Reconstructing 800 years of summer temperatures in Scotland from tree rings
We thank The Carnegie Trust for the Universities of Scotland for providing funding for Miloš Rydval’s PhD. The Scottish pine network expansion has been an ongoing task since 2007 and funding must be acknowledged to the following projects: EU project ‘Millennium’ (017008-2), Leverhulme Trust project...
Published in: | Climate Dynamics |
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Main Authors: | , , , , , , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
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2017
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Online Access: | http://hdl.handle.net/10023/10093 https://doi.org/10.1007/s00382-016-3478-8 |
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ftstandrewserep:oai:research-repository.st-andrews.ac.uk:10023/10093 |
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Open Polar |
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University of St Andrews: Digital Research Repository |
op_collection_id |
ftstandrewserep |
language |
English |
topic |
Temperature reconstruction Subfossil Tree-ring Scots pine Scotland GE Environmental Sciences QH301 Biology NDAS GE QH301 |
spellingShingle |
Temperature reconstruction Subfossil Tree-ring Scots pine Scotland GE Environmental Sciences QH301 Biology NDAS GE QH301 Rydval, Miloš Loader, Neil J. Gunnarson, Björn E. Druckenbrod, Daniel L. Linderholm, Hans W. Moreton, Steven G. Wood, Cheryl Victoria Wilson, Rob Reconstructing 800 years of summer temperatures in Scotland from tree rings |
topic_facet |
Temperature reconstruction Subfossil Tree-ring Scots pine Scotland GE Environmental Sciences QH301 Biology NDAS GE QH301 |
description |
We thank The Carnegie Trust for the Universities of Scotland for providing funding for Miloš Rydval’s PhD. The Scottish pine network expansion has been an ongoing task since 2007 and funding must be acknowledged to the following projects: EU project ‘Millennium’ (017008-2), Leverhulme Trust project ‘RELiC: Reconstructing 8000 years of Environmental and Landscape change in the Cairngorms (F/00 268/BG)’ and the NERC project ‘SCOT2K: Reconstructing 2000 years of Scottish climate from tree rings (NE/K003097/1)’. This study presents a summer temperature reconstruction using Scots pine tree-ring chronologies for Scotland allowing the placement of current regional temperature changes in a longer-term context. ‘Living-tree’ chronologies were extended using ’subfossil’ samples extracted from nearshore lake sediments resulting in a composite chronology > 800 years in length. The North Cairngorms (NCAIRN) reconstruction was developed from a set of composite blue intensity high-pass and ring-width low-pass chronologies with a range of detrending and disturbance correction procedures. Calibration against July-August mean temperature explains 56.4% of the instrumental data variance over 1866-2009 and is well verified. Spatial correlations reveal strong coherence with temperatures over the British Isles, parts of western Europe, southern Scandinavia and northern parts of the Iberian Peninsula. NCAIRN suggests that the recent summer-time warming in Scotland is likely not unique when compared to multi-decadal warm periods observed in the 1300s, 1500s, and 1730s, although trends before the mid-16th century should be interpreted with some caution due to greater uncertainty. Prominent cold periods were identified from the 16th century until the early 1800s – agreeing with the so-called Little Ice Age observed in other tree-ring reconstructions from Europe - with the 1690s identified as the coldest decade in the record. The reconstruction shows a significant cooling response one year following volcanic eruptions although this result is sensitive to the datasets used to identify such events. In fact, the extreme cold (and warm) years observed in NCAIRN appear more related to internal forcing of the summer North Atlantic Oscillation. Publisher PDF Peer reviewed |
author2 |
NERC University of St Andrews. Earth and Environmental Sciences University of St Andrews. Scottish Oceans Institute University of St Andrews. St Andrews Sustainability Institute |
format |
Article in Journal/Newspaper |
author |
Rydval, Miloš Loader, Neil J. Gunnarson, Björn E. Druckenbrod, Daniel L. Linderholm, Hans W. Moreton, Steven G. Wood, Cheryl Victoria Wilson, Rob |
author_facet |
Rydval, Miloš Loader, Neil J. Gunnarson, Björn E. Druckenbrod, Daniel L. Linderholm, Hans W. Moreton, Steven G. Wood, Cheryl Victoria Wilson, Rob |
author_sort |
Rydval, Miloš |
title |
Reconstructing 800 years of summer temperatures in Scotland from tree rings |
title_short |
Reconstructing 800 years of summer temperatures in Scotland from tree rings |
title_full |
Reconstructing 800 years of summer temperatures in Scotland from tree rings |
title_fullStr |
Reconstructing 800 years of summer temperatures in Scotland from tree rings |
title_full_unstemmed |
Reconstructing 800 years of summer temperatures in Scotland from tree rings |
title_sort |
reconstructing 800 years of summer temperatures in scotland from tree rings |
publishDate |
2017 |
url |
http://hdl.handle.net/10023/10093 https://doi.org/10.1007/s00382-016-3478-8 |
genre |
North Atlantic North Atlantic oscillation |
genre_facet |
North Atlantic North Atlantic oscillation |
op_relation |
Climate Dynamics Rydval , M , Loader , N J , Gunnarson , B E , Druckenbrod , D L , Linderholm , H W , Moreton , S G , Wood , C V & Wilson , R 2017 , ' Reconstructing 800 years of summer temperatures in Scotland from tree rings ' , Climate Dynamics , vol. 49 , no. 9-10 , pp. 2951-2974 . https://doi.org/10.1007/s00382-016-3478-8 0930-7575 PURE: 248169755 PURE UUID: c59fc9ef-9587-4089-8e77-eb91ebde5435 Scopus: 85009274759 ORCID: /0000-0003-4486-8904/work/59953625 WOS: 000414153800002 http://hdl.handle.net/10023/10093 https://doi.org/10.1007/s00382-016-3478-8 NE/K003097/1 |
op_rights |
(c) The Authors 2017. This article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. |
op_rightsnorm |
CC-BY |
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https://doi.org/10.1007/s00382-016-3478-8 |
container_title |
Climate Dynamics |
container_volume |
49 |
container_issue |
9-10 |
container_start_page |
2951 |
op_container_end_page |
2974 |
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1766136094384979968 |
spelling |
ftstandrewserep:oai:research-repository.st-andrews.ac.uk:10023/10093 2023-05-15T17:36:34+02:00 Reconstructing 800 years of summer temperatures in Scotland from tree rings Rydval, Miloš Loader, Neil J. Gunnarson, Björn E. Druckenbrod, Daniel L. Linderholm, Hans W. Moreton, Steven G. Wood, Cheryl Victoria Wilson, Rob NERC University of St Andrews. Earth and Environmental Sciences University of St Andrews. Scottish Oceans Institute University of St Andrews. St Andrews Sustainability Institute 2017-01-13T11:30:11Z 24 application/pdf http://hdl.handle.net/10023/10093 https://doi.org/10.1007/s00382-016-3478-8 eng eng Climate Dynamics Rydval , M , Loader , N J , Gunnarson , B E , Druckenbrod , D L , Linderholm , H W , Moreton , S G , Wood , C V & Wilson , R 2017 , ' Reconstructing 800 years of summer temperatures in Scotland from tree rings ' , Climate Dynamics , vol. 49 , no. 9-10 , pp. 2951-2974 . https://doi.org/10.1007/s00382-016-3478-8 0930-7575 PURE: 248169755 PURE UUID: c59fc9ef-9587-4089-8e77-eb91ebde5435 Scopus: 85009274759 ORCID: /0000-0003-4486-8904/work/59953625 WOS: 000414153800002 http://hdl.handle.net/10023/10093 https://doi.org/10.1007/s00382-016-3478-8 NE/K003097/1 (c) The Authors 2017. This article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. CC-BY Temperature reconstruction Subfossil Tree-ring Scots pine Scotland GE Environmental Sciences QH301 Biology NDAS GE QH301 Journal article 2017 ftstandrewserep https://doi.org/10.1007/s00382-016-3478-8 2022-04-14T22:27:34Z We thank The Carnegie Trust for the Universities of Scotland for providing funding for Miloš Rydval’s PhD. The Scottish pine network expansion has been an ongoing task since 2007 and funding must be acknowledged to the following projects: EU project ‘Millennium’ (017008-2), Leverhulme Trust project ‘RELiC: Reconstructing 8000 years of Environmental and Landscape change in the Cairngorms (F/00 268/BG)’ and the NERC project ‘SCOT2K: Reconstructing 2000 years of Scottish climate from tree rings (NE/K003097/1)’. This study presents a summer temperature reconstruction using Scots pine tree-ring chronologies for Scotland allowing the placement of current regional temperature changes in a longer-term context. ‘Living-tree’ chronologies were extended using ’subfossil’ samples extracted from nearshore lake sediments resulting in a composite chronology > 800 years in length. The North Cairngorms (NCAIRN) reconstruction was developed from a set of composite blue intensity high-pass and ring-width low-pass chronologies with a range of detrending and disturbance correction procedures. Calibration against July-August mean temperature explains 56.4% of the instrumental data variance over 1866-2009 and is well verified. Spatial correlations reveal strong coherence with temperatures over the British Isles, parts of western Europe, southern Scandinavia and northern parts of the Iberian Peninsula. NCAIRN suggests that the recent summer-time warming in Scotland is likely not unique when compared to multi-decadal warm periods observed in the 1300s, 1500s, and 1730s, although trends before the mid-16th century should be interpreted with some caution due to greater uncertainty. Prominent cold periods were identified from the 16th century until the early 1800s – agreeing with the so-called Little Ice Age observed in other tree-ring reconstructions from Europe - with the 1690s identified as the coldest decade in the record. The reconstruction shows a significant cooling response one year following volcanic eruptions although this result is sensitive to the datasets used to identify such events. In fact, the extreme cold (and warm) years observed in NCAIRN appear more related to internal forcing of the summer North Atlantic Oscillation. Publisher PDF Peer reviewed Article in Journal/Newspaper North Atlantic North Atlantic oscillation University of St Andrews: Digital Research Repository Climate Dynamics 49 9-10 2951 2974 |