Abstract

A case study of Western Siberia has shown that the anomalies observed in the natural environment of the Sub-Arctic are the consequences of the unfolding process of the movement of the planet’s core in the northward direction which is accompanied by enhanced degassing of the subsoil. It is demonstrated that the flow of heat into the lower atmosphere during the oxidation of increasing volumes of hydrogen has led to an increase in air temperature over the last several decades, and the largest anomalies are observed in September ‒ December. This is the effect of an enhancement in degassing as the Earth approaches the perihelion point, when the core continues to move by inertia and its pressure on the outer shells increases. An analysis is made of dendrochronological data indicating a negative impact on the growth of trees by a shortage of available soil moisture with an enhanced transpiration in conditions of high summer temperatures and degradation of permafrost. The study revealed a northward expansion of the habitats of many plant and animal species and a contradictory behavior of forest at the boundary with the tundra. It is established that two options should be considered in the analysis of the possible ways of a further development of events. One variant implies a continuation of directional changes in the endogenous origin in northern geosystems. The other variant is characterized by forced oscillations associated with long-term cycles of the Solar System, the latest temporal time limit of which dates back to 1990. We compiled a general scheme of the chain reaction “movement of the Earth’s core - degassing of the subsoil ‒ hydrogen oxidation – warming of the soil and ground air – plant growth” chain reaction; however, a large number of uncertainties remain as to the mechanisms of momentum transfer in each link.

中文翻译：

---

西西伯利亚北部地球系统当前变化的原因

摘要

西伯利亚西部的一个案例研究表明，在亚北极自然环境中观察到的异常现象是行星核向北运动的展开过程的结果，同时伴随着地下土壤脱气的增加。事实证明，在过去几十年中，随着氢气体积的增加，氧化过程中进入低层大气的热量导致气温升高，并且在9月至12月期间观测到最大的异常现象。当岩心继续通过惯性运动并且其在外壳上的压力增加时，随着地球接近近日点，这是增强脱气的效果。对树木年代学数据的分析表明，由于夏季高温和多年冻土退化的条件下土壤水分的缺乏以及蒸腾作用的增强，对树木的生长产生了负面影响。研究表明，许多动植物物种的生境向北扩展，在苔原边界处森林的行为相互矛盾。确定在分析事件进一步发展的可能方式时应考虑两个选择。一种变体意味着北部地球系统内生源的方向变化的延续。另一个变体的特征是与太阳系的长期循环有关的强迫振荡，其最新的时间期限可追溯到1990年。我们编制了一个连锁反应的总体方案：“地核的运动-底土脱气‒氢氧化-土壤和地面空气的变暖-植物生长”连锁反应；但是，在每个环节中动量传递的机制仍存在大量不确定性。