Higher-than-present medieval pine (Pinus sylvestris) treeline along the Swedish scandes

The upper treeline of Scots pine (Pinus sylvestris L.) is renowned as a sensitive indicator of climate change and variability. By use of megafossil tree remains, preserved exposed on the ground surface, treeline shift over the past millennium was investigated at multiple sites along the Scandes in n...

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Published in:Landscape Online
Main Author: Kullman, Leif
Format: Article in Journal/Newspaper
Language:English
Published: Umeå universitet, Institutionen för ekologi, miljö och geovetenskap 2015
Subjects:
Online Access:http://urn.kb.se/resolve?urn=urn:nbn:se:umu:diva-212352
https://doi.org/10.3097/LO.201542
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spelling ftumeauniv:oai:DiVA.org:umu-212352 2023-10-29T02:36:15+01:00 Higher-than-present medieval pine (Pinus sylvestris) treeline along the Swedish scandes Kullman, Leif 2015 application/pdf http://urn.kb.se/resolve?urn=urn:nbn:se:umu:diva-212352 https://doi.org/10.3097/LO.201542 eng eng Umeå universitet, Institutionen för ekologi, miljö och geovetenskap International Association for Landscape Ecology Landscape Online, 2015, 42:1, s. 1-14 http://urn.kb.se/resolve?urn=urn:nbn:se:umu:diva-212352 doi:10.3097/LO.201542 Scopus 2-s2.0-84940040383 info:eu-repo/semantics/openAccess Climate change Little ice age Medieval warm period Megafossils Pinus sylvestris Swedish scandes Treeline Climate Research Klimatforskning Ecology Ekologi Article in journal info:eu-repo/semantics/article text 2015 ftumeauniv https://doi.org/10.3097/LO.201542 2023-10-04T22:36:29Z The upper treeline of Scots pine (Pinus sylvestris L.) is renowned as a sensitive indicator of climate change and variability. By use of megafossil tree remains, preserved exposed on the ground surface, treeline shift over the past millennium was investigated at multiple sites along the Scandes in northern Sweden. Difference in thermal level between the present and the Medieval period, about AD 1000-1200, is a central, although controversial, aspect concerning the detection and attribution of anthropogenic climate warming. Radiocarbon-dated megafossil pines revealed that the treeline was consistently positioned as much as 115 m higher during the Medieval period than today (AD 2000-2010), after a century of warming and substantial treeline upshift. Drawing on the last-mentioned figure, and a lapse rate of 0.6 o C/100 m, it may be inferred that Medieval summer temperatures were about 0.7 o C warmer than much of the past 100 years. Extensive pine mortality and treeline descent after the Medieval warming peak reflect substantially depressed temperatures during the Little Ice Age. Warmer-than-present conditions during the Medieval period concur with temperature reconstructions from different parts of northern Fennoscandia, northwestern Russia and Greenland. Modern warming has not been sufficient to restore Medieval treelines. Against this background, there is little reason to view further modest warming as unnatural. Article in Journal/Newspaper Fennoscandia Greenland Northern Sweden Umeå University: Publications (DiVA) Landscape Online 42 1 14
institution Open Polar
collection Umeå University: Publications (DiVA)
op_collection_id ftumeauniv
language English
topic Climate change
Little ice age
Medieval warm period
Megafossils
Pinus sylvestris
Swedish scandes
Treeline
Climate Research
Klimatforskning
Ecology
Ekologi
spellingShingle Climate change
Little ice age
Medieval warm period
Megafossils
Pinus sylvestris
Swedish scandes
Treeline
Climate Research
Klimatforskning
Ecology
Ekologi
Kullman, Leif
Higher-than-present medieval pine (Pinus sylvestris) treeline along the Swedish scandes
topic_facet Climate change
Little ice age
Medieval warm period
Megafossils
Pinus sylvestris
Swedish scandes
Treeline
Climate Research
Klimatforskning
Ecology
Ekologi
description The upper treeline of Scots pine (Pinus sylvestris L.) is renowned as a sensitive indicator of climate change and variability. By use of megafossil tree remains, preserved exposed on the ground surface, treeline shift over the past millennium was investigated at multiple sites along the Scandes in northern Sweden. Difference in thermal level between the present and the Medieval period, about AD 1000-1200, is a central, although controversial, aspect concerning the detection and attribution of anthropogenic climate warming. Radiocarbon-dated megafossil pines revealed that the treeline was consistently positioned as much as 115 m higher during the Medieval period than today (AD 2000-2010), after a century of warming and substantial treeline upshift. Drawing on the last-mentioned figure, and a lapse rate of 0.6 o C/100 m, it may be inferred that Medieval summer temperatures were about 0.7 o C warmer than much of the past 100 years. Extensive pine mortality and treeline descent after the Medieval warming peak reflect substantially depressed temperatures during the Little Ice Age. Warmer-than-present conditions during the Medieval period concur with temperature reconstructions from different parts of northern Fennoscandia, northwestern Russia and Greenland. Modern warming has not been sufficient to restore Medieval treelines. Against this background, there is little reason to view further modest warming as unnatural.
format Article in Journal/Newspaper
author Kullman, Leif
author_facet Kullman, Leif
author_sort Kullman, Leif
title Higher-than-present medieval pine (Pinus sylvestris) treeline along the Swedish scandes
title_short Higher-than-present medieval pine (Pinus sylvestris) treeline along the Swedish scandes
title_full Higher-than-present medieval pine (Pinus sylvestris) treeline along the Swedish scandes
title_fullStr Higher-than-present medieval pine (Pinus sylvestris) treeline along the Swedish scandes
title_full_unstemmed Higher-than-present medieval pine (Pinus sylvestris) treeline along the Swedish scandes
title_sort higher-than-present medieval pine (pinus sylvestris) treeline along the swedish scandes
publisher Umeå universitet, Institutionen för ekologi, miljö och geovetenskap
publishDate 2015
url http://urn.kb.se/resolve?urn=urn:nbn:se:umu:diva-212352
https://doi.org/10.3097/LO.201542
genre Fennoscandia
Greenland
Northern Sweden
genre_facet Fennoscandia
Greenland
Northern Sweden
op_relation Landscape Online, 2015, 42:1, s. 1-14
http://urn.kb.se/resolve?urn=urn:nbn:se:umu:diva-212352
doi:10.3097/LO.201542
Scopus 2-s2.0-84940040383
op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.3097/LO.201542
container_title Landscape Online
container_volume 42
container_start_page 1
op_container_end_page 14
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