accessibility__skip_menu__jump_to_main

Full text: Annalen der Hydrographie und maritimen Meteorologie, 22 (1894)

Börgen: Ueber eine neue Methode, die harmonischen Konstanten’ abzuleiten, 229 
a) Bei den halbtägigen Tiden ist genähert in ix t = in ix (t + 12%) 
und == os ix (t + 6°), wir müssen daher die um 12 Stunden auseinander 
liegenden Werthe von Dt zusammenaddiren und die um 6 Stunden auseinander 
liegenden Summen von einander subtrahiren. - 
Es ist nach (9) 
Di = — Ay c08 t ix + Bzx sin t ix — Ay cost iy + By sin tiy— ++... 
und 
D12t + t = — Ax (cos 12% + €) ix + Bx sin (12% + t) ix — Ay cos (12 + t) iy + By sin (12b + t) iy — -4+<0+++ 
also: 
Dit-+ Dia + t= St = — 2 Ax cos 6 ix cos (6 + €) ix + 2 Bx cos 6 ix sin (6 + t) iz — 2 Ay cos 6 iy cos (6 +) iy 
. +2 By cos 6 iy sin (6 +) iy — + ++« 4 
Sirt= — 24x cos 6 ix cos (12 +) ix +72 Bz cos 6 ix sin (12 +) ix— 2 Ay cos 6iy cos (12 +t) iy 
* +2 By cos 6 iy sin (12 +) iy — «004 
Daher: 
St — Se +4 = — 4 Ax cos 6 ix sin 3 ix sin (9 + t) iz — 4 By cos 6 ix sin 3 ix cos (9 + t) ix 
— 4 Ay cos 6 iy sin 3 iy sin (9 + t) iy — 4 By cos 6 iy sin 3 iy cos (9 +) iy — +++ 
Auf bekannte Weise ergeben sich nun Fx‘ und Gx’ durch die Formeln: 
5 
| = 3 (St — So4+4) sin (9+1) ix 
5 5 
= —4 cos 6 ix sin 3 ix {ax Z sin (9 +1) ix? + Bx X sin (9 +1) ix cos (@+9i} 
„0 0 
5 5 
— 4 cos 6 iy sin 3 iy {Ay 3 sin (9 + t) ix sin (9 + t) iy + By X sin (9 + €) ix cos (9 +) ir} — 0... 
9 0 
5 
Gx‘ =Z8— S6 ++) cos (9 + t) ix 
5 ; 5 
=-—4cos 6 ix sin 3 ix {ax X sin (9 +) ix cos (9 +) ix +Bx 3 cos (9-4) ix :} 
0 0 
5 5 
— 4 cos 6 iy sin 3 iy {Ay X cos (9 + t) ix sin (9 + t) iy + By 3 cos (9 +) ix cos 0+0iy} — u... 
9 
Es sei 
(14) } 
| a= Zen kt=3 co 23 ix 
5006 (0 +0) ixt = 3-43 MRS G05 23 
Sin (9 +) ix 005 (0 + 0) ir = Zr ng si0 28 1a 
3 sin (9 +) ix Ei ws iy) + Re (ix — iy) 
2 sin (9 +1) ix (00 ein (x + iy) + yet (ix — iy) 
20 (0 +9 sin@+ 0 => En (ix + iy) + ED (ix — iy) 
g = Z cos {9 + €) ix cos +0 GE (ix + iy}) + EDS (ix — iy) 
und ferner: 
(15) 
m = -— 48 cos 6 ix sin 3 ix 
| n = — 4c cos 6 ix sin 3 ix 
pP = — 4d cos 6 iy sin 3 iy 
a = — 4e cos 6 iv sin 3 iv 
r == — 4b cos 6 ix sin 3 ix 
8 == — 4f cos 6 iy sin 3 Iy 
t=— — 4g cös 6 iv sin 3 iv
	        
Waiting...

Note to user

Dear user,

In response to current developments in the web technology used by the Goobi viewer, the software no longer supports your browser.

Please use one of the following browsers to display this page correctly.

Thank you.