What drives growth of Scots pine in continental Mediterranean climates: drought, low temperatures or both?
Autor: | Emilia Gutiérrez, Juan Carlos Linares, Andreas Rigling, Andrea Hevia, J. Julio Camarero, Mar Génova, Gabriel Sangüesa-Barreda, Raúl Sánchez-Salguero, Raquel Alfaro-Sánchez, J. Diego Galván, Jaime Madrigal-González, Ángela Sánchez-Miranda, Juan Antonio Ballesteros-Cánovas |
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Přispěvatelé: | Universitat de Barcelona |
Jazyk: | angličtina |
Rok vydání: | 2015 |
Předmět: |
Mediterranean climate
Atmospheric Science Drought stress Species distribution Sequeres Growing season Climate change Mediterranean Basin Temperatura atmosfèrica Dendroecology Latitude Atmospheric temperature Pins Clima mediterrani Precipitation Global and Planetary Change Minimum temperature biology Ecology Scots pine Forestry Pinus sylvestris biology.organism_classification Latitudinal gradient Pine Droughts Environmental science Physical geography Elevational gradient Agronomy and Crop Science |
Zdroj: | Digital.CSIC. Repositorio Institucional del CSIC instname Dipòsit Digital de la UB Universidad de Barcelona Recercat. Dipósit de la Recerca de Catalunya |
Popis: | Sánchez-Salguero, R. et al.- 37 páginas Scots pine forests subjected to continental Mediterranean climates undergo cold winter temperatures and drought stress. Recent climatic trends towards warmer and drier conditions across the Mediterranean Basin might render some of these pine populations more vulnerable to drought-induced growth decline at the Southernmost limit of the species distribution. We investigated how cold winters and dry growing seasons drive the radial growth of Scots pine subject to continental Mediterranean climates by relating growth to climate variables at local (elevational gradient) and regional (latitudinal gradient) scales. Local climate-growth relationships were quantified on different time scales (5-, 10- and 15-days) to evaluate the relative role of elevation and specific site characteristics. A negative water balance driven by high maximum temperatures in June (low-elevation sites) and July (high-elevation sites) was the major constraint on growth, particularly on a 5- to 10-day time scale. Warm nocturnal conditions in January were associated with wider rings at the high-elevation sites. At the regional scale, Scots pine growth mainly responded positively to July precipitation, with a stronger association at lower elevations and higher latitudes. January minimum temperatures showed similar patterns but played a secondary role as a driver of tree growth. The balance between positive and negative effects of summer precipitation and winter temperature on radial growth depends on elevation and latitude, with low-elevation populations being more prone to suffer drought and heat stress; whereas, high-elevation populations may be favoured by warmer winter conditions. This negative impact of summer heat and drought has increased during the past decades. This interaction between climate and site conditions and local adaptations is therefore decisive for the future performance and persistence of Scots pine populations in continental Mediterranean climates. Forecasting changes in the Scots pine range due to climate change should include this site-related information to obtain more realistic predictions, particularly in Mediterranean rear-edge areas. © 2015 Elsevier B.V. We were glad to be able to use the E-OBS dataset (EU- project ENSEMBLES) and the data providers in the ECA&D project (http://www.ecad.eu), and thank Dr. Geert Jan van Oldenborgh for his assistance with these data. We are grateful to the researchers who provided data on the International Tree-Ring Data Bank. This study was funded by the projects CoMo-ReAdapt (CGL2013-48843-C2-1-R) and FORRISK (Interreg IV B SUDOE 2007-2013). The authors thank CENEAM, Montes de Valsaín and OAPN and all participants involved in the International Tree-Ring Summer School carried out in 2012 in Valsaín (Segovia-Spain), especially to Kenza Garah, María Tabakova, Virginia Garófano-Gómez and Clara Rodriguez-Morata. R. Sánchez-Salguero is grateful for the financial support of University of Córdoba-Campus de Excelencia ceiA3 and “Fondo Europeo de Desarrollo Regional (FEDER)-Programa de Fortalecimiento de las capacidades en I + D + i de las Universidades 2014–2015, Junta de Andalucía”. We are grateful to Silvia Dingwall for the language review. This work has been carried out under the framework of the COST FP1106 network STReESS. |
Databáze: | OpenAIRE |
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