北方森林生态资源对温室气体的吸附和对全球变暖的适应

E. Kolomyts
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摘要

实现《巴黎气候变化协定》(2015年)规定的目标的最重要方法之一是解决双重任务:1)森林群落在全球变暖期间从大气中吸收二氧化碳,2)适应这些气候变化,这应确保吸附本身的有效性。给定的报告介绍了该任务数值求解的区域经验。对奥卡-伏尔加河流域森林形成的碳平衡进行了计算,用于全球中度和极端变暖的预测。所提出的森林生态系统不稳定弹塑性稳定性指数是森林生态系统同构恢复潜力的特征,被用作适应指标。使用多元回归方法对奥卡河流域的领土进行了数值实验,以评估森林结构的弹性稳定性和预测的气候条件对碳平衡的影响。共得到11个线性方程(显著性水平为P<10-6)。在即将到来的100年预测期内,森林结构的整体弹塑性稳定性应该会提高,并在极端变暖的情况下最大限度地提高。因此,人们应该预计北方森林吸收温室气体的能力会显著提高。碳平衡值的比较​​用初始(基本)和最终(最终)稳定性指数获得的森林形成的数据清楚地表明,北方森林的吸附能力随着其再生潜力的增加而显著增加。植树造林适应能力的提高对增加温室气体的吸收起到了决定性的作用,这是一个直接的环境因素。
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Ecological resources of boreal forests in the adsorption of greenhouse gases and in adaptation to global warming
One of the most important ways to achieve the goals stipulated by the Paris (2015) Agreement on Climate Change is to solve a two-fold task: 1) the absorption of CO2 by the forest communities from the atmosphere during global warming and 2) their adaptation to these climate changes, which should ensure the effectiveness of adsorption itself. Given report presents the regional experience of the numerical solution of this task. Calculations of the carbon balance of forest formations in the Oka-Volga River basin were carried out for global forecasts of moderate and extreme warming. The proposed index of labile elastic-plastic stability of forest ecosystems, which characterizes their isomorphic-restorative potential, was used as an indicator of adaptation. For the territory of the Oka river basin using multiple regression methods, a numerical experiment was conducted to assess the effect of the elastic stability of forest formations and the predicted climatic conditions on the carbon balance. A total of 11 linear equations were obtained (with a significance level of P <10-6). In the upcoming 100-year forecast period, the overall elastic-plastic stability of forest formations should increase, and to the greatest extent with extreme warming. Accordingly, one should expect a significant increase in the ability of boreal forests to absorb greenhouse gases. A comparison of the carbon balance values ​​of forest formations obtained with initial (base) and final (final) stability indices gives an unambiguous picture of a significant increase in the adsorption capacity of boreal forests with an increase in their regenerative potential. A decisive contribution to increasing the adsorption of greenhouse gases is made by the growth of reforestation adaptation, which plays the role of a direct environmental factor.
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