30.12.2012 Views

1 - NGA

1 - NGA

1 - NGA

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

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“

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!