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A 520 year record of summer sunshine for the eastern European Alps based on stable carbon isotopes in larch tree rings
Climate Dynamics, Volume: 43, Issue: 3-4, Pages: 971 - 980
Swansea University Authors: Danny McCarroll, Iain Robertson , Neil Loader , Mary Gagen , Giles Young
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DOI (Published version): 10.1007/s00382-013-1864-z
Abstract
A 520-year stable carbon isotope chronology from tree ring cellulose in high altitude larch trees (Larix decidua Mill.), from the eastern European Alps, correlates more strongly with summer temperature than with summer sunshine hours. However, when instrumental records of temperature and sunshine di...
Published in: | Climate Dynamics |
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2014
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2019-02-13T17:41:59.8227645 v2 23984 2015-10-26 A 520 year record of summer sunshine for the eastern European Alps based on stable carbon isotopes in larch tree rings 6d181d926aaac8932c2bfa8d0e7f6960 Danny McCarroll Danny McCarroll true false ef8912c57e0140e9ecb2a69b7e34467e 0000-0001-7174-4523 Iain Robertson Iain Robertson true false 8267a62100791965d08df6a7842676e6 0000-0002-6841-1813 Neil Loader Neil Loader true false e677a6d0777aed90ac1eca8937e43d2b 0000-0002-6820-6457 Mary Gagen Mary Gagen true false e0c807e6b9b663f1c297feecd2f54c3a Giles Young Giles Young true false 2015-10-26 FGSEN A 520-year stable carbon isotope chronology from tree ring cellulose in high altitude larch trees (Larix decidua Mill.), from the eastern European Alps, correlates more strongly with summer temperature than with summer sunshine hours. However, when instrumental records of temperature and sunshine diverge after AD 1980, the tree ring time series does not follow warming summer temperatures but more closely tracks summer sunshine trends. It is concluded that sunshine is the dominant control on carbon isotope fractionation in these trees, via the influence of photosynthetic rate on the internal partial pressure of CO2, and that high summer (July-August) sunshine hours is a suitable target for climate reconstruction. We thus present the first reconstruction of summer sunshine for the eastern Alps and compare it with the regional temperature evolution. Journal Article Climate Dynamics 43 3-4 971 980 Carbon isotopes; dendrochronology; climate change; cloud cover 31 12 2014 2014-12-31 10.1007/s00382-013-1864-z COLLEGE NANME Science and Engineering - Faculty COLLEGE CODE FGSEN Swansea University 2019-02-13T17:41:59.8227645 2015-10-26T13:57:06.1860995 Faculty of Science and Engineering School of Biosciences, Geography and Physics - Geography Polona Hafner 1 Danny McCarroll 2 Iain Robertson 0000-0001-7174-4523 3 Neil Loader 0000-0002-6841-1813 4 Mary Gagen 0000-0002-6820-6457 5 Giles Young 6 Roderick J. Bale 7 Eloni Sonninen 8 Tom Levanič 9 0023984-11052017124313.pdf Hafneretal150513.pdf 2017-05-11T12:43:13.5600000 Output 618516 application/pdf Accepted Manuscript true 2017-05-11T00:00:00.0000000 true eng |
title |
A 520 year record of summer sunshine for the eastern European Alps based on stable carbon isotopes in larch tree rings |
spellingShingle |
A 520 year record of summer sunshine for the eastern European Alps based on stable carbon isotopes in larch tree rings Danny McCarroll Iain Robertson Neil Loader Mary Gagen Giles Young |
title_short |
A 520 year record of summer sunshine for the eastern European Alps based on stable carbon isotopes in larch tree rings |
title_full |
A 520 year record of summer sunshine for the eastern European Alps based on stable carbon isotopes in larch tree rings |
title_fullStr |
A 520 year record of summer sunshine for the eastern European Alps based on stable carbon isotopes in larch tree rings |
title_full_unstemmed |
A 520 year record of summer sunshine for the eastern European Alps based on stable carbon isotopes in larch tree rings |
title_sort |
A 520 year record of summer sunshine for the eastern European Alps based on stable carbon isotopes in larch tree rings |
author_id_str_mv |
6d181d926aaac8932c2bfa8d0e7f6960 ef8912c57e0140e9ecb2a69b7e34467e 8267a62100791965d08df6a7842676e6 e677a6d0777aed90ac1eca8937e43d2b e0c807e6b9b663f1c297feecd2f54c3a |
author_id_fullname_str_mv |
6d181d926aaac8932c2bfa8d0e7f6960_***_Danny McCarroll ef8912c57e0140e9ecb2a69b7e34467e_***_Iain Robertson 8267a62100791965d08df6a7842676e6_***_Neil Loader e677a6d0777aed90ac1eca8937e43d2b_***_Mary Gagen e0c807e6b9b663f1c297feecd2f54c3a_***_Giles Young |
author |
Danny McCarroll Iain Robertson Neil Loader Mary Gagen Giles Young |
author2 |
Polona Hafner Danny McCarroll Iain Robertson Neil Loader Mary Gagen Giles Young Roderick J. Bale Eloni Sonninen Tom Levanič |
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Climate Dynamics |
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43 |
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10.1007/s00382-013-1864-z |
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description |
A 520-year stable carbon isotope chronology from tree ring cellulose in high altitude larch trees (Larix decidua Mill.), from the eastern European Alps, correlates more strongly with summer temperature than with summer sunshine hours. However, when instrumental records of temperature and sunshine diverge after AD 1980, the tree ring time series does not follow warming summer temperatures but more closely tracks summer sunshine trends. It is concluded that sunshine is the dominant control on carbon isotope fractionation in these trees, via the influence of photosynthetic rate on the internal partial pressure of CO2, and that high summer (July-August) sunshine hours is a suitable target for climate reconstruction. We thus present the first reconstruction of summer sunshine for the eastern Alps and compare it with the regional temperature evolution. |
published_date |
2014-12-31T03:28:22Z |
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1763751076741251072 |
score |
11.037581 |