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Full text: Annalen der Hydrographie und maritimen Meteorologie, 17 (1889)

Berechnung der Gangformela für Marine-Chronometer. 
305 
Ausgleichung III. 4-12,0 
[ab] 
0,0 
[ac] 
4-31,0 
[ad] 
4-932,5 
[ae] 
4-25,0 
[bb] 
4-14300,0 
[bc| 
-4,0 
[bd] 
4-28,5 
[be] 
4-815,0 
[cc] 
4-93246 
[cd] 
4-7006,27 
[cc] 
—765,6 
[dd] 
4-140419,37 
[de] 
4-584,1 
[ee] 
4-1507,0 
Auflösung der Norraalgleichuiigen. 
Ausgleichung I. 
[bill] =. (0,000000 ) [bn] 
[eng] — (0,446721 )[bn] 4- (0,000000 )[cn] 
tdngj — (7,544278n) [b »] 4- (0,731874a) [en] 4- (0,000000) [dn] 
x — (7,481550a) [eng] 4 (7,169565a) [<lng] 
y = (5,844664)[bin] 4- (3,510093 ) [eng] 4- (2,909192«) [dn 3 ] 
z = (7,069369 ) [e 112] 4- (6,096788n) [dns] 
t. — (5,364914 ) [<1 n:i] 
[w] = [nn] 4-(5,844664») [bni]ä + (7,069369«) [cng] 2 4- (5,364914n)[dr.;,p 
es. [» n]'— £b n] y — [c a] z — [du] t (Kontrolle) 
Ausgleichung IL 
[hm] 1 
V siehe Ausgleichung I. 
[cns] ) 
[ens] = (3,75374ln) [tut] 4- (9,983423) [c d] 4- (0.000000) [eu] 
x — (7481550h) [eng] 4-(7,884234») [ens] 
y = (5,844664) [bn,] 4- (3,516093 )£«»*] + (5,975339h) [en 3 ] 
z —* (7,069369 ) [cns-] 4- (7,210021 ) [enj] 
u = (7,221598 ) [en3] 
[w] = [nn] 4- (5,844664») [hm] 2 4- (7,069369h) [cos] 2 4- (7,221598h) [«ns] 2 
= [nn] — [bn] y — [en] z—[eu] u (Kontrolle) 
Ausgleichung III. 
[ent] = (8,751801h)[bn] 4- (0,134530) [en] 4- (8,858533h) [da] 4- (0,000000) [en] 
x « xo 4- (5,189352 ) [en.,] 
y = yo4-(6,177351n) [en,] 
z = zo 4~ (7,560080 ) [ein] 
t — to 4- (6,284083a} [en,j] 
u = (7,425550 ) [ent] 
Die Werthe xo, yo, zo, U) und [wo] sind gleich den 
Glotsen x, y, z, t und [v v] in Ausgleichung I. 
[v v] — [V vo] 4- (7,425550n) [en,] 2 
-- [an] — [bn] y — [ca] z — [da] t — [en] u (Kontrolle) 
Durch Einsetzung der für jedes Chronometer einzeln zu berechnenden 
Werthe [bn], [cn], [dnj und [en] ergeben sich dann für die drei Ausgleichungen 
die folgenden Gangformeln sowie die mittleren Fehler der einzelnen Kocfficienten.
	        
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