Geomorphic features as indicators of climatic fluctuations in a periglacial environment, northern Sweden / Rolf Nyberg, Lars Lindh.

MARCXML

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008 230327s1990####xx#ab#|##|###|0||#0|eng#d
035 ## ‡aSPRI-104586
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aNyberg, Rolf.
245 10 ‡aGeomorphic features as indicators of climatic fluctuations in a periglacial environment, northern Sweden /‡cRolf Nyberg, Lars Lindh.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1990.
300 ## ‡ap. 203-210 :‡bill., diags., table, map.
500 ## ‡aGeografiska Annaler. Series A. Physical Geography. Vol. 72A(2) :203-210 (1990).
520 3# ‡aIn Abisko mountains. Debris flows and slush flows were possibly frequent during Little Ice Age, according to lichenometric dating. Field observations suggest fairly high frequency also during last few decades. Boulder pavements, moraine-like ridges and glacial striae in front of major snow fields indicate that previously that these were larger and in some cases active as small glaciers, perhaps in beginning of 1900s. During warmer 1920s-30s snow patches and glaciers, as well as permafrost mounds, were affected by general degeneration. It is suggested that features are beginning to respond to cooling trend affecting northern Scandinavia since about 1940. Impact of greenhouse warming has not yet been noticeable in this area.
650 07 ‡a551.343 -- Periglacial processes. Thermokarst.‡2udc
650 07 ‡a551.4 -- Geomorphology.‡2udc
650 07 ‡a551.582 -- Climatology of particular places.‡2udc
650 07 ‡a551.583 -- Climatic changes.‡2udc
650 07 ‡aE8 -- Glaciology: frost action and permafrost.‡2local
651 #7 ‡a(*57) -- Sweden.‡2udc
651 #7 ‡a(*571.12) -- Torne lappmark.‡2udc
700 1# ‡aLindh, Lars.
773 0# ‡7nnas ‡tGeografiska Annaler. Series A. Physical Geography. ‡gVol. 72A(2) (1990) ‡wSPRI-40621
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20230327