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Record #104583:
- #104583
Main publication details
MARC recordThe spring in the forest terrain at Svartberget, Northern Sweden / Hans Odin, Christer Deg Ermark.
| Title: | The spring in the forest terrain at Svartberget, Northern Sweden / Hans Odin, Christer Deg Ermark. |
| Author(s): | Odin, Hans. Deg Ermark, Christer. |
| Date: | 1990. |
| In: | Geografiska Annaler. Series A. Physical Geography. (1990.), Vol. 72A(2) (1990) |
| Abstract: | Relationship between air temperature, soil temperature and snow cover has been studied at three different sites (1980-88). Maximum difference between first snow-free day and beginning of warming of mineral soil surface below vegetation and humus was only four days, but sites differed greatly between start of warming of soil surface and that of deeper soil layers. In early spring, change in temperature gradient in frozen and dry soil was observed, associated with infiltration of meltwater, and it occurred at almost same time as mean daily air temperature exceeded 0.5° C. |
| Notes: | Geografiska Annaler. Series A. Physical Geography. Vol. 72A(2) :167-178 (1990). |
| Keywords: | 551.524.4 -- Air temperatures, vertical distribution. 551.578.46 -- Snow cover and snow patches. 631.436 -- Soils, thermal properties. D -- Atmospheric sciences. (*57) -- Sweden. (*571) -- Norrland. |
| SPRI record no.: | 104583 |
LDR 01529naa#a2200000#a#4500 001 SPRI-104583 005 20230328100126.0 007 ta 008 230328s1990####xx#a##|##|###|0||#0|eng#d 035 ## ‡aSPRI-104583 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aOdin, Hans. 245 14 ‡aThe spring in the forest terrain at Svartberget, Northern Sweden /‡cHans Odin, Christer Deg Ermark. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1990. 300 ## ‡ap. 167-178 :‡bill., diags. 500 ## ‡aGeografiska Annaler. Series A. Physical Geography. Vol. 72A(2) :167-178 (1990). 520 3# ‡aRelationship between air temperature, soil temperature and snow cover has been studied at three different sites (1980-88). Maximum difference between first snow-free day and beginning of warming of mineral soil surface below vegetation and humus was only four days, but sites differed greatly between start of warming of soil surface and that of deeper soil layers. In early spring, change in temperature gradient in frozen and dry soil was observed, associated with infiltration of meltwater, and it occurred at almost same time as mean daily air temperature exceeded 0.5° C. 650 07 ‡a551.524.4 -- Air temperatures, vertical distribution.‡2udc 650 07 ‡a551.578.46 -- Snow cover and snow patches.‡2udc 650 07 ‡a631.436 -- Soils, thermal properties.‡2udc 650 07 ‡aD -- Atmospheric sciences.‡2local 651 #7 ‡a(*57) -- Sweden.‡2udc 651 #7 ‡a(*571) -- Norrland.‡2udc 700 1# ‡aDeg Ermark, Christer. 773 0# ‡7nnas ‡tGeografiska Annaler. Series A. Physical Geography. ‡gVol. 72A(2) (1990) ‡wSPRI-40621 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230328