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Ankerpladsen paa Vestsiden ligger 10. "9 nordligere og 1'
49." 1 vestligere end Fugleberget. Ankerpladsen paa Vest-
siden ligger altsaa 2' l."3 nordligere og 4' 27" vestligere
end Ankerpladsen paa 0stsiden. Er for den sidste r/>0 =
7.0° 58.'0 og Iq = 0h 33™ 48.'3, saa bliver for Ankerplad-
sen paa Vestsiden tpu — 71° 0' 1" og k0 — O'* 34m 6/1.
Efter do mindste Kvadraters Methode beregnede jeg
de sandsynligste Correctioner til <p0 og k .
Xaar jeg derefter grupperede Differentserne (hvis
Kvadratsum er Minimum) mellem de observerede (redu-
cerede) Hojder af Solcentret og de efter de fundne sand-
synligste Yferdier for Bredden og Lsengden beregnede,- efter
de obseyverede Solrender, viste det sig, at Middeldifferent-
sen for Ovre Band var -f- 0/295 og for nedre Band
— 0/282. Den observerede Solradius er saaledes gjennem-
snitlig 0/3 storre end den til Beregningen benyttede.
Corrigeres med .denne Storrelse, faaes .de i den folgende
Tabel anforte Yaerdier af Differentserne J mellem obser-
veret minus beregnet Solhojde. I Tabellen ere alle Uhr-
tider reducerede til Beid, og alle maalte Solhojder corri-
gerede for Indexfejl, Kimmingdaling,'Befraction, Parallaxe
og Solradius (Xaut. Almanac's), o betegner ovre Solrand,
n nedre Solrand. Aflaesningerne paa Sextan ten ere gjorte
i Secunder og Beductionen udfort med Secunder, men da
den sandsynlige Fejl' af en enkelt Hojde er over et halvt
Minut. opiores i Tabellen Tiendedels Minut, ligesoni Be-
regningen efter de mindste Kvadraters Methode er fort
med femzifrede Logarithmer.
anchorage oft' the east coast. From the foot of the Fugle-
berg. the height of the mast, as measured by myself on
the 29th of July, gave an angle of 0° 55/5, which corre-
sponds to a distance of 0/62. At this point, the azimuth
of the ship from the Fugleberg was about 70°. Computing
. with these results, our anchorage off the west coast should
lie 10."9 farther north and V 49."i farther west than the
Fugleberg. Hence, the anchorage off the west coast lies
2' l."3 farther north and 4' 27" • farther west than the
anchorage oft’ the east coast. Assuming for the latter <pa
: 70° 58/0 and ka = O'* 33”1 48/3, for the anchorage off
the west coaSt rp0 = 71° 0' 1" and l0 = O'* 34”‘ 6/1.
By the method of the least squares, I computed the
most probable corrections of f/0 and A0.
Then, on grouping the differences (the sum of the
squares of which is a minimum) between the observed
(duly corrected) altitudes of the sun’s centre and those
computed with the .most probable values found for latitude
and longitude, according to the observed solar limbs, the
mean difference for the upper limb proved to be -)- 0/295,
and for the lower — 0/282. On an average, therefore,
the observed semidiameter of the sun is 0/3 greater than
that taken for the computation. Corrected with this quan-
tity, we get the values given in the following Table for
the differences, J, between the observed and the computed
solar altitudes. In this Table all cbronometer-times are
reduced to those of the Beid chronometer', and all observed
altitudes corrected for the index-error, the dip of the hori-
zon, refraction, parallax, and the sun's semidiameter (from
Xaut. Almanac); o signifies upper solar limb, n lower solar
limb. The readings of the sextant were noted in seconds,
and their reduction computed in seconds; but the probable
error of a single altitude amounting to more than half a
minute, tenths of a minute have been given in the Table.
The computation by the method of the least squares is
made with five decimals in the logarithms.
Ankerplads paa Vestsiden. 1877. Juli 30.
(Anchorage on the West Side. 1877. July 30.)
Chron. Reid. Obs. H0jde. (Obs. Altitude.) Band. (Limb.) Sext. Obs. J
5a 47” 28‘ 20" 57/2 n. E. (?. 4- 0/9
5 48 1 20 56. 4 n. S. M. — i-3
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