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Record #159258:
Lapin jääkauden jälkeisten ilmastonmuutosten rekonstruktiot / Heikki Seppä.
Title: | Lapin jääkauden jälkeisten ilmastonmuutosten rekonstruktiot / Heikki Seppä. |
Translated title: | Reconstructing the post-glacial climatic changes in Lapland. |
Author(s): | Seppä, Heikki. |
Date: | 2001. |
Language: | Finnish. |
In: | Terra. (2001.), Vol. 113(3) (2001) |
Abstract: | Different time scales and methods give different aspects of climate history. Pollen-based ones suggest that early Holocene was maritime in character, with mild temperatures and high precipitation. Summer reached high point c. 6000-4500 BC, being average of 1.6-2.2 deg.C warmer than now, followed by gradual cooling. Independent methods, especially from Greenland ice cores, support general reconstructed trend. Possible short-term events are discussed. Cooler periods were at least c. 9300 BC and during Little Ice Age (800-300 yr ago). Cyclic cold events are unproven. |
Notes: | Terra. Vol. 113(3) :161-170 (2001). English summary p.161, English captions. |
Keywords: | 551.321.2 -- Snow and ice, methods of sampling, excavating, drilling, etc. 551.58 -- Climatology. 551.582 -- Climatology of particular places. 581.081.3 -- Pollen analysis. D -- Atmospheric sciences. (*3) -- Arctic regions. (*561) -- Finnish Lapland. |
SPRI record no.: | 159258 |
LDR 01615naa#a2200000#a#4500 001 SPRI-159258 005 20240328144935.0 007 ta 008 240328s2001####xx#ab#|##|###|0||#0|fin#d 035 ## ‡aSPRI-159258 040 ## ‡aUkCU-P‡beng‡eaacr 041 0# ‡afin 100 1# ‡aSeppä, Heikki. 242 10 ‡aReconstructing the post-glacial climatic changes in Lapland.‡yeng 245 10 ‡aLapin jääkauden jälkeisten ilmastonmuutosten rekonstruktiot /‡cHeikki Seppä. 260 ## ‡a[S.l.] :‡b[s.n.],‡c2001. 300 ## ‡ap. 161-170 :‡bill., diags., map. 500 ## ‡aTerra. Vol. 113(3) :161-170 (2001). 500 ## ‡aEnglish summary p.161, English captions. 520 3# ‡aDifferent time scales and methods give different aspects of climate history. Pollen-based ones suggest that early Holocene was maritime in character, with mild temperatures and high precipitation. Summer reached high point c. 6000-4500 BC, being average of 1.6-2.2 deg.C warmer than now, followed by gradual cooling. Independent methods, especially from Greenland ice cores, support general reconstructed trend. Possible short-term events are discussed. Cooler periods were at least c. 9300 BC and during Little Ice Age (800-300 yr ago). Cyclic cold events are unproven. 546 ## ‡aIn Finnish. 650 07 ‡a551.321.2 -- Snow and ice, methods of sampling, excavating, drilling, etc.‡2udc 650 07 ‡a551.58 -- Climatology.‡2udc 650 07 ‡a551.582 -- Climatology of particular places.‡2udc 650 07 ‡a581.081.3 -- Pollen analysis.‡2udc 650 07 ‡aD -- Atmospheric sciences.‡2local 651 #7 ‡a(*3) -- Arctic regions.‡2udc 651 #7 ‡a(*561) -- Finnish Lapland.‡2udc 773 0# ‡7nnas ‡tTerra. ‡gVol. 113(3) (2001) ‡wSPRI-21051 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240328