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MIL-HDBK-850<br />
vertical angle, if meaeurest to the right timb in<br />
lhe a.m., then the angle should be measured to<br />
Ihe feti limb in the p.m. The same limb shoutd<br />
be observed In vertical angle. The mean of the<br />
two horizontal angles, with smell correction for<br />
the change in the Sun’s declination during the<br />
Interval from the a.m. 10 Ihe p.m. readings,<br />
@res a reeutling horizontal angle 10 the<br />
meridian.<br />
equal-eltltude obaervatlona—<br />
Observatbns of celestial objects al a fixed<br />
altitude (such as by an aatrolabe) taken at more<br />
or teas uniformly spaced azimuths around the<br />
horizon<br />
equal-araa map projactlon—A map<br />
prmjectbn havin~ a mnstant area scale. Such a<br />
projection is not mntorrnal and is not used for<br />
navlgarlon. Also called aUthallC map<br />
projection; equivalent map projection.<br />
eqIJ8t10n of tha equinox—The difference<br />
behveen the mean and true right ascensions of<br />
a body on the Equator, thus the difference<br />
between mean and apparent sidereal time. Also<br />
called ntnatlon In tight aacenslon.<br />
equallon of tlma-The algebraic dillerence<br />
in hour angle between apparent solar time and<br />
mean solar time, usually labeled “+. or .-. as h is<br />
to be applied to mean solar time to obtain<br />
apparent solar time.<br />
equation—Seis angle equation; azimuth<br />
equetlon; condition ●quation; correlate<br />
equallon; error equation; Euler”a<br />
equation; hydr08tatlC equation; Laplace<br />
equation; latllude equation; length<br />
equation; Iongltude equation: lunar<br />
equation; normal equation; obaewatlon<br />
●qustlon; parametric equationa;<br />
perpendicular equation; personal<br />
equation; elde equation; elde equation<br />
teata.<br />
equator ayatem—See celestial equator<br />
eyatem ot coordinates.<br />
equatorial axl-1. The diameter of the<br />
Earth described between two points on the<br />
Equator. 2. (astronomy) A telaacopa mounting<br />
axis oriented parallel to the Earth’s rotational<br />
axki.<br />
equatorial bulge-The excess of the Earth’e<br />
equatorial dtameter over the polar chameter.<br />
85<br />
equatorial chart-1. A chart of aquatotial<br />
areas. 2. A chatl on an equatorial pmjeCS~n.<br />
equatorial cylindrical orthomorphlc<br />
chart—Sac Mercator chart.<br />
equatorial cylindrical orlhomorphlc map<br />
projection—Sae Marcator map<br />
projection.<br />
equatorial diameter—Tha diameter of the<br />
Earth at the great circle comprising the laweatrial<br />
equator.<br />
equatorial grevlly value-The mean<br />
acceleration of gravity al the Equator,<br />
approximately equal to 9.7803 rrVae~.<br />
equetorlel horizontal parallax—The angle<br />
at a celestial object subtended by the equatorial<br />
semldiameter of the Earih used to indicate tha<br />
distance of the object from the Earth.<br />
equatorial lntewala—The englea, expreseed<br />
in units of time, between the varbua lines which<br />
mmpose the raticle of an astronomic transit and<br />
the maan pesition 01 .Ihose Iinaa.<br />
equatorial map projection—A map<br />
projection canterad on the Equator.<br />
equatorial node—Elrher of the two poims<br />
whera Iha orbit o? the satellite Imer’eects Ihe<br />
equatorial plana of its primary.<br />
equatorial redlua-The radius aesignad to<br />
the great circle mmprlsing lhe terrestrial<br />
equator.<br />
equatorial aatelllta-A satellite whose otbit<br />
plana coincides, or almost coincides, wfth the<br />
Earth’s equatorial plane.<br />
equatorial etara-Stars having declinations<br />
closa 10 zero and whose diurnal path k a<br />
parallel of declination cbsa to the Equator.<br />
Equalorlat stare, because o~ thalr apparently<br />
graatar speed of lravel, are preferred for tima<br />
and bngitude determinations.<br />
equatorial ayatem-See celeatlal equator<br />
ayetem of coordlnataa.<br />
Equator—The great circle on !he Earth midway<br />
belwean the poles and in a plane perpendicular<br />
to the Earth’s azia of rotation. II is the line of O“