfmejor asta for<br />

aflipiiwl orbits.<br />

trmnavuce chart-A chart on a transverse<br />

pmjaction. Also cefkd Invoraa chain<br />

transverse cylindrical orthomorphk<br />

chart (lCOC)-See trarrswrso Mercator<br />

chart.<br />

transwraa cylindrical otihomorphlc map<br />

projoctlon —See trmrsverw Morcstor<br />

map projcctlorr.<br />

transvemo equntor—The plane which is<br />

parpadwbu to Ihe axis of a lraneverprojection.<br />

Aleo called Inverso equator.<br />

transversal graticula+l fiiitiius graticule<br />

baaed ~ a Ifarcwersa Pr+3cfion. See eka<br />

flctltlous gratlcuk.<br />

transveraa iatttudc-4u@ar dkttrmce from a<br />

tranaverae equator. Also called Inveree<br />

Iatltude. Sw Eke fictitious Iatltude.<br />

trmsveras Iongltuda-+ngutar distance<br />

Mvmarr a ptfme tranavarea meridian and any<br />

given transverse maridiin. Also ceiled Invaraa<br />

Iottgttudo. See also fictitious Iongltude.<br />

transvarso map projaotlon-A map<br />

projedkn in whiih the projection axis is rotated<br />

9tP in azimuth.<br />

tranawrse Mercator chart-A cherl on the<br />

transverse Mercator prajactiin. Afao called<br />

Inwrso cvlhrdrlcal orthomor~hk chart:<br />

Inveraa Mercator chart; transverse<br />

cyllndrlcsl orthomorphlc chart.<br />

trsnsvsrse Mercotor grid—An informal<br />

daeignetkn for a stale coordinate system baaed<br />

on a transverse Mercator map projection. Afeo<br />

celled Geusa-Kruger grid.<br />

tranaverso Msrcator map projection—A<br />

conformel cdindrical meD Dmiactiorr. being in<br />

principla aqiwalent to the ‘regular M“ercal~r map<br />

pmjedion Iumad (tranaveread) 90” in ezimulh.<br />

In ths projadon, Ihe central meridiin is<br />

MI L-H DBK-850<br />

. .<br />

265<br />

mpraaantod by a atrelgfd line, ccmwpmdi to<br />

thaline wtJchreprasenk fhe Equafaron the<br />

m@ar Mere.@or ~ pru@dii. NeiUws the<br />

o-c ~ne (Sxcapr the Cantrrd<br />

marsfiin) nor the geodetic pallek (faccept the<br />

Equator) are repmaamted by etm@ht lines. Ak<br />

CJSllad Inwrao cylktdrlcd orthomorphk<br />

msp projoctlon; Inverso Mercator msp<br />

projection; trutevoraa cyllndrlaal<br />

orthomorphlc map proJactlon.<br />

transwraa mwidla+ greet circle<br />

pWp3tiiUkf toe transverse equator. Tfrs<br />

reference tmneversa maridiin in cells! prima<br />

trsnavarca maridkn. Also calkd Invorssr<br />

meridian. Sea afao fictitious meridian.<br />

transverse model datum-See modol<br />

datum. definition 1.<br />

transverse parallel-A side or fine parellai to<br />

a transverse eque!or, connecting ell points al<br />

equal traneveree Iatfiude, Also called (nwrsc<br />

psrallal. See aleo flctltioua psrallal.<br />

tr.wswrsa pcrJAna of the !WO pints 90”<br />

from a transferee equator.<br />

. . .. ... . . . . . .. ,’..-..<br />

transnrerse polycordc map projection-A<br />

pofy=onic map pmjwfion * is turned<br />

(tranevaraad) 90° in azimuth by substffuting for<br />

the &sntral merkftan, e great circle parpandmular<br />

10 the gaographc rnaridiin to provide e control<br />

axis for the pmjectiin, akng whii axis will fIe<br />

the centara ci ths circular arcs ~rsser#ing ffnaa<br />

of tangency of cones with the surface of the<br />

sphere.<br />

transverse posltlon—A CPM camare<br />

instelktkn se poaitiinad that the pkne<br />

containing the arnare axis is pwpandicufar to<br />

the tine d fight.<br />

tranmrer- rhumb llnc-A line making the<br />

same cbliqua angle vkth all ftiis meridians<br />

of a transverse Mercetor projection. Tmnsveraa<br />

parallels and meridians may be Cu’laldamd<br />

special cases of the transverse rtru~ fine. Also<br />

called Inverse rhumb Ilne, See also<br />

fictitious rhumb line.<br />

trrmaveras-in cartography, panaining Io or<br />

maeeurad on a map prqection In wl’iih a<br />

meridien is ueed as e Iictit”kmisequator. Alw<br />

called In versa.<br />

traverae adjustment—See balsnclng ●<br />

survey.

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