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84
Under lOU Favne er Temperaturen i samme Vertical
constant (No. 81 eller svagt aftagende meel Dybden. Fra
Sydvest mod Nordost, fra Havet mod Land, er don
gennemsnitlige Dyb-Temperatur aftagende.
Udenfor Folden-Fjorden ligger en Banke, der grunder
op til lin Favne Vand. Mellem denne og Kysten strækker
sig en Dybreude, adskilt fra Foldenljordens ved en
grundere Ryg. I den förste har man fra "Hansteen" taget
ful-gende Temperaturrækker.
Below 100 fathoms, the temperature in the same
vertical is constant |No. 8), or diminishes slightly with the
depth. From the south-west to the north-east, or from the
sea towards the land, the average deep-temperature is found
to decrease.
Off the F oldenfjord. lies a bank on which the water
shoals up to (ill fathoms. Between this bank and the const,
extends a deep-channel, cut of from that of the Foldenfjord
by a shallower ridge. In the former, the following serial
temperatures were taken from the ■’Hansteen."
H. No. 10. H No. 11. H. No. 12. H. No. 3.
!SS0. Juli 21 0. Juli i) 1SS. . Juli ISNO Juli •211.
tø* •> 1’ N’. Br. !•" 21’ E. Lgd. <S4° 40’ N. Br. !l" -’o’ E. Ljv.l. <i 1" .-.n’ X. \r. !)" •_’<!’ E. Lgd. ’U" IN’ X. Br. 10" .’ IS. Lgd.
Favne. Moter. Temp. Favne. Meter. Temp. Favne. Meter. Temp. Favne. Meter. Temp.
(*■’««)• H
0 0 I2".4 0 0 u°.8 0 0 12".I 0 0 12".2
5 1 12.2 10 (8 11 .1 5 9 12 .0 5 9 ’’ -3
10 18 10 .2 20 37 10.4 10 18 11 .5 10 18 11 .2
20 37 8 .0 30 55 8.4 20 37 0 -4 20 37 10 .0
30 55 7-5 40 73 7-9 30 55 S-6 30 55 9 .2
40 73 7-5 50 9.1 7-4 40 73 8 -2 40 73 8.4
6t 112 7 -4 61 112 7-5 61 112 7-7 (h 112 8.0
82 1^0 7-2 82 ’50 7-3 82 150 7 -3 82 ’So 7 -9
124 227 7 >0 •03 188 7.6 103 188 7-0 103 188 7 -7
15. .44 263 6 .9 •55 283 7 -2 B. 127 232 6.9 129 236 7-4
B. 206 377 6.9 <55 283 7
Teiu| eraturen er synkende fra 100 Favne til Bunden.
Observationerne stemme vel overens medde paa
Nordhavs-Expeditionen i det samme Strog i 1870 maalt« (No. 55 til
No. til) Bundtemperaturer, der gan. fra 7».2 til G°.9.
Paa Vestsiden af den ovennævnte Banke har
"Hansteen" to Temperatumekker.
The temperature continues sinking from a depth of loo
fathoms to the bottom. The observations exhibit excellent
agreement with the bottom-temperatures — from 7°.2 to 6°.9;
Nos. 55—01 — registered on the North-Atlantic
Expedition in 18713 throughout the same tract.
On the west side of the aforesaid bank, we have two
serial temperatures from the "Hansteen,"
H. No. 14.
1880. Juli -it.
ii4" as’ X. Br. 8° i.v E. Lgil.
Favne. Meter. Temjj
O O I2’’.3
5 9 II-5
10 18 II .4
20 37 10.8
30 55 9.8
4° 73 8 -7
6i 113 7.8
82 150 7.3
103 188 6.9
II. 115 210 6.9
Temperaturen aftager med Dybden i de dybere Lag.
Paa Nordhavs-Expeditionen fandtes midt imellem disse f
Punkter (Station No. (17) i 119 Favnes Dyb 6°.9. Altsaa
en meget nær Overensstemmelse.
H. N 0. I 15.
1880. J uli 2s.
(i4° .Mi’ X. Hr. s" : E. Lgd.
Favne. Ä [eter Temp.
(>"»««).
0 0 12°. 2
5 9 12 .O
10 18 ti .6
20 37 9 .0
30 55 8.4
40 73 8 .0
61 112 7 -7
82 ’50 7-2
B. ut 203 6.8
The temperature diminishes with the depth in the
deeper strata. Ou the North-Atlantic Expedition, a
temperature of 0°.9 was measured midway between these points
(Station No. 07), at a depth ol’ 119 fathoms. Accordingly,
a very close agreement.
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