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The impact of future forest dynamics on climate: interactive effects of changing vegetation and disturbance regimes

机译:未来森林动力对气候的影响:不断变化的植被和干扰机制的相互作用

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摘要

Currently, the temperate forest biome cools the earth’s climate and dampens anthropogenic climate change. However, climate change will substantially alter forest dynamics in the future, affecting the climate regulation function of forests. Increasing natural disturbances can reduce carbon uptake and evaporative cooling, but at the same time increase the albedo of a landscape. Simultaneous changes in vegetation composition can mitigate disturbance impacts, but also influence climate regulation directly (e.g., via albedo changes). As a result of a number of interactive drivers (changes in climate, vegetation, and disturbance) and their simultaneous effects on climate-relevant processes (carbon exchange, albedo, latent heat flux) the future climate regulation function of forests remains highly uncertain. Here we address these complex interactions to assess the effect of future forest dynamics on the climate system. Our specific objectives were (1) to investigate the long-term interactions between changing vegetation composition and disturbance regimes under climate change, (2) to quantify the response of climate regulation to changes in forest dynamics, and (3) to identify the main drivers of the future influence of forests on the climate system. We investigated these issues using the individual-based forest landscape and disturbance model (iLand). Simulations were run over 200 yr for Kalkalpen National Park (Austria), assuming different future climate projections, and incorporating dynamically responding wind and bark beetle disturbances. To consistently assess the net effect on climate the simulated responses of carbon exchange, albedo, and latent heat flux were expressed as contributions to radiative forcing. We found that climate change increased disturbances (+27.7% over 200 yr) and specifically bark beetle activity during the 21st century. However, negative feedbacks from a simultaneously changing tree species composition (+28.0% broadleaved species) decreased disturbance activity in the long run (−10.1%), mainly by reducing the host trees available for bark beetles. Climate change and the resulting future forest dynamics significantly reduced the climate regulation function of the landscape, increasing radiative forcing by up to +10.2% on average over 200 yr. Overall, radiative forcing was most strongly driven by carbon exchange. We conclude that future changes in forest dynamics can cause amplifying climate feedbacks from temperate forest ecosystems.
机译:目前,温带森林生物群落可冷却地球的气候,并抑制人为的气候变化。然而,气候变化将在未来极大地改变森林的动态,影响森林的气候调节功能。自然干扰的增加会减少碳的吸收和蒸发冷却,但同时会增加景观的反照率。植被组成的同时变化可以减轻干扰影响,但也可以直接影响气候调节(例如,通过反照率变化)。由于许多互动驱动因素(气候,植被和干扰的变化)及其对气候相关过程(碳交换,反照率,潜热通量)的同时影响,森林的未来气候调节功能仍然高度不确定。在这里,我们解决了这些复杂的相互作用,以评估未来森林动力对气候系统的影响。我们的具体目标是(1)研究气候变化下植被组成的变化与干扰机制之间的长期相互作用;(2)量化气候调节对森林动态变化的响应;(3)确定主要驱动力森林对气候系统的未来影响我们使用基于个体的森林景观和干扰模型(iLand)调查了这些问题。假设未来的气候变化不同,并结合了动态响应的风和树皮甲虫干扰,对加尔卡彭国家公园(奥地利)进行了200年的模拟。为了一致地评估对气候的净影响,将碳交换,反照率和潜热通量的模拟响应表示为对辐射强迫的贡献。我们发现,在21世纪,气候变化增加了干扰(200多年以来增加了27.7%),尤其是树皮甲虫的活动。但是,从同时变化的树种组成(+ 28.0%阔叶树种)获得的负面反馈从长远来看降低了干扰活动(-10.1%),主要是通过减少可用于树皮甲虫的寄主树。气候变化和由此产生的未来森林动态显着降低了景观的气候调节功能,在200年内平均平均使辐射强迫增加了+ 10.2%。总体而言,辐射强迫受碳交换的驱动最大。我们得出结论,森林动态的未来变化会导致来自温带森林生态系统的气候反馈放大。

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