Articles | Volume 13, issue 11
https://doi.org/10.5194/cp-13-1515-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-13-1515-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Modelling tree ring cellulose δ18O variations in two temperature-sensitive tree species from North and South America
Aliénor Lavergne
CORRESPONDING AUTHOR
Aix Marseille Université, CNRS, IRD, Collège de France,
CEREGE, ECCOREV, Aix-en-Provence, France
now at: Imperial College London, Department of Life Sciences, Silwood Park Campus, Buckhurst Road, Ascot SL5 7PY, UK
Fabio Gennaretti
CORRESPONDING AUTHOR
Aix Marseille Université, CNRS, IRD, Collège de France,
CEREGE, ECCOREV, Aix-en-Provence, France
now at: INRA Centre Grand Est – Nancy, UMR1137 Ecologie et Ecophysiologie Forestières, Champenoux, 54280, France
Camille Risi
Laboratoirede Météorologie Dynamique, IPSL, UPMC, CNRS, Paris,
France
Valérie Daux
Laboratoire des Sciences du Climat et de l'Environnement, CEA-CNRS-UVSQ,
91191 Gif-sur-Yvette, France
Etienne Boucher
Department of Geography and GEOTOP, Université du Québec à
Montréal, Montréal, Canada
Martine M. Savard
Geological Survey of Canada, Natural Resources Canada, 490 rue de la
Couronne, QC, G1K9A9, Canada
Maud Naulier
Institut de Radioprotection et de Sureté Nucléaire (IRSN),
PRP-ENV, SERIS/LRTE, Saint-Paul-lez-Durance, France
Ricardo Villalba
Instituto Argentino de Nivología, Glaciología y Ciencias
Ambientales, IANIGLA-CONICET, Mendoza, Argentina
Christian Bégin
Geological Survey of Canada, Natural Resources Canada, 490 rue de la
Couronne, QC, G1K9A9, Canada
Joël Guiot
Aix Marseille Université, CNRS, IRD, Collège de France,
CEREGE, ECCOREV, Aix-en-Provence, France
Related authors
Ignacio Hermoso de Mendoza, Etienne Boucher, Fabio Gennaretti, Aliénor Lavergne, Robert Field, and Laia Andreu-Hayles
Geosci. Model Dev., 15, 1931–1952, https://doi.org/10.5194/gmd-15-1931-2022, https://doi.org/10.5194/gmd-15-1931-2022, 2022
Short summary
Short summary
We modify the numerical model of forest growth MAIDENiso by explicitly simulating snow. This allows us to use the model in boreal environments, where snow is dominant. We tested the performance of the model before and after adding snow, using it at two Canadian sites to simulate tree-ring isotopes and comparing with local observations. We found that modelling snow improves significantly the simulation of the hydrological cycle, the plausibility of the model and the simulated isotopes.
Di Wang, Camille Risi, Lide Tian, Di Yang, Gabriel Bowen, Siteng Fan, Yang Su, Hongxi Pang, and Laurent Li
Atmos. Meas. Tech. Discuss., https://doi.org/10.5194/amt-2024-151, https://doi.org/10.5194/amt-2024-151, 2024
Preprint under review for AMT
Short summary
Short summary
We developed and validated a theoretical model for water vapor diffusion through sampling bags. This model accurately reconstructs the initial isotopic composition of the vapor samples. When applied to upper troposphere samples, the corrected data aligned closely with IASI satellite observations, enhancing the accuracy of drone-based measurements.
Mohamed Ayache, Jean-Claude Dutay, Anne Mouchet, Kazuyo Tachikawa, Camille Risi, and Gilles Ramstein
Geosci. Model Dev., 17, 6627–6655, https://doi.org/10.5194/gmd-17-6627-2024, https://doi.org/10.5194/gmd-17-6627-2024, 2024
Short summary
Short summary
Water isotopes (δ18O, δD) are one of the most widely used proxies in ocean climate research. Previous studies using water isotope observations and modelling have highlighted the importance of understanding spatial and temporal isotopic variability for a quantitative interpretation of these tracers. Here we present the first results of a high-resolution regional dynamical model (at 1/12° horizontal resolution) developed for the Mediterranean Sea, one of the hotspots of ongoing climate change.
Jérôme Lopez-Saez, Christophe Corona, Lenka Slamova, Matthias Huss, Valérie Daux, Kurt Nicolussi, and Markus Stoffel
Clim. Past, 20, 1251–1267, https://doi.org/10.5194/cp-20-1251-2024, https://doi.org/10.5194/cp-20-1251-2024, 2024
Short summary
Short summary
Glaciers in the European Alps have been retreating since the 1850s. Monitoring glacier mass balance is vital for understanding global changes, but only a few glaciers have long-term data. This study aims to reconstruct the mass balance of the Silvretta Glacier in the Swiss Alps using stable isotopes and tree ring proxies. Results indicate increased glacier mass until the 19th century, followed by a sharp decline after the Little Ice Age with accelerated losses due to anthropogenic warming.
Joel Guiot, Nicolas Bernigaud, Alberte Bondeau, Laurent Bouby, and Wolfgang Cramer
Clim. Past, 19, 1219–1244, https://doi.org/10.5194/cp-19-1219-2023, https://doi.org/10.5194/cp-19-1219-2023, 2023
Short summary
Short summary
In the Mediterranean the vine has been an important part of the economy since Roman times. Viticulture expanded within Gaul during warmer climate phases and regressed during cold periods. Now it is spreading strongly to northern Europe and suffering from drought in North Africa, Spain, and southern Italy. This will worsen if global warming exceeds 2 °C above the preindustrial period. While the driver of this is increased greenhouse gases, we show that the main past forcing was volcanic activity.
Di Wang, Lide Tian, Camille Risi, Xuejie Wang, Jiangpeng Cui, Gabriel J. Bowen, Kei Yoshimura, Zhongwang Wei, and Laurent Z. X. Li
Atmos. Chem. Phys., 23, 3409–3433, https://doi.org/10.5194/acp-23-3409-2023, https://doi.org/10.5194/acp-23-3409-2023, 2023
Short summary
Short summary
To better understand the spatial and temporal distribution of vapor isotopes, we present two vehicle-based spatially continuous snapshots of the near-surface vapor isotopes in China during the pre-monsoon and monsoon periods. These observations are explained well by different moisture sources and processes along the air mass trajectories. Our results suggest that proxy records need to be interpreted in the context of regional systems and sources of moisture.
Mariano S. Morales, Doris B. Crispín-DelaCruz, Claudio Álvarez, Duncan A. Christie, M. Eugenia Ferrero, Laia Andreu-Hayles, Ricardo Villalba, Anthony Guerra, Ginette Ticse-Otarola, Ernesto C. Rodríguez-Ramírez, Rosmery LLocclla-Martínez, Joali Sanchez-Ferrer, and Edilson J. Requena-Rojas
Clim. Past, 19, 457–476, https://doi.org/10.5194/cp-19-457-2023, https://doi.org/10.5194/cp-19-457-2023, 2023
Short summary
Short summary
In this study, we develop the first tree-ring-based precipitation reconstruction for the northern South American Altiplano back to 1625 CE. We established that the occurrence rate of extreme dry events together with a shift in mean dry conditions for the late 20th–beginning of the 21st century is unprecedented in the past 389 years, consistent with other paleoclimatic records. Our reconstruction provides valuable information about El Niño–Southern Oscillation influences on local precipitation.
Jeanne Rezsöhazy, Quentin Dalaiden, François Klein, Hugues Goosse, and Joël Guiot
Clim. Past, 18, 2093–2115, https://doi.org/10.5194/cp-18-2093-2022, https://doi.org/10.5194/cp-18-2093-2022, 2022
Short summary
Short summary
Using statistical tree-growth proxy system models in the data assimilation framework may have limitations. In this study, we successfully incorporate the process-based dendroclimatic model MAIDEN into a data assimilation procedure to robustly compare the outputs of an Earth system model with tree-ring width observations. Important steps are made to demonstrate that using MAIDEN as a proxy system model is a promising way to improve large-scale climate reconstructions with data assimilation.
Jiacheng Chen, Jie Chen, Xunchang John Zhang, Peiyi Peng, and Camille Risi
Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2021-460, https://doi.org/10.5194/essd-2021-460, 2022
Manuscript not accepted for further review
Short summary
Short summary
To make full use of the advantages of isotope observations and simulations, this study generates a new dataset by integrating multi-GCM data based on data fusion and bias correction methods. This dataset contains monthly δ18Op over mainland China for the 1870–2017 period with a spatial resolution of 50–60 km. The built isoscape shows similar spatial and temporal distribution characteristics to observations, which is reliable and useful to extend the time and space of observations in China.
Ignacio Hermoso de Mendoza, Etienne Boucher, Fabio Gennaretti, Aliénor Lavergne, Robert Field, and Laia Andreu-Hayles
Geosci. Model Dev., 15, 1931–1952, https://doi.org/10.5194/gmd-15-1931-2022, https://doi.org/10.5194/gmd-15-1931-2022, 2022
Short summary
Short summary
We modify the numerical model of forest growth MAIDENiso by explicitly simulating snow. This allows us to use the model in boreal environments, where snow is dominant. We tested the performance of the model before and after adding snow, using it at two Canadian sites to simulate tree-ring isotopes and comparing with local observations. We found that modelling snow improves significantly the simulation of the hydrological cycle, the plausibility of the model and the simulated isotopes.
Jonathan Barichivich, Philippe Peylin, Thomas Launois, Valerie Daux, Camille Risi, Jina Jeong, and Sebastiaan Luyssaert
Biogeosciences, 18, 3781–3803, https://doi.org/10.5194/bg-18-3781-2021, https://doi.org/10.5194/bg-18-3781-2021, 2021
Short summary
Short summary
The width and the chemical signals of tree rings have the potential to test and improve the physiological responses simulated by global land surface models, which are at the core of future climate projections. Here, we demonstrate the novel use of tree-ring width and carbon and oxygen stable isotopes to evaluate the representation of tree growth and physiology in a global land surface model at temporal scales beyond experimentation and direct observation.
Feng Wang, Dominique Arseneault, Étienne Boucher, Shulong Yu, Steeven Ouellet, Gwenaëlle Chaillou, Ann Delwaide, and Lily Wang
Biogeosciences, 17, 4559–4570, https://doi.org/10.5194/bg-17-4559-2020, https://doi.org/10.5194/bg-17-4559-2020, 2020
Short summary
Short summary
Wood stain is challenging the use of the blue intensity technique for dendroclimatic reconstructions. Using stained subfossil trees from eastern Canadian lakes, we compared chemical destaining approaches with the
delta bluemathematical correction of blue intensity data. Although no chemical treatment was completely efficient, the delta blue method is unaffected by the staining problem and thus is promising for climate reconstructions based on lake subfossil material.
Martine M. Savard and Valérie Daux
Clim. Past, 16, 1223–1243, https://doi.org/10.5194/cp-16-1223-2020, https://doi.org/10.5194/cp-16-1223-2020, 2020
Short summary
Short summary
Climatic reconstructions based on tree-ring isotopic series convey key information on past conditions prevailing in forested regions. However, in some cases, the relations between isotopes and climate appear unstable over time, generating isotopic divergences. Former reviews have thoroughly discussed the divergence concept for tree-ring width but not for isotopes. Here we present a synopsis of the isotopic divergence problem and suggest collaborative work for improving climatic reconstructions.
Jeanne Rezsöhazy, Hugues Goosse, Joël Guiot, Fabio Gennaretti, Etienne Boucher, Frédéric André, and Mathieu Jonard
Clim. Past, 16, 1043–1059, https://doi.org/10.5194/cp-16-1043-2020, https://doi.org/10.5194/cp-16-1043-2020, 2020
Short summary
Short summary
Tree rings are the main data source for climate reconstructions over the last millennium. Statistical tree-growth models have limitations that process-based models could overcome. Here, we investigate the possibility of using a process-based ecophysiological model (MAIDEN) as a complex proxy system model for palaeoclimate applications. We show its ability to simulate tree-growth index time series that can fit robustly tree-ring width observations under certain conditions.
Camille Risi, Joseph Galewsky, Gilles Reverdin, and Florent Brient
Atmos. Chem. Phys., 19, 12235–12260, https://doi.org/10.5194/acp-19-12235-2019, https://doi.org/10.5194/acp-19-12235-2019, 2019
Short summary
Short summary
Water molecules can be light (one oxygen atom and two hydrogen atoms) or heavy (one hydrogen atom is replaced by a deuterium atom). These different molecules are called water isotopes. The isotopic composition of water vapor can potentially provide information about physical processes along the water cycle, but the factors controlling it are complex. As a first step, we propose an equation to predict the water vapor isotopic composition near the surface of tropical oceans.
David Kaniewski, Nick Marriner, Rachid Cheddadi, Joël Guiot, and Elise Van Campo
Clim. Past, 14, 1529–1542, https://doi.org/10.5194/cp-14-1529-2018, https://doi.org/10.5194/cp-14-1529-2018, 2018
Short summary
Short summary
Studies have long suggested that a protracted drought phase, termed the 4.2 ka BP event, directly impacted subsistence systems (dry farming agro-production, pastoral nomadism, and fishing) and outlying nomad habitats, forcing rain-fed cereal agriculturalists into habitat-tracking when agro-innovations were not available. Here, we focus on this crucial period to examine whether drought was active in the eastern Mediterranean Old World, especially in the Levant.
Martine M. Savard, Amanda S. Cole, Robert Vet, and Anna Smirnoff
Atmos. Chem. Phys., 18, 10373–10389, https://doi.org/10.5194/acp-18-10373-2018, https://doi.org/10.5194/acp-18-10373-2018, 2018
Short summary
Short summary
Improving air quality requires understanding of the atmospheric processes transforming nitrous oxides emitted by human activities into nitrates, an N form that may degrade natural ecosystems. Isotopes (∆17O, δ18O) are characterized in separate wet, particulate and gaseous nitrates for the first time. The gas ranges are distinct from those of the other nitrates, and the plume dynamics emerge as crucial in interpreting the results, which unravel key processes behind the distribution of nitrates.
Fabio Gennaretti, Guillermo Gea-Izquierdo, Etienne Boucher, Frank Berninger, Dominique Arseneault, and Joel Guiot
Biogeosciences, 14, 4851–4866, https://doi.org/10.5194/bg-14-4851-2017, https://doi.org/10.5194/bg-14-4851-2017, 2017
Short summary
Short summary
A model–data fusion approach is used to study how boreal forests assimilate and allocate carbon depending on weather/climate conditions. First, we adapted the MAIDEN ecophysiological forest model to consider important processes for boreal tree species. We tested the modifications on black spruce gross primary production and ring width data. We show that MAIDEN is a powerful tool for understanding how environmental factors interact with tree ecophysiology to influence boreal forest carbon fluxes.
Jean-Lionel Lacour, Cyrille Flamant, Camille Risi, Cathy Clerbaux, and Pierre-François Coheur
Atmos. Chem. Phys., 17, 9645–9663, https://doi.org/10.5194/acp-17-9645-2017, https://doi.org/10.5194/acp-17-9645-2017, 2017
Short summary
Short summary
We present temporal and spatial δD distributions derived from IASI obtained above the North Atlantic in the vicinity of West Africa. We show that the seasonality of δD in the North Atlantic is closely associated with the influence of the Saharan heat low (SHL). We provide an interpretation of the temporal and spatial variations in δD and show that the interactions between the large-scale subsidence, the ITCZ, and the SHL can be disentangled thanks to the added information contained in δD.
Alexandre Cauquoin and Camille Risi
Geosci. Model Dev. Discuss., https://doi.org/10.5194/gmd-2017-178, https://doi.org/10.5194/gmd-2017-178, 2017
Revised manuscript not accepted
Short summary
Short summary
AGCMs are known to have a warm and isotopically enriched bias over Antarctica. We test here the hypothesis that these biases are consequences of a too diffusive advection. We show here that a good representation of the advection, especially on the horizontal, is very important to reduce the bias in the isotopic contents of precipitation above this area and to improve the modelled water isotopes – temperature relationship, essential when using GCMs for paleoclimate applications.
Nesibe Köse, H. Tuncay Güner, Grant L. Harley, and Joel Guiot
Clim. Past, 13, 1–15, https://doi.org/10.5194/cp-13-1-2017, https://doi.org/10.5194/cp-13-1-2017, 2017
Timothé Bolliet, Patrick Brockmann, Valérie Masson-Delmotte, Franck Bassinot, Valérie Daux, Dominique Genty, Amaelle Landais, Marlène Lavrieux, Elisabeth Michel, Pablo Ortega, Camille Risi, Didier M. Roche, Françoise Vimeux, and Claire Waelbroeck
Clim. Past, 12, 1693–1719, https://doi.org/10.5194/cp-12-1693-2016, https://doi.org/10.5194/cp-12-1693-2016, 2016
Short summary
Short summary
This paper presents a new database of past climate proxies which aims to facilitate the distribution of data by using a user-friendly interface. Available data from the last 40 years are often fragmented, with lots of different formats, and online libraries are sometimes nonintuitive. We thus built a new dynamic web portal for data browsing, visualizing, and batch downloading of hundreds of datasets presenting a homogeneous format.
Inga Labuhn, Valérie Daux, Olivier Girardclos, Michel Stievenard, Monique Pierre, and Valérie Masson-Delmotte
Clim. Past, 12, 1101–1117, https://doi.org/10.5194/cp-12-1101-2016, https://doi.org/10.5194/cp-12-1101-2016, 2016
Short summary
Short summary
This article presents a reconstruction of summer droughts in France for the last 680 years, based on oxygen isotope ratios in tree ring cellulose from living trees and building timbers at two sites, Fontainebleau and Angoulême. Both sites show coherent drought patterns during the 19th and 20th century, and are characterized by increasing drought in recent decades. A decoupling between sites points to a more heterogeneous climate in France during earlier centuries.
M. Naulier, M. M. Savard, C. Bégin, F. Gennaretti, D. Arseneault, J. Marion, A. Nicault, and Y. Bégin
Clim. Past, 11, 1153–1164, https://doi.org/10.5194/cp-11-1153-2015, https://doi.org/10.5194/cp-11-1153-2015, 2015
Short summary
Short summary
This paper presents a millennial δ18O series and the reconstruction of the maximal temperature. The maximal replication and annual resolution have been obtained by using cohort sampling method. Three contrasted climatic periods have been identified: the medieval warm period (~997-1250; the warmest), the little ice age (~1450-1880) and the modern period (1970-2000) that is one of the fastest warming over the last millennium.
M. S. Morales, J. Carilla, H. R. Grau, and R. Villalba
Clim. Past, 11, 1139–1152, https://doi.org/10.5194/cp-11-1139-2015, https://doi.org/10.5194/cp-11-1139-2015, 2015
Short summary
Short summary
A 601-year lake area reconstruction in NW Argentina and SW Bolivia, characterized the occurrence of annual to multi-decadal lake area fluctuations and its main oscillation modes of variability. Our reconstruction points out that the late 20th century decrease in lake area was exceptional over the period 1407–2007. A persistent negative trend in lake area is clear in the reconstruction and consistent with glacier retreat and other climate proxies from the Altiplano and the tropical Andes.
G. Gea-Izquierdo, F. Guibal, R. Joffre, J. M. Ourcival, G. Simioni, and J. Guiot
Biogeosciences, 12, 3695–3712, https://doi.org/10.5194/bg-12-3695-2015, https://doi.org/10.5194/bg-12-3695-2015, 2015
Short summary
Short summary
We developed a process-based model for evergreen Mediterranean forests. We used multiproxy data including eddy covariance CO2 flux and annual growth dendrochronological time series. The model explicitly takes into account the influence of climatic variability to calculate photosynthesis and carbon allocation. We analyzed long-time acclimation processes and climatic trade-offs between the C-source and the C-sink. There is much potentiality to apply the model at a larger scale.
É. Boucher, J. Guiot, C. Hatté, V. Daux, P.-A. Danis, and P. Dussouillez
Biogeosciences, 11, 3245–3258, https://doi.org/10.5194/bg-11-3245-2014, https://doi.org/10.5194/bg-11-3245-2014, 2014
C. Risi, A. Landais, R. Winkler, and F. Vimeux
Clim. Past, 9, 2173–2193, https://doi.org/10.5194/cp-9-2173-2013, https://doi.org/10.5194/cp-9-2173-2013, 2013
M. Casado, P. Ortega, V. Masson-Delmotte, C. Risi, D. Swingedouw, V. Daux, D. Genty, F. Maignan, O. Solomina, B. Vinther, N. Viovy, and P. Yiou
Clim. Past, 9, 871–886, https://doi.org/10.5194/cp-9-871-2013, https://doi.org/10.5194/cp-9-871-2013, 2013
P. G. C. Amaral, A. Vincens, J. Guiot, G. Buchet, P. Deschamps, J.-C. Doumnang, and F. Sylvestre
Clim. Past, 9, 223–241, https://doi.org/10.5194/cp-9-223-2013, https://doi.org/10.5194/cp-9-223-2013, 2013
Related subject area
Subject: Proxy Use-Development-Validation | Archive: Terrestrial Archives | Timescale: Instrumental Period
Cryogenic cave minerals recorded the 1889 CE melt event in northeastern Greenland
Ring-width and blue-light chronologies of Podocarpus lawrencei from southeastern mainland Australia reveal a regional climate signal
Climate signals in stable carbon and hydrogen isotopes of lignin methoxy groups from southern German beech trees
Seasonal climate signals preserved in biochemical varves: insights from novel high-resolution sediment scanning techniques
Reconstructing paleoclimate fields using online data assimilation with a linear inverse model
Stable isotopes in caves over altitudinal gradients: fractionation behaviour and inferences for speleothem sensitivity to climate change
Anika Donner, Paul Töchterle, Christoph Spötl, Irka Hajdas, Xianglei Li, R. Lawrence Edwards, and Gina E. Moseley
Clim. Past, 19, 1607–1621, https://doi.org/10.5194/cp-19-1607-2023, https://doi.org/10.5194/cp-19-1607-2023, 2023
Short summary
Short summary
This study investigates the first finding of fine-grained cryogenic cave minerals in Greenland, a type of speleothem that has been notably difficult to date. We present a successful approach for determining the age of these minerals using 230Th / U disequilibrium and 14C dating. We relate the formation of the cryogenic cave minerals to a well-documented extreme weather event in 1889 CE. Additionally, we provide a detailed report on the mineralogical and isotopic composition of these minerals.
Jacinda A. O'Connor, Benjamin J. Henley, Matthew T. Brookhouse, and Kathryn J. Allen
Clim. Past, 18, 2567–2581, https://doi.org/10.5194/cp-18-2567-2022, https://doi.org/10.5194/cp-18-2567-2022, 2022
Short summary
Short summary
Tree-ring records provide a unique window into past climate variability. However, there are few such records from the Australian mainland. We present results from nine cross-sections of an alpine tree species from the Victorian Alps from 1929–1998. The tree-ring widths have significant correlations with winter temperature, precipitation and snow depth. The intensity of reflected blue light from the wood surface shows a strong response to growing season temperature and winter precipitation.
Anna Wieland, Markus Greule, Philipp Roemer, Jan Esper, and Frank Keppler
Clim. Past, 18, 1849–1866, https://doi.org/10.5194/cp-18-1849-2022, https://doi.org/10.5194/cp-18-1849-2022, 2022
Short summary
Short summary
We examined annually resolved stable carbon and hydrogen isotope ratios of wood lignin methoxy groups of beech trees growing in temperate, low elevation environments. Here, carbon isotope ratios reveal highest correlations with regional summer temperatures while hydrogen isotope ratios correlate more strongly with large-scale temperature changes. By combining the dual isotope ratios of wood lignin methoxy groups, a proxy for regional- to subcontinental-scale temperature patterns can be applied.
Paul D. Zander, Maurycy Żarczyński, Wojciech Tylmann, Shauna-kay Rainford, and Martin Grosjean
Clim. Past, 17, 2055–2071, https://doi.org/10.5194/cp-17-2055-2021, https://doi.org/10.5194/cp-17-2055-2021, 2021
Short summary
Short summary
High-resolution geochemical imaging techniques provide new opportunities to investigate the biogeochemical composition of sediments at micrometer scale. Here, we compare biogeochemical data from biochemical varves with meteorological data to understand how seasonal meteorological variations are recorded in varve composition. We find that these scanning techniques help to clarify climate–proxy relationships in biochemical varves and show great potential for high-resolution climate reconstruction.
Walter A. Perkins and Gregory J. Hakim
Clim. Past, 13, 421–436, https://doi.org/10.5194/cp-13-421-2017, https://doi.org/10.5194/cp-13-421-2017, 2017
Short summary
Short summary
We examine the skill of a novel data assimilation approach to paleoclimate reconstruction that uses linear climate model forecasts. Many reconstruction studies forego the use of forecasts from climate models due to their high computational expense and relatively low skill. We show that the use of simpler linear models can improve reconstruction skill for both global mean temperature and spatial fields. Improvements displayed seem to be related to dynamical constraints from the forecasts.
V. E. Johnston, A. Borsato, C. Spötl, S. Frisia, and R. Miorandi
Clim. Past, 9, 99–118, https://doi.org/10.5194/cp-9-99-2013, https://doi.org/10.5194/cp-9-99-2013, 2013
Cited articles
Baldocchi, D. D., Ma, S., Rambal, S., Misson, L., Ourcival, J. M., Limousin, J. M., Pereira, J., and Papale, D.: On the differential advantages of evergreenness and deciduousness in mediterranean oak woodlands: A flux perspective, Ecol. Appl., 20, 1583–1597, https://doi.org/10.1890/08-2047.1, 2010.
Barbour, M. M.: Stable oxygen isotope composition of plant tissue: a review, Funct. Plant Biol., 34, 83–94, https://doi.org/10.1071/FP06228, 2007.
Barbour, M. M., Cernusak, L. A., and Farquhar, G. D.: Factors affecting the oxygen isotope ratio of plant organic material, in: Stable isotopes and biosphere-atmosphere interactions: Processes and Biological Controls, edited by: Flanagan, L. B., Ehleringer, J. R., and Pataki, D. E., Elsevier, Amsterdam, 9–28, 2005.
Boucher, É., Guiot, J., Hatté, C., Daux, V., Danis, P.-A., and Dussouillez, P.: An inverse modeling approach for tree-ring-based climate reconstructions under changing atmospheric CO2 concentrations, Biogeosciences, 11, 3245–3258, https://doi.org/10.5194/bg-11-3245-2014, 2014.
Brienen, R. J. W., Helle, G., Pons, T. L., Guyot, J.-L., and Gloor, M.: Oxygen isotopes in tree rings are a good proxy for Amazon precipitation and El Niño-Southern Oscillation variability, Proc. Natl. Acad. Sci. USA, 109, 16957–16962, https://doi.org/10.1073/pnas.1205977109, 2012.
Buhay, W. M., Edwards, T. W. D., and Aravena, R.: Evaluating kinetic fractionation factors used for reconstructions from oxgen and hydrogen isotope ratios in plant water and cellulose, Geochem. Geophy. Geosy., 60, 2209–2218, 1996.
Cernusak, L. A. and English, N. B.: Beyond tree-ring widths: stable isotopes sharpen the focus on climate responses of temperate forest trees, Tree Physiol., 35, 1–3, https://doi.org/10.1093/treephys/tpu115, 2015.
Compo, G. P., Whitaker, J. S., Sardeshmukh, P. D., Matsui, N., Allan, R. J., Yin, X., Gleason, B. E., Vose, R. S., Rutledge, G., Bessemoulin, P., BroNnimann, S., Brunet, M., Crouthamel, R. I., Grant, A. N., Groisman, P. Y., Jones, P. D., Kruk, M. C., Kruger, A. C., Marshall, G. J., Maugeri, M., Mok, H. Y., Nordli, O., Ross, T. F., Trigo, R. M., Wang, X. L., Woodruff, S. D., and Worley, S. J.: The twentieth century reanalysis project, Q. J. Roy Meteor. Soc., 137, 1–28, https://doi.org/10.1002/qj.776, 2011.
Craig, H. and Gordon, L. I.: Deuterium and oxygen 18 variations in the ocean and the marine atmosphere, Spoleto, 1965.
Danis, P. A., Hatté, C., Misson, L. and Guiot, J.: MAIDENiso: a multiproxy biophysical model of tree-ring width and oxygen and carbon isotopes, Can. J. Forest Res., 42, 1697–1713, https://doi.org/10.1139/x2012-089, 2012.
Danis, P. A., Masson-Delmotte, V., Stievenard, M., Guillemin, M. T., Daux, V., Naveau, P., and von Grafenstein, U.: Reconstruction of past precipitation δ18O using tree-ring cellulose δ18O and δ13C: A calibration study near Lac d'Annecy, France, Earth Planet. Sc. Lett., 243, 439–448, https://doi.org/10.1016/j.epsl.2006.01.023, 2006.
Dansgaard, W.: Stable isotopes in precipitation, Tellus A, 16, 436–468, https://doi.org/10.3402/tellusa.v16i4.8993, 1964.
DeNiro, M. J. and Epstein, S.: Relationship between the oxygen isotope ratios of terrestrial plant cellulose, carbon dioside, and water, Science, 204, 51–53, 1979.
DeNiro, M. J. and Epstein, S.: Isotopic composition of cellulose from aquatic organisms, Geochim. Cosmochim. Ac., 45, 1885–1894, https://doi.org/10.1016/0016-7037(81)90018-1, 1981.
Donoso, C.: Tipos forestales de los bosques nativos de Chile., Documento de Trabajo Nu. 38, Investigación y Desarrollo Forestal (CONAF, PNUD-FAO), FAO Chile, 1981.
ESRL-NOAA: 20th Century Reanalysis V2c, https://www.esrl.noaa.gov/psd/data/gridded/data.20thC_ReanV2c.html, last access: March 2017.
ESRL-NOAA: Mauna Loa data, http://www.esrl.noaa.gov/gmd/ccgg/trends/, last access: March 2017.
Farquhar, G. D., Hubick, H. T., Condon, A. G., and Richards, R. A.: Carbon isotope fractionation and plant water-use efficiency, in: Stable isotopes in ecological research, 21–40, 1989.
Farquhar, G. D., Barbour, M. M., and Henry, B. K.: Interpretation of oxygen isotope composition of leaf material, in Stable isotopes: integration of biological, ecological and geochemical processes, BIOS Scientific Publishers, Oxford, 27–61, 1998.
Gea-Izquierdo, G., Guibal, F., Joffre, R., Ourcival, J. M., Simioni, G., and Guiot, J.: Modelling the climatic drivers determining photosynthesis and carbon allocation in evergreen Mediterranean forests using multiproxy long time series, Biogeosciences, 12, 3695–3712, https://doi.org/10.5194/bg-12-3695-2015, 2015.
Gennaretti, F., Arseneault, D., Nicault, A., Perreault, L., and Bégin, Y.: Volcano-induced regime shifts in millennial tree-ring chronologies from northeastern North America, Proc. Natl. Acad. Sci. USA, 111, 10077–10082, https://doi.org/10.1073/pnas.1324220111, 2014.
Gennaretti, F., Gea-Izquierdo, G., Boucher, E., Berninger, F., Arseneault, D., and Guiot, J.: Ecophysiological modeling of photosynthesis and carbon allocation to the tree stem in the boreal forest, Biogeosciences, 14, 4851–4866, https://doi.org/10.5194/bg-14-4851-2017, 2017a.
Gennaretti, F., Huard, D., Naulier, M., Savard, M., Bégin, C., Arseneault, D., and Guiot, J.: Bayesian multiproxy temperature reconstruction with black spruce ring widths and stable isotopes from the northern Quebec taiga, Clim. Dynam., 1–13, https://doi.org/10.1007/s00382-017-3565-5, 2017b.
Gessler, A., Ferrio, J. P., Hommel, R., Treydte, K., Werner, R. A., and Monson, R. K.: Stable isotopes in tree rings: towards a mechanistic understanding of isotope fractionation and mixing processes from the leaves to the wood, Tree Physiol., 1–23, 2014.
Guiot, J., Boucher, E., and Gea-Izquierdo, G.: Process models and model-data fusion in dendroecology, Front. Ecol. Evol., 2, 1–12, https://doi.org/10.3389/fevo.2014.00052, 2014.
Hartl-Meier, C., Zang, C., Büntgen, U. L. F., Esper, J. A. N., Rothe, A., Göttlein, A., Dirnböck, T., and Treydte, K.: Uniform climate sensitivity in tree-ring stable isotopes across species and sites in a mid-latitude temperate forest, Tree Physiol., 2003, 4–15, https://doi.org/10.1093/treephys/tpu096, 2014.
Helliker, B. R. and Richter, S. L.: Subtropical to boreal convergence of tree-leaf temperatures, Nature, 454, 511–514, https://doi.org/10.1038/nature07031, 2008.
Horita, J. and Wesolowski, D. J.: Liquid-vapor fractionation of oxygen and hydrogen isotopes of water from the freezing to the critical temperature, Geochim. Cosmochim. Ac., 58, 3425–3437, https://doi.org/10.1016/0016-7037(94)90096-5, 1994.
Hourdin, F., Grandpeix, J. Y., Rio, C., Bony, S., Jam, A., Cheruy, F., Rochetin, N., Fairhead, L., Idelkadi, A., Musat, I., Dufresne, J. L., Lahellec, A., Lefebvre, M. P., and Roehrig, R.: LMDZ5B: The atmospheric component of the IPSL climate model with revisited parameterizations for clouds and convection, Clim. Dynam., 40, 2193–2222, https://doi.org/10.1007/s00382-012-1343-y, 2013.
Hutchinson, M. F., McKenney, D. W., Lawrence, K., Pedlar, J. H., Hopkinson, R. F., Milewska, E., and Papadopol, P.: Development and testing of Canada-wide interpolated spatial models of daily minimum-maximum temperature and precipitation for 1961–2003, J. Appl. Meteorol. Clim., 48, 725–741, https://doi.org/10.1175/2008JAMC1979.1, 2009.
Insel, N., Poulsen, C. J., Sturm, C., and Ehlers, T. A.: Climate controls on Andean precipitation δ18O interannual variability, J. Geophys. Res.-Atmos., 118, 9721–9742, https://doi.org/10.1002/jgrd.50619, 2013.
Kahmen, A., Sachse, D., Arndt, S. K., Tu, K. P., Farrington, H., Vitousek, P. M., and Dawson, T. E.: Cellulose δ18O is an index of leaf-to-air vapor pressure difference (VPD) in tropical plants., Proc. Natl. Acad. Sci. USA, 108, 1981–1986, https://doi.org/10.1073/pnas.1018906108, 2011.
Keeling, C. D., Bacastow, R. B., Bainbridge, A. E., Ekdahl Jr., C. A., Guenther, P. R., Waterman, L. S., and Chin, J. F. S.: Atmospheric carbon dioxide variations at Mauna Loa Observatory, Hawaii, Tellus A, 28, 538–551, https://doi.org/10.3402/tellusa.v28i6.11322, 1976.
Labuhn, I., Daux, V., Girardclos, O., Stievenard, M., Pierre, M., and Masson-Delmotte, V.: French summer droughts since 1326 CE: a reconstruction based on tree ring cellulose δ18O, Clim. Past, 12, 1101–1117, https://doi.org/10.5194/cp-12-1101-2016, 2016.
Lavergne, A., Daux, V., Villalba, R., and Barichivich, J.: Temporal changes in climatic limitation of tree-growth at upper treeline forests: Contrasted responses along the west-to-east humidity gradient in Northern Patagonia, Dendrochronologia, 36, 49–59, 2015.
Lavergne, A., Daux, V., Villalba, R., Pierre, M., Stievenard, M., Srur, A. M., and Vimeux, F.: Are the δ18O of F. cupressoides and N. pumilio promising proxies for climate reconstructions in northern Patagonia?, J. Geophys. Res.-Biogeo., 121, 767–776, https://doi.org/10.1002/2015JG003260, 2016.
Lavergne, A., Daux, V., Villalba, R., Pierre, M., Stievenard, M., and Srur, A. M.: Improvement of isotope-based climate reconstructions in Patagonia through a better understanding of climate influences on isotopic fractionation in tree rings, Earth Planet. Sc. Lett., 459, 372–380, https://doi.org/10.1016/j.epsl.2016.11.045, 2017
López Bernal, P., Defossé, G. E., Quinteros, C. P., and Bava, J. O.: Sustainable management of lenga (Nothofagus pumilio) forests through group selection system, in: Sustainable forest management – current research, edited by: Diez, J. J., 45–66, 2012.
Lorrey, A. M., Brookman, T. H., Evans, M. N., Fauchereau, N.C., Barbour, M., Macinnis-Ng, C. Criscitiello, A., Eischeid, G., Fowler, A. M., Horton, T. W., and Schrag, D. P.: Stable oxygen isotope signatures of early season wood in New Zealand kauri (Agathis australis) tree rings: Prospects for palaeoclimate reconstruction, Dendrochronologia, 40, 50–63, https://doi.org/10.1016/j.dendro.2016.03.012, 2016.
Magnin, A., Puntieri, J., and Villalba, R.: Interannual variations in primary and secondary growth of Nothofagus pumilio and their relationships with climate, Trees, 28, 1463–1471, 2014.
Misson, L.: MAIDEN: a model for analyzing ecosystem processes in dendroecology, Can. J. For. Res., 34, 874–887, 2004.
Natural Resources Canada: http://cfs.nrcan.gc.ca/projects/3/4, last access: February 2017.
Naulier, M., Savard, M. M., Bégin, C., Marion, J., Arseneault, D., and Bégin, Y.: Carbon and oxygen isotopes of lakeshore black spruce trees in northeastern Canada as proxies for climatic reconstruction, Chem. Geol., 374/375, 37–43, https://doi.org/10.1016/j.chemgeo.2014.02.031, 2014.
Naulier, M., Savard, M. M., Bégin, C., Gennaretti, F., Arseneault, D., Marion, J., Nicault, A., and Bégin, Y.: A millennial summer temperature reconstruction for northeastern Canada using oxygen isotopes in subfossil trees, Clim. Past, 11, 1153–1164, https://doi.org/10.5194/cp-11-1153-2015, 2015.
Noone, D. and Simmonds, I.: Associations between δ18O of water and climate parameters in a simulation of atmospheric circulation for 1979–95, J. Clim., 15, 3150–3169, 2002.
Ogée, J., Brunet, Y., Loustau, D., Berbigier, P., and Delzon, S.: MuSICA, a CO2, water and energy multilayer, multileaf pine forest model: Evaluation from hourly to yearly time scales and sensitivity analysis, Glob. Change Biol., 9, 697–717, https://doi.org/10.1046/j.1365-2486.2003.00628.x, 2003.
Ogée, J., Barbour, M. M., Wingate, L., Bert, D., Bosc, A., Stievenard, M., Lambrot, C., Pierre, M., Bariac, T., Loustau, D., and Dewar, R. C.: A single-substrate model to interpret intra-annual stable isotope signals in tree-ring cellulose, Plant, Cell Environ., 32, 1071–1090, https://doi.org/10.1111/j.1365-3040.2009.01989.x, 2009.
Rinne, K. T., Loader, N. J., Switsur, V. R., and Waterhouse, J. S.: 400-year May-August precipitation reconstruction for Southern England using oxygen isotopes in tree rings, Quaternary Sci. Rev., 60, 13–25, https://doi.org/10.1016/j.quascirev.2012.10.048, 2013.
Risi, C., Bony, S., Vimeux, F., and Jouzel, J.: Water-stable isotopes in the LMDZ4 general circulation model: Model evaluation for present-day and past climates and applications to climatic interpretations of tropical isotopic records, J. Geophys. Res.-Atmos., 115, 1–27, https://doi.org/10.1029/2009JD013255, 2010.
Roden, J. S., Lin, G., and Ehleringer, J. R.: A mechanistic model for interpretation of hydrogen and oxygen isotope ratios in tree-ring cellulose, Geochim. Cosmochim. Ac., 64, 21–35, https://doi.org/10.1016/S0016-7037(99)00195-7, 2000.
Rozanski, K. and Araguás-Araguás, L.: Spatial and temporal variability of stable isotope composition of precipitation over the South American continent, Bull. l'Institut Fr. d'eìtudes Andin., 24, 379–390, 1995.
Rozanski, K., Araguás-Araguás, L., and Gonfiantini, R.: Isotopic patterns in modern global precipitation, in: Climate change in continental isotopic records, edited by: Swart, P. K., Lohmann, K. C., McKenzie, J., and Savin, S., American Geophysical Union, 1993.
Running, S. W., Nemani, R. R., and Hungerford, R. D.: Extrapolation of synoptic meteorological data in mountainous terrain and its use for simulating forest evapotranspiration and photosynthesis, Can. J. Forest Res., 17, 472–483, https://doi.org/10.1139/x87-081, 1987.
Rusch, V. E.: Altitudinal variation in the phenology of Nothofagus pumilio in Argentina, Rev. Chil. Hist. Nat., 66, 131–141, 1993.
Saurer, M., Aellen, K., and Siegwolf, R. T. W.: Correlating δ13C and δ18O in cellulose of trees, Plant Cell Environ., 20, 1543–1550, 1997.
Saurer, M., Cherubini, P., Reynolds-Henne, C. E., Treydte, K. S., Anderson, W. T., and Siegwolf, R. T. W.: An investigation of the common signal in tree ring stable isotope chronologies at temperate sites, J. Geophys. Res.-Biogeo., 113, 1–11, https://doi.org/10.1029/2008JG000689, 2008.
Schlatter, J.: Requerimientos de sitio para la lenga, Nothofagus pumilio (Poepp. et Endl.) Krasser, Bosque, 15, 3–10, 1994.
Shi, C., Daux, V., Zhang, Q. B., Risi, C., Hou, S. G., Stievenard, M., Pierre, M., Li, Z., and Masson-Delmotte, V.: Reconstruction of southeast Tibetan Plateau summer climate using tree ring δ18O: Moisture variability over the past two centuries, Clim. Past, 8, 205–213, https://doi.org/10.5194/cp-8-205-2012, 2012.
Smith, R. B. and Evans, J. P.: Orographic precipitation and water vapor fractionation over the Southern Andes, J. Hydrometeorol., 8, 3–19, https://doi.org/10.1175/JHM555.1, 2007.
Stern, L. A. and Blisniuk, P. M.: Stable isotope composition of precipitation across the southern Patagonian Andes, J. Geophys. Res.-Atmos., 107, D234667, https://doi.org/10.1029/2002JD002509, 2002.
Sternberg, L. D. S. L.: Oxygen and hydrogen isotope ratios in plant cellulose: Mechanisms and applications, in: Stable isotopes in ecological research, edited by: Rundel, P. W., Ehleringer J. R., and Nagy K. A., 124–141, 1989.
Sternberg, L. D. S. L. and Ellsworth, P. F. V.: Divergent biochemical fractionation, not convergent temperature, explains cellulose oxygen isotope enrichment across latitudes, PLoS One, 6, e28040, https://doi.org/10.1371/journal.pone.0028040, 2011.
Sturm, C., Vimeux, F., and Krinner, G.: Intraseasonal variability in South America recorded in stable water isotopes, J. Geophys. Res.-Atmos., 112, 2156–2202, https://doi.org/10.1029/2006JD008298, 2007.
Sturm, K., Hoffmann, G., Langmann, B., and Stichler, W.: Simulation of δ18O in precipitation by the regional circulation model REMOiso, Hydrol. Process., 19, 3425–3444, https://doi.org/10.1002/hyp.5979, 2005.
SWING project: http://paos.colorado.edu/~dcn/SWING/database.php, last access: June 2017.
Treydte, K., Boda, S., Graf Pannatier, E., Fonti, P., Frank, D., Ullrich, B., Saurer, M., Siegwolf, R. T. W., Battipaglia, G., Werner, W., and Gessler, A.: Seasonal transfer of oxygen isotopes from precipitation and soil to the tree ring: Source water versus needle water enrichment, New Phytol., 202, 772–783, https://doi.org/10.1111/nph.12741, 2014.
Viereck, L. A. and Johnston, W. F.: Picea mariana (Mill.) B. S. P., in: Silvics of North America: 1. Conifers; 2. Hardwoods, edited by: Burns, R. M. and Honkala, B. H., US, Department of Agriculture, Forest Service, Washington, DC, 443–464, 1990.
Wernicke, J., Grießinger, J., Hochreuther, P., and Braüning, A.: Variability of summer humidity during the past 800 years on the eastern Tibetan Plateau inferred from δ18O of tree-ring cellulose, Clim. Past, 11, 327–337, https://doi.org/10.5194/cp-11-327-2015, 2015.
Wershaw, R. L., Friedman, I., and Heller, S. J.: Hydrogen isotope fractionation in water passing through trees, in: Advances in Organic Geochemistry, edited by: Hobson, F. and Speers, M., New York, Pergamon, 55–67, 1966.
Yakir, D. and DeNiro, M. J.: Oxygen and hydrogen isotope fractionation during cellulose metabolism in lemna gibba L., Plant Physiol., 93, 325–332, https://doi.org/10.1104/pp.93.1.325, 1990.
Short summary
Tree rings are long-term recorders of past climate variations, but the origin of the climate signals imprinted is difficult to interpret. Here, using a complex model we show that the temperature signal recorded in tree rings from two species from North and South America is likely related to processes occurring at the leaf level. This result contributes to the quantitative interpretation of these proxies for their future exploitation for millennium-scale climate reconstructions.
Tree rings are long-term recorders of past climate variations, but the origin of the climate...