Detecting instabilities in tree-ring proxy calibration

Evidence has been found for reduced sensitivity of tree growth to temperature in a number of forests at high northern latitudes and alpine locations. Furthermore, at some of these sites, emergent subpopulations of trees show negative growth trends with rising temperature. These findings are typicall...

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Main Authors: Visser, H., Buentgen, U., D'Arrigo, R., Petersen, A.C.
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2010
Subjects:
Online Access:http://eprints.lse.ac.uk/28870/
http://www.climate-of-the-past.net/home.html
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spelling ftlondoneconom:oai:eprints.lse.ac.uk:28870 2023-05-15T15:08:19+02:00 Detecting instabilities in tree-ring proxy calibration Visser, H. Buentgen, U. D'Arrigo, R. Petersen, A.C. 2010-06 http://eprints.lse.ac.uk/28870/ http://www.climate-of-the-past.net/home.html eng eng Copernicus Publications Visser, H., Buentgen, U., D'Arrigo, R. and Petersen, A.C. (2010) Detecting instabilities in tree-ring proxy calibration. Climate of the Past, 6 (3). 367 -377. ISSN 1814-9324 GE Environmental Sciences Article PeerReviewed 2010 ftlondoneconom 2022-03-02T20:13:42Z Evidence has been found for reduced sensitivity of tree growth to temperature in a number of forests at high northern latitudes and alpine locations. Furthermore, at some of these sites, emergent subpopulations of trees show negative growth trends with rising temperature. These findings are typically referred to as the 'Divergence Problem' (DP). Given the high relevance of paleoclimatic reconstructions for policy-related studies, it is important for dendrochronologists to address this issue of potential model uncertainties associated with the DP. Here we address this issue by proposing a calibration technique, termed 'stochastic response function' (SRF), which allows the presence or absence of any instabilities in growth response of trees (or any other climate proxy) to their calibration target to be visualized and detected. Since this framework estimates confidence limits and subsequently provides statistical significance tests, the approach is also very well suited for proxy screening prior to the generation of a climate-reconstruction network. Two examples of tree growth/climate relationships are provided, one from the North American Arctic treeline and the other from the upper treeline in the European Alps. Instabilities were found to be present where stabilities were reported in the literature, and vice versa, stabilities were found where instabilities were reported. We advise to apply SRFs in future proxy-screening schemes, next to the use of correlations and RE/CE statistics. It will improve the strength of reconstruction hindcasts Article in Journal/Newspaper Arctic The London School of Economics and Political Science: LSE Research Online Arctic
institution Open Polar
collection The London School of Economics and Political Science: LSE Research Online
op_collection_id ftlondoneconom
language English
topic GE Environmental Sciences
spellingShingle GE Environmental Sciences
Visser, H.
Buentgen, U.
D'Arrigo, R.
Petersen, A.C.
Detecting instabilities in tree-ring proxy calibration
topic_facet GE Environmental Sciences
description Evidence has been found for reduced sensitivity of tree growth to temperature in a number of forests at high northern latitudes and alpine locations. Furthermore, at some of these sites, emergent subpopulations of trees show negative growth trends with rising temperature. These findings are typically referred to as the 'Divergence Problem' (DP). Given the high relevance of paleoclimatic reconstructions for policy-related studies, it is important for dendrochronologists to address this issue of potential model uncertainties associated with the DP. Here we address this issue by proposing a calibration technique, termed 'stochastic response function' (SRF), which allows the presence or absence of any instabilities in growth response of trees (or any other climate proxy) to their calibration target to be visualized and detected. Since this framework estimates confidence limits and subsequently provides statistical significance tests, the approach is also very well suited for proxy screening prior to the generation of a climate-reconstruction network. Two examples of tree growth/climate relationships are provided, one from the North American Arctic treeline and the other from the upper treeline in the European Alps. Instabilities were found to be present where stabilities were reported in the literature, and vice versa, stabilities were found where instabilities were reported. We advise to apply SRFs in future proxy-screening schemes, next to the use of correlations and RE/CE statistics. It will improve the strength of reconstruction hindcasts
format Article in Journal/Newspaper
author Visser, H.
Buentgen, U.
D'Arrigo, R.
Petersen, A.C.
author_facet Visser, H.
Buentgen, U.
D'Arrigo, R.
Petersen, A.C.
author_sort Visser, H.
title Detecting instabilities in tree-ring proxy calibration
title_short Detecting instabilities in tree-ring proxy calibration
title_full Detecting instabilities in tree-ring proxy calibration
title_fullStr Detecting instabilities in tree-ring proxy calibration
title_full_unstemmed Detecting instabilities in tree-ring proxy calibration
title_sort detecting instabilities in tree-ring proxy calibration
publisher Copernicus Publications
publishDate 2010
url http://eprints.lse.ac.uk/28870/
http://www.climate-of-the-past.net/home.html
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_relation Visser, H., Buentgen, U., D'Arrigo, R. and Petersen, A.C. (2010) Detecting instabilities in tree-ring proxy calibration. Climate of the Past, 6 (3). 367 -377. ISSN 1814-9324
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