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Record #126741:

Lateglacial and Holocene glacier fluctuations and climate variations in western Norway: a review / Atle Nesje, Svein Olaf Dahl.

Title: Lateglacial and Holocene glacier fluctuations and climate variations in western Norway: a review / Atle Nesje, Svein Olaf Dahl.
Author(s): Nesje, Atle.
Dahl, Svein Olaf.
Date: 1993.
In: Quaternary Science Reviews. (1993.), Vol. 12(4) (1993)
Abstract: Evidence from moraine, palynological data, and tree limits suggest that considerable climate changes occurred from late glacial (14 ka BP) up to present, and especially during Younger Dryas and Erdalen events and Little Ice Age (11-10 ka BP, 9.1±2 ka BP, and mid-18th century, respectively). Jostedalbre and most of west Norwegian glaciers disappeared during Early Holocene (8-6 ka BP) and reformed about 5 ka BP. From 2.5 ka BP, equilibrium-line altitude fluctuated around modern levels. Modern glaciers reached maximum neoglacial extent during Little Ice Age.
Notes:

Quaternary Science Reviews. Vol. 12(4) :255-261 (1993).

Keywords: 551.336 -- Ice ages.
551.791 -- Pleistocene.
551.794 -- Holocene.
551.324.63 -- Land ice, advance and retreat.
551.583.3 -- Climatic changes, Quaternary.
551.583.2 -- Climatic changes, historic.
551.588.5 -- Climate, relationship with ice.
001.814.4 -- Review article.
E7 -- Glaciology: glacial geology and ice ages.
(*58) -- Norway.
SPRI record no.: 126741

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100 1# ‡aNesje, Atle.
245 10 ‡aLateglacial and Holocene glacier fluctuations and climate variations in western Norway :‡ba review /‡cAtle Nesje, Svein Olaf Dahl.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1993.
300 ## ‡ap. 255-261 :‡bdiag., map.
500 ## ‡aQuaternary Science Reviews. Vol. 12(4) :255-261 (1993).
520 3# ‡aEvidence from moraine, palynological data, and tree limits suggest that considerable climate changes occurred from late glacial (14 ka BP) up to present, and especially during Younger Dryas and Erdalen events and Little Ice Age (11-10 ka BP, 9.1±2 ka BP, and mid-18th century, respectively). Jostedalbre and most of west Norwegian glaciers disappeared during Early Holocene (8-6 ka BP) and reformed about 5 ka BP. From 2.5 ka BP, equilibrium-line altitude fluctuated around modern levels. Modern glaciers reached maximum neoglacial extent during Little Ice Age.
650 07 ‡a551.336 -- Ice ages.‡2udc
650 07 ‡a551.791 -- Pleistocene.‡2udc
650 07 ‡a551.794 -- Holocene.‡2udc
650 07 ‡a551.324.63 -- Land ice, advance and retreat.‡2udc
650 07 ‡a551.583.3 -- Climatic changes, Quaternary.‡2udc
650 07 ‡a551.583.2 -- Climatic changes, historic.‡2udc
650 07 ‡a551.588.5 -- Climate, relationship with ice.‡2udc
650 07 ‡a001.814.4 -- Review article.‡2udc
650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local
651 #7 ‡a(*58) -- Norway.‡2udc
700 1# ‡aDahl, Svein Olaf.
773 0# ‡7nnas ‡tQuaternary Science Reviews. ‡gVol. 12(4) (1993) ‡wSPRI-78722
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