E n o n t e k i s . med, ex med. ex med. hor.
maximis minimis mediorum
Januar. 1 — 10 — 16 .3 — 2 r .8 — 19 0
I I — 20 — 14 -7 — i 9<8 — 17-2
21 — 31 — 1 4 .2 — i 8-5 — 16. 3
F eb r . 1 — 10 — 19 -9 — 2 3 .9 — 2 1 .9
1 1 — 20 — 1 3 .2 — 19 .9 — 1 6 .5
2 i — 28 — i 3-7 — 17- Ç — i 5-8
M a rt. I — JO — 8 .9 — 1 5 .4 — 1 2 . 1
I I — 20 — 7 .2 — 15-3 — 1 1 .2
2T — 31 — 7- 5„ — 1 4 .4 — 10 .9
A p r i l . I — 10 — 1 .2 . 7-7 — 4 .4
I I ---- 20 — ,0 .7 - 5-6 — 3-1
2 1 — 30 0 .9 — 3-9 — 1-5
M a ji 1 — 10 2 .3 2 .1 0 .1
I I — 20 4-8 0 .9 2 .8
2 1 — 31 6 .4 2 .9 4 .6
J u n ii I — IO 8 .2 4 .4 6-3
I I — 20 14. 2 9-5 i i . 8
21 — 31 1 2 .8 9 .2 1 1 .0
Julii-' I — IO IÔ.8 1 2 .2 .H - 5:
I I — 20 17.9 13 2 i 5- 5
21 — 31 I8 . 2 13-8 16 .0
AugUSt. I -r- IO l 8.3 14-5 1 6 .4
I I — 20 l6 . 4 11-. 4 13-9
2 1 — 31 i i - 5 8 . 1 9-8
Sept. I — .10 8-7 3-8 6 .2
I I — 20 9-5 4 .4 6.9
2 1 — 30 4-9 1-3 3-1
Octob. I — ^10 1 . 1 — 3 .3 — 1 .1
1 1 — 20 i -3 — 3-0 — 0 .8
21 — 31 — 2 .6 - 8-7 — 5-6
Novbr. 1 — To — 5-7 — 9-9 - 7-8
I I --- 20 — 6.87 — n -39 — 9.13
2T — 30 — 13-69 — i 8-33 — t6. 01
Decbr. 1 — 10 — 13-9 — 18 .4 — 1 6 . 1
11 — 20 — 1 3 .3 — 20.3 — 16.8
21 — 31 — 1.5- 8 — 2 1 .6 — 1 8 .7
Medium — 0.41]— 5-3 1 !
Median*
mensium.
— 17-50
— 18. 06
i— 11.40
— 3.00
if 50
9.70
i 5- 33
i 3- 36
5-40
— 2. 50 .
10.98
— 17.20
— 2.86
Hyerne (mens.I. II., et XII.) med. ex maximis — 14.98
minimis — 20.2 E
differentia 5.23
Vere (mens. III. IV. V .) med. ex maximis — 1.22
minimis — 6.73
differentia 5-5 1
Aestate (mens. VI. VII. VIII.) med. ex maximis 14.92
minimis 10.67
differentia 4., 25
i Antumno (mens. IX.X. XI.) med. ex maximis — 0.37
minimis — 5-00
differentia 4.63
Tale clima pro valde singular! sane habendum est,
ubi temperatura media totius anni ad — 2 °.86 et
mensis Januarii temperatura media ad — i8 ° .6 dela-
b itu r , et tamen temperatura media mensis aestivalis
Julii usque ad + 15°.33 elevatur, terraque adhuc 3yl-
va s , ne dicam olera, producere potest. < Id omnino
clima sibiricuin vel continentale clici meretur. Verunx
quidem est has observationes, quemadmodum nobis
quidem videtur, institutas esse cum thermometro Hy-
drargyri demumfrigus forsan justo intensius indicante;
quuin vero frigus infra — 4°° nonnisi bis annotatum
videamus sciL d. 23 Januarii 1803 et d. 5Februarii 1804»
I hanc considerationem paruin valere putamus, ad no-
stram computationem mutandam.
Has observationes Enontekenses satis common-
strant, quantum sibirico climate gaudeant Lapponise
svecicæ prope alpiurn jugum sit£ ; e s t-vero altera pars
lapponiæ, quæ clima ma-ritimum vel ut ita dicam islan-
dicum habet. In latere norvégien àlpium progressio-
nem longe aliam temperiei invenimus. lbi quoque la-
s ; ' titudo geographies major vel minor multum confert ad
i f temperatuçam minuendam vel augendam, quamquam
in propatulo est, situs terræ a mari vel remotioris vel
,j propioris si non majorem certe parem esse vim ac la-
titudinis ad clima teinperandum. In profundis et oc-
clusis illis convallibus inferalpinis Nordlandiæ meri-
dionalis temperaturam satis calidam esse comperimus.
•"É Cum ibi nullas habeamus observationes therinornetri-
cas, juvat eas adferre, quæ Nidr.osiæ institutæ sunt
utpote in loco aNordlandia norvegica non admodum