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flti
Disse Observationer ere tagne paa Steder, hvor
(leivar Drivis. Et Maximum af Temperatur om Hosten i
mindre Dybder antydes af de Observationer, Cand. Wallem
gjorde med et Negretti- & Zambia’s Vciulcthermoiaeter i
1*84 i Egnen omkring Bo,lo. i Senjen, Malangen og Eids.
fjorden. Indtil de ringe Dybder, paa hvilke Cand. Wallem
observerede, var Temperaturen i Regelen voxende ined
Dybden. I d.. følgende Tilfalder kommer Maximum frem
i ringere Dybde,
These observations were taken in localities encumbered
with drift-ice. A maximum of temperature in autumn at
comparatively inconsiderable depths, is shown to occur from
tile observations of Mr. Wallem, with a Negretti
Zambia iuvrrtiug-thomionieter. 1884. round Bodø, in Senjen,
Malangen, and tile Eidsfjord. Down to the trifling depths
at which Mr. Wallem extended his observations, the
temperature was found as a rule to increase with the depth.
In the following cases, a maximum is met with in lesser
depths.
Iss-l. lii-t. :;.
Bakkeby.
Dybde i h./.n,) Temp.
Favne. Meter.
! MM.)
ü O ’i".I)
5 <1
10 i8 0.8
|6 29 0.4
1SS4. Oct. in.
SUilpiillen.
JlyMo (D.fM) Tcih|I.
Favue-. Meter.
o o cl".0
10 18 10.S
18 33 10.3
NK Vin.l. Ira Laud.
(UV»,/ .VA’/i-w» Lwé)
Vi have seet. at ved Lodingen og i Altenfjorden viser
Aarets Middeltemperatur i Havet et Maximum ved
Overfladen og et Minimum niellelll 30 og 50 Favue. For at
komme til Kundskab 0111, hvorledes det forholder sig i denne
Henseende i Grønlandshavet, bar jeg taget Medium afCapt.
C. Bruun’» Temperaturiwkkcr fra Marts og April 1878 og
sammenstillet dette med vor Temperatumekke fra Juli 1878
No. 2H8. Middelet af Viutcmrkkcn og Sommerra-klien vil
give ell tilnamnet Va-rdi for Aarets Middeltemperatur i de
forskjellige Dybder. Resultatet heraf sees af den følgende
Tabel.
We have seen that at Lødingen and in the Altenfjord
the annual mean temperature of the sea exhibits a
maximum at the surface aud a minimum between 30 and ÖO
fathoms. With a view to ascertain the- law of distribution
ill the Greenland Sea. I took the mean of Capt. C. Bruuns
serial temperatures from March and April 1878, comparing
it with our serial temperatures from July 1878. No. 2»8.
The mean of the winter-series and of the summer-series
will give an approximate value for the annual mean
temperature of the sea in the different depths. The result is
shown by the following Table: —
72° 1" Mi’ N. Hr. Ili’ E. Lgd. 72" :.2’ 1° 51’ 72".’.4’ 1° 3:*.’
Dyl>de iVe,.th) r (Tempe, •aturc) Aarlig
Favue. Meter, April (i. .1 uli 17. Aar. Var.
(I-»’*-) (Year.) (Bange.)
O 0 -2°.0 4".o 1".0 6".o
20 37 -I .7 2 -3 0 -3 4 -o
30 55 -2 .0 -0 .1 - I .0 1 .9
40 73 -2 .0 -0 .8 -3s 1 .2
SO 01 -1 -3 -i .2 -1 .2 0 .1
60 110 -0.6 -i .1 -0.8 0-5
80 146 -0 .4 -0.4 -0.4 0 .0
100 183 -0 .2 0 .0 -0.1 0 .2
120 2iq -0 .1 0 .0 0 .0 0:1
Mail faar ogsaa her et Maximum i Overfladen og et
Minimum i 40 Favnes Dyb i den aarlige Middeltemperatur.
Herefter er Temperaturens Fordeling for Aaret i de øverste
100 Favne construeret i Teniperaturcurven No. 298, Pl. VI
og i Tversnittet XVII. Pi. XII ved denne Station.
Ved Kysten er 0111 Vinteren Temperaturen i Havet
lavest ved Land øg voxer saavel udover mod Søen som
Here, too, we have a maximum at the surface, and a
minimum at the depth of 40 fathoms, ill the annual mean
temperature. From these data, the annual distribution of
temperature in the upper 100 fathoms has been marked
off in the curve of temperature No. 2’J8. Pl. VT. and in the
transverse section XVII. Pl. XII. at that Station.
Off the coast, the temperature of the sea in winter
is lowest inshore, augmenting alike seaward and down-
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