1 - NGA
1 - NGA
1 - NGA
You also want an ePaper? Increase the reach of your titles
YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.
I<br />
I<br />
I<br />
I<br />
i,<br />
I<br />
I<br />
I<br />
1<br />
and with dl tfVSS SXES tfii in a pk’t13<br />
perPczMkufar 10 the fins d ffiiht. Most SSM<br />
esssMea dthkdas@n wemmfan’ad tOSS<br />
trlmatrogorr camera because of the<br />
wideepreed uaega of the MatrogIxI lens in earfy<br />
trlcamara photography.<br />
Mmotrogon photo mphy-Saa fan<br />
1<br />
camsm photogmp y.<br />
trlmmlng and rnountlrrg dlagrmrt-A<br />
&eroh * how the prints of a tmnsfermad<br />
muft!!ldans @mtogmph should be corrected to<br />
oMaino h effect, a phdegm@r rrbsda bys airt@e<br />
Iana. lhekhrrn=fionieghfaintitirnr of<br />
d-m mfermd to tha fduckd rnadta on the<br />
photograph, end k the mauk of the salibretkn<br />
test fer ha particular samem used.<br />
Tropk of Cancer—The nerthem parallel of<br />
decfirrstion, approximately 23”27 from the<br />
celaetii equstor, raeched by the Sun at ils<br />
r-neximum dacikdkn, or the ocrreapondng<br />
parallel on the Earth.<br />
Tropk of Caprico~The aeuthem parallel<br />
of declination, Spproxirnatety 23%?7 from the<br />
--- ~W SUuator, reached @.lha Sun at ils<br />
mesimum .3eol@stim, or the corresponding<br />
parallel on the Earth.<br />
tropical month-The average period of the<br />
revolutii of the Meon Mrcmt the Earth with<br />
I mamd 10 the vernal tmuinox, eppmsirnetefy 27<br />
1/3” days.<br />
tropkal yeer-The intervel of time between<br />
k wcumaive peaaogea of the Varnel equinox<br />
by rha Sun. The tmpics+l year is the yaar of the<br />
aaaama. and the MS of ttm sorwetimnal<br />
sekndsr year. Ake celled ●stronomic year;<br />
squlrtootkl yaec natural yaec solar<br />
year.<br />
tropopttuae-(JCS) The trenailbn zone<br />
between the atratosphare and the tmpoe@era.<br />
The tmpcpauaa normally cxxwrs et en aftiiude of<br />
atmut 25,000 to 45,CKN feet in pokr afd<br />
temperate zones, end at 55,0M feet in the<br />
lrepka. See also atmoriphera.<br />
troponphars+JCS) The kwer Iayara of<br />
atmcaphem, in wtich the ctwnge of<br />
temperature with halght is relatively large. It is<br />
the region where ckwds form, oonvastiin “m<br />
ediva, and mtzing ia cordnuoue and more or<br />
leas somplete. See ak.o atmosphara.<br />
MI L-HDBK-850<br />
260<br />
tropoapherk ecMter+JCS) The<br />
Propegm’m d radii waves by scattering as a<br />
* d iIIEWtikW or d~inuibs in the<br />
physical properties c4 the tmpOs@m.<br />
trough compasa-See daalinatoim.<br />
Troughton level-An Engfkh inatmrnant<br />
having thaq)iritteval PamW8ntty atteched to<br />
the top of the klhcopa tuba<br />
truo ●ltttuda-1. (JCS) The height of an<br />
aimmft as maaaured fm.tn mean see level. 2<br />
The add afIiiwte of a oskslii body above the<br />
Sakstial horizon. Akc czdkrt observed<br />
●ltltuda.<br />
truo empllWla-Ampktude relative to true<br />
nest or weet. See also amplltude.<br />
true anomsly—Sefr anomaly, definition 3.<br />
true azlmuttr-The horizontal dkestion of any<br />
line measured clc-drwisa from true rsx’th.<br />
true bearln~The horizontal angle between<br />
the meddkn line ard a tine en the Earth. Tne<br />
term true bsartng ia used in many cd the earty<br />
dessripticms of knd boumianes in the United<br />
states. h is associated with tma north. derring<br />
to the direction ef the north @nt aS detanmined<br />
by astmrrornk cbserwliens. If an eatrcrrcsmicaliy<br />
determined bauring is used, howemr, the term<br />
astrsrnomk boarlng ie preferred over truo<br />
besrlrtg.<br />
true dsprasslon ●rglxl%a setting of the<br />
tique cameras In the pfmt~ abcratf W*<br />
rebdion to the trus frarizon. It k defined by a my<br />
from the exposure statism ttwm@h the principal<br />
point d the obhque phc&gmph and a ray to the<br />
tme hol-kon.<br />
true dlmctlon-herkotial direstkm sspreeeed<br />
as angular dktance fmm true nrnth.<br />
true arror—See resultant error.<br />
true horizon—(JCS) 1. The boundary of a<br />
horizontal plane passing through a point d<br />
vision. 2. In pho!ogrammetry, the boundary of a<br />
horizontal plane pesdng Ihreugh the<br />
pemp-~e center of a lens eyetem. See al~<br />
horizon trsce.<br />
true llrm-A line of constant b-ring (rhumb