96 
Disse Observationer ere tagne paa Steder, hvor der These observations were taken in localities encumbered 
var Drivis. Et Maximum af Temperatur om Høsten i with drift-ice. A maximum of temperature in autumn at 
mindre Dybder antydes. af de Observationer, Cand. Wallem | comparatively inconsiderable depths, is shown to occur from 
gjorde med et Negretti- & Zambra’s Vendethermometer i | the observations of Mr. Wallem, with a Negretti & Zam- 
1884 i Egnen omkring Bodø, i Senjen, Malangen og Hids- bra inverting-thermometer, 1884, round Bodø, in Senjen, 
fjorden. Indtil de ringe Dybder, paa hvilke Cand. Wallem Malangen, and the Eidsfjord. Down to the trifling depths 
observerede, var Temperaturen i Regelen voxende med at which Mr. Wallem extended his observations, the tem- 
Dybden. TI de følgende Tilfælder kommer Maximum frem perature was found as a rule to increase with the depth. 
i ringere Dybde. In the following cases, a maximum is met with in lesser 
| depths. 
1884. Oct. 3. 1884. Oct. 10. 
Bakkeby. Sildpollen. 
Dybde (Depth) Temp. Dybde (Depth) Temp. 
Fayne. Meter. Fayne. Meter. 
(F'ms.) (Fms.) 
AG) O 9.9 O 0) 9°.9 
5 9 10.0 IO 18 10.8 
10 18 9.8 18 33 10.3 
16 2 9.4 NE Vind, fra Land. 
(Wind NE from Land.) 
Vi have seet, at ved Lødingen og i Altenfjorden viser We have seen that at Lødingen and in the Altenfjord 
Aarets : Middeltemperatur i Havet et Maximum ved Over- the annual mean temperature of the sea exhibits a max- 
fladen og et Minimum mellem 30 og 50 Favne. For at imum at the surface and a minimum between 30 and 50 
komme til Kundskab om, hvorledes det forholder sig i denne || fathoms. With a view to ascertain the law of distribution 
Henseende i Grønlandshavet, har jeg taget Medium af Capt. in the Greenland Sea, I took the mean of Capt. C. Bruun’s 
C. Bruun’s Temperaturreekker fra Marts og April 1878 og | serial temperatures from March and April 1878, comparing 
sammenstillet dette med vor Temperaturrekke fra Juli 1878 | it with our serial temperatures from July 1878, No. 298. 
No. 298. Middelet af Vinterrækken og Sommerrækken vil | The mean of the winter-series and of the summer-series 
give en tilnærmet Værdi for Aarets Middeltemperatur i de | will give an approximate value for the annual mean tem- 
forskjellige Dybder. Resultatet heraf sees af den følgende perature of the sea in the different depths. The result is 
Tabel. 5 shown by the following Table: — 
TD? BB? IN, Br BR? (TY Bl” 
10167 Es Wed. Wnty 10083, 
Dybde (Depth) Temperatur (Temperature) Aarlig: 
Favne. Meter. April 6. Juli 17. Aar. Var. 
(Fms.) (Xear.) (Range.) 
(0) O =2%0 4°.0 1°.0 6°.0 
20 SÅ SU off 2.3 0.3 4.0 
30 515 2210 > SØ off sil JO TG 
40 73 3240 119 0 Oil og” 1, 
50 91 ail 8 ait Ø =-1).2 © ol 
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.I 0.2 
120 219 —(0) ol 0.0 0.0 O.I 
Man 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 Temperaturcurven No. 298, Pl. VI 
og i Tversnittet XVII, Pl. XII ved denne Station. 
Ved Kysten er om Vinteren Temperaturen i Havet 
lavest ved Land og voxer saavel udover mod Søen som 
Here, too, we haye a maximum at the surface, and a 
minimum at the depth of 40 fathoms, in the annual mean tem- 
perature. From these data, the annual distribution of 
temperature in the upper 100 fathoms has been marked 
off in the curve of temperature No. 298, Pl. VI, 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- 
; pr 
å 
~ 
