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Record #104582:
- #104582
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MARC recordInversion characteristics in a valley. Data from Máze (Masi) on Finnmarksvidda, Northern Norway / Per Øyvind Nordli.
| Title: | Inversion characteristics in a valley. Data from Máze (Masi) on Finnmarksvidda, Northern Norway / Per Øyvind Nordli. |
| Author(s): | Nordli, Per Øyvind. |
| Date: | 1990. |
| In: | Geografiska Annaler. Series A. Physical Geography. (1990.), Vol. 72A(2) (1990) |
| Abstract: | Based on information from three meteorological observation stations operational since autumn 1981 and situated at bottom, on side and at top of valley. Temperature inversions most frequent in winter, especially December. No variation in frequency of inversion during day from November to January; greatest daily variation observed in period February-May. Inversions more frequent in cold winters, but below -15° C there is no correlation between monthly mean temperature and frequency of valley inversion. Inversion near valley floor may even be missing in extremely cold weather. Temperature inversions cause mean temperature to increase with elevation between November and March. |
| Notes: | Geografiska Annaler. Series A. Physical Geography. Vol. 72A(2) :157-166 (1990). |
| Keywords: | 551.524.4 -- Air temperatures, vertical distribution. D -- Atmospheric sciences. (*58) -- Norway. (*582) -- Finnmark. |
| SPRI record no.: | 104582 |
LDR 01528naa#a2200000#a#4500 001 SPRI-104582 005 20231210104408.0 007 ta 008 231210s1990####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-104582 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aNordli, Per Øyvind. 245 10 ‡aInversion characteristics in a valley. Data from Máze (Masi) on Finnmarksvidda, Northern Norway /‡cPer Øyvind Nordli. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1990. 300 ## ‡ap. 157-166 :‡bdiags., tables, map. 500 ## ‡aGeografiska Annaler. Series A. Physical Geography. Vol. 72A(2) :157-166 (1990). 520 3# ‡aBased on information from three meteorological observation stations operational since autumn 1981 and situated at bottom, on side and at top of valley. Temperature inversions most frequent in winter, especially December. No variation in frequency of inversion during day from November to January; greatest daily variation observed in period February-May. Inversions more frequent in cold winters, but below -15° C there is no correlation between monthly mean temperature and frequency of valley inversion. Inversion near valley floor may even be missing in extremely cold weather. Temperature inversions cause mean temperature to increase with elevation between November and March. 650 07 ‡a551.524.4 -- Air temperatures, vertical distribution.‡2udc 650 07 ‡aD -- Atmospheric sciences.‡2local 651 #7 ‡a(*58) -- Norway.‡2udc 651 #7 ‡a(*582) -- Finnmark.‡2udc 773 0# ‡7nnas ‡tGeografiska Annaler. Series A. Physical Geography. ‡gVol. 72A(2) (1990) ‡wSPRI-40621 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20231210