...
首页> 外文期刊>Global and planetary change >Declining pine growth in Central Spain coincides with increasing diurnal temperature range since the 1970s
【24h】

Declining pine growth in Central Spain coincides with increasing diurnal temperature range since the 1970s

机译:自1970年代以来,西班牙中部的松树生长下降与昼夜温度范围增加同时发生

获取原文
获取原文并翻译 | 示例
   

获取外文期刊封面封底 >>

       

摘要

Growing evidence suggests environmental change to be most severe across the semi-arid subtropics, with past, present and projected drying of the Mediterranean Basin posing a key multidisciplinary challenge. Consideration of a single climatic factor, however, often fails to explain spatiotemporal growth dynamics of drought-prone ecosystems. Here, we present annually resolved and absolutely dated ring width measurements of 871 Scots pines (Pinus sylvestris) from 18 individual plot sites in the Central Spanish Pinar Grande forest reserve. Although comprising tree ages from 6 to 175 years, this network correlates surprisingly well with the inverse May-July diurnal temperature range (r = 0.84; p < 0.0001_(1956-2011))- Ring width extremes were triggered by pressure anomalies of the North Atlantic Oscillation, and the long-term growth decline coincided with Iberian-wide drying since the mid-1970s. Climate model simulations not only confirm this negative trend over the last decades but also project drought to continuously increase over the 21st century. Associated ecological effects and socio-economic consequences should be considered to improve adaptation strategies of agricultural and forest management as well as biodiversity conservation and ecosystem service.
机译:越来越多的证据表明,在半干旱亚热带地区,环境变化最为严重,地中海盆地的过去,现在和预计的干旱构成了关键的多学科挑战。然而,考虑单一气候因素常常无法解释干旱多发的生态系统的时空增长动态。在这里,我们介绍了西班牙中部Pinar Grande森林保护区中18个样地的871个苏格兰松树(Pinus sylvestris)的年分辨和绝对日期的环宽测量结果。尽管包含6至175年的树龄,但该网络与5月至7月的反日温度范围(r = 0.84; p <0.0001_(1956-2011))令人惊讶地具有良好的相关性。自1970年代中期以来,北大西洋涛动和长期增长下降与伊比利亚全境干旱同时发生。气候模型模拟不仅证实了过去几十年来的这种负面趋势,而且还预测干旱将在21世纪持续增加。应考虑相关的生态影响和社会经济后果,以改善农业和森林管理以及生物多样性保护和生态系统服务的适应战略。

著录项

  • 来源
    《Global and planetary change》 |2013年第8期|177-185|共9页
  • 作者单位

    Swiss Federal Research Institute for Forest Snow and Landscape (WSL), 8903 Birmensdorf, Switzerland ,Oeschger Centre for Climate Change Research (OCCR), University of Bern, 3012 Bern, Switzerland ,CzechGlobe - Global Change Research Centre AS CR, 60300 Brno, Czech Republic;

    Research Unit of Forestry Mycology and Trufficulture, Cesefor Foundation, 42005 Soria, Spain;

    Research Unit of Forestry Mycology and Trufficulture, Cesefor Foundation, 42005 Soria, Spain;

    Swiss Federal Research Institute for Forest Snow and Landscape (WSL), 8903 Birmensdorf, Switzerland;

    Institute for Atmospheric and Climate Science, ETH Zurich, 8092 Zurich, Switzerland;

    ARAID-Instituto Pirenaico de Ecologia CSIC, Avda. Montanana 1005, 50080 Zaragoza, Spain ,Dept. of Ecology, University de Barcelona, Avda. Diagonal 645,08028 Barcelona, Spain;

    National Drought Mitigation Centre, University of Nebraska-Lincoln, 68583-0988 Lincoln, USA ,CzechGlobe - Global Change Research Centre AS CR, 60300 Brno, Czech Republic;

    Swiss Federal Research Institute for Forest Snow and Landscape (WSL), 8903 Birmensdorf, Switzerland;

    Swiss Federal Research Institute for Forest Snow and Landscape (WSL), 8903 Birmensdorf, Switzerland;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    climate change; dendroecology; diurnal temperature range; ecosystem response; forest growth; Mediterranean Basin;

    机译:气候变化;树状生态学昼夜温度范围生态系统反应;森林生长;地中海盆地;

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号