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首页> 外文期刊>Global change biology >Long-term physiological and growth responses of Himalayan fir to environmental change are mediated by mean climate
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Long-term physiological and growth responses of Himalayan fir to environmental change are mediated by mean climate

机译:喜马拉雅杉木对环境变革的长期生理和生长反应是由平均气候介导的

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High-elevation forests are experiencing high rates of warming, in combination with CO2 rise and (sometimes) drying trends. In these montane systems, the effects of environmental changes on tree growth are also modified by elevation itself, thus complicating our ability to predict effects of future climate change. Tree-ring analysis along an elevation gradient allows quantifying effects of gradual and annual environmental changes. Here, we study long-term physiological (ratio of internal to ambient CO2, i.e., C-i/C-a and intrinsic water-use efficiency, iWUE) and growth responses (tree-ring width) of Himalayan fir (Abies spectabilis) trees in response to warming, drying, and CO2 rise. Our study was conducted along elevational gradients in a dry and a wet region in the central Himalaya. We combined dendrochronology and stable carbon isotopes (delta C-13) to quantify long-term trends in C-i/C-a ratio and iWUE (delta C-13-derived), growth (mixed-effects models), and evaluate climate sensitivity (correlations). We found that iWUE increased over time at all elevations, with stronger increase in the dry region. Climate-growth relations showed growth-limiting effects of spring moisture (dry region) and summer temperature (wet region), and negative effects of temperature (dry region). We found negative growth trends at lower elevations (dry and wet regions), suggesting that continental-scale warming and regional drying reduced tree growth. This interpretation is supported by delta C-13-derived long-term physiological responses, which are consistent with responses to reduced moisture and increased vapor pressure deficit. At high elevations (wet region), we found positive growth trends, suggesting that warming has favored tree growth in regions where temperature most strongly limits growth. At lower elevations (dry and wet regions), the positive effects of CO2 rise did not mitigate the negative effects of warming and drying on tree growth. Our results raise concerns on the productivity of Himalayan fir forests at low and middle (<3,300 m) elevations as climate change progresses.
机译:高海拔森林正在经历高温率,与二氧化碳崛起和(有时)干燥趋势相结合。在这些蒙尾系统中,环境变化对树木增长的影响也被提升本身修改,从而使我们预测未来气候变化影响的能力使我们能够变得复杂化能力。沿着高程梯度的树木分析允许量化逐渐和年度环境变化的影响。在这里,我们研究喜马拉雅杉(Abies Spectabilis)树木的长期生理(内部到环境CO2,即CI / CA和内在水使用效率,IWUE)和生长响应(树木宽度)的生长响应(树木宽度)。变暖,干燥和二氧化碳上升。我们的研究沿着喜马拉雅市中心的干燥和潮湿地区沿着高地梯度进行。我们组合树突和稳定的碳同位素(Delta C-13)来量化CI / Ca比和IWUE(Delta C-13-衍生的),生长(混合效果模型)的长期趋势,评价气候敏感性(相关性) 。我们发现IWUE在所有高度随时间都随着时间的推移而增加,干燥区域越来越强。气候生长关系显示春季水分(干燥区)和夏季温度(湿地区)的生长限制效果,以及温度(干燥区)的负面影响。我们发现较低的海拔(干湿地区)的负增长趋势,表明大陆级变暖和区域干燥降低了树增长。该解释由Delta C-13衍生的长期生理反应支持,这与对降低水分和增加的蒸气压缺损的反应一致。在高海拔(潮湿地区),我们发现了积极的增长趋势,表明变暖在温度最大限度地限制的区域中有利于树木增长。在较低的海拔(干湿区域),二氧化碳崛起的正效应并未减轻暖和干燥对树生长的负面影响。随着气候变化的进展,我们的结果提高了低于低中和中间(<3,300米)的杉木森林的生产率的担忧。

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