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I<br />

I<br />

least altitude.<br />

.— ..— .—. .——_ _<br />

IJPPr MOtb~6WVeYbg) Rotation of the<br />

upper *M 0/ a repasting ~.<br />

war tinah-Tranti d a cdtdd ~ ~w<br />

the ippar brench of ths celrdal meridiin. Also<br />

celled cmtpartor transit. See also<br />

culmination,<br />

uaar httaflaca-Ths method by wlich the<br />

human qaamtcx mmmunidns with the vWiOuS<br />

dste base and appliibrra modules.<br />

user raqulramant ●mlysls (URA)-The<br />

study of the needs C4 ths polerrtisl system<br />

Uaara.<br />

UTO tfme-Tfre mesn universal time ~<br />

frem otmewetii ol Iims ot eisr transils. Sinca<br />

tha directions CAthe maridismr chsnge with tima<br />

b-usa of the motion c4 the pole, the IJTO time<br />

will, thus, be affected and N, thamfora, ba<br />

Irrsgutsr. See also UT1 tlma; UT2 tlma.<br />

UT1 tlms-l%e true angulsr rotation of the<br />

Emth about its instantaneous spin sscis in the<br />

mean ~untorisl 6y61em of dstas. UTl is<br />

cbtsirrsd fmm Lrro by 00r1adii UTo f’w the<br />

dfierence between the instsrrtsrreous and<br />

maen kmgttude e! the obsawing station, Sines<br />

LITI is keyed ~ to the instmda-s<br />

mtden ef the Esrth, wlii is not sttitly uniform,<br />

UTI does not ~- urdicimly. Saa also UTO<br />

time; UT2 tlms.<br />

UT2 tlma-llre mean angulsr motion ot the<br />

Esrth, treed of pmdHtb& periodic vtui.don bul<br />

still affected by bregular vatiatii and aeculsr<br />

varMerra. UT2 la cbtgin.art b UTI ~<br />

cOrmdng u—rlfor Maaaral vartstions in rcddii<br />

rote. Sae elso UTO tlma; UTl tlma;<br />

unlvoraal tlmo coordlrmted.<br />

MIL-HDBK-850<br />

273

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