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The Dynamics of the Tundra-Taiga Boundary: An Overview and Suggested Coordinated and Integrated Approach to Research

机译:Tundra-Taiga边界的动力学:研究概述和建议的协调综合方法

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The tundra-taiga boundary stretches for more than 13 400 km around the Northern Hemisphere and is probably the Earth's greatest vegetation transition. The trees that define the boundary have been sensitive to climate changes in the past and models of future vegetation distribution suggest a rapid and dramatic invasion of the tundra by the taiga. Such changes would generate both positive and negative feedbacks to the climate system and the balance could result in a net warming effect. However, the boundary is becoming increasingly affected by human activities that remove trees and degrade forest-tundra into tundra-like areas. Because of the vastness and remoteness of the tundra-taiga boundary, and of methodological problems such as problematic definitions and lack of standardized methods to record the location and characteristics of the ecotone, a project group has been established under the auspices of the International Arctic Science Committee (IASC). This paper summarizes the initial output of the group and focuses on our uncertainties in understanding the current processes at the tundra-taiga boundary and the conflicts between model predictions of change sin the location of the boundary and contrasting recently observed changes due to human activities. Finally, we present recommendations for a coordinated international approach to the problem and invite the international community to join us in reducing the uncertainties about the dynamics of the ecotone and their consequences.
机译:苔原-taiga边界在北半球周围延伸了13400多公里,可能是地球上最大的植被转变。界定边界的树木过去对气候变化敏感,未来的植被分布模型表明,针叶林对苔原的迅速而戏剧性的入侵。这样的变化将对气候系统产生正反馈和负反馈,并且平衡可能导致净变暖效应。但是,边界越来越受到人类活动的影响,这些活动将树木砍伐并使森林冻原退化为苔原状区域。由于苔原-taiga边界的广阔和遥远,以及诸如定义问题和缺乏记录生态交错带位置和特征的标准化方法等方法学问题,在国际北极科学的主持下成立了一个项目小组委员会(IASC)。本文总结了该小组的初始产出,并将重点放在不确定性上,以了解苔原-taiga边界的当前过程以及边界变化的模型预测与边界位置之间的冲突,以及对比最近由于人类活动而观察到的变化。最后,我们提出了以协调一致的国际办法解决这一问题的建议,并邀请国际社会与我们一道减少关于生态过渡动态及其后果的不确定性。

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