首页> 外文会议>Korea-Russia International Symposium on Science and Technology >NATURAL DYNAMICS OF SUB-ARCTIC LANDSCAPES IN THE WEST SIBERIAN PLAIN AS INDICATOR OF GLOBAL CHANGES OF CLIMATE
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NATURAL DYNAMICS OF SUB-ARCTIC LANDSCAPES IN THE WEST SIBERIAN PLAIN AS INDICATOR OF GLOBAL CHANGES OF CLIMATE

机译:西伯利亚平原西北北极风景的自然动态作为气候全球变迁指标

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摘要

The natural dynamics of landscapes is a complex process driven by various factors. Climate, which in many cases determines the general direction of landscape development, plays an important role among them. However, separate components of landscape respond to the influence of climate and its changes in a different degree. Vegetation is one of the most unstable and sensitive components among them. According to investigations carried out by Tomsk State University in the West Siberian plain, contrasting processes are occurring in the South and North parts of the region. Bogs are expanding in the taiga zone and there is progressive swamping there, which leads to forest tree death. The situation in the northern part of the West Siberian Plain is completely opposite. The bogs are becoming reduced in area in this territory. Here, the forest-tundra area to the North is experiencing thermokarst activity and colonisation of bogs by trees. This is likely to be connected to recent changes of climate and probably to global warming.
机译:景观的自然动态是由各种因素驱动的复杂过程。在许多情况下,气候决定了景观发展的一般方向,在其中起重要作用。然而,单独的景观组成部分应对气候的影响及其在不同程度上的变化。植被是其中最不稳定和最敏感的部件之一。根据西伯利亚西伯利亚州大学的调查,在该地区的南部和北部地区发生了对比过程。沼泽在Taiga区扩展,那里有逐步震荡,导致森林树死亡。西西伯利亚平原北部的情况完全相反。这遍境内的区域变得越来越减少。在这里,北方的森林 - 苔原地区正在经历沼泽的热量活动和树木殖民。这可能与最近的气候变化以及全球变暖有关。

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