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Analysis of dynamic properties of Siberia climatic system

机译:西伯利亚气候系统动态特性分析

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摘要

The results of analysis of climatic system dynamic properties, which manifest themselves in temporal changeability features of atmosphere states, meteorological fields and phenomena, weather regimes and rhythms, are presented Changeability of climate forming factors and climate rhythms is considered in correlation with transformations of the environment and interrelation between the geosphere elements. A system-evolutionary approach to describe climatic changes in the context of multilevel model with the use of the information about different objects and processes of different levels has been evolved. New techniques of coupling analysis of changeability of environment, state ensemble, and intersystem relations in geosphere were developed. Special dynamics types such as long-term oscillations and directional climatic changes, which are caused by partly reversible transformations of relations, were revealed and studied. The mechanism of climate process reorganization due to the media transformation in the atmosphere and in the ocean with the subsequent formation of ice cover in North seas, which leads to changes in interrelations of the Ocean-Atmosphere-Land system, heat-mass exchange, the atmospheric circulation, and weather formation regimes, has been discovered.
机译:气候系统动态性质的分析结果,其在颞型变化状态,气象场和现象,天气制度和节奏中表现出在时间的变化特征中,被呈现了气候形成因素的可变性,并且在环境的转变相关中考虑了气候节律和地理学元素之间的相互关系。一种系统演化方法,用于描述多级模型的背景下的气候变化,利用了不同对象的信息和不同级别的过程的信息。制定了地理学环境,国家集合和地工学间关系的耦合分析的新技术。揭示和研究了由部分可逆变换引起的长期振荡和方向气候变化等特殊动力学类型。由于北海随后形成了大气和海洋中介质转化导致的气候过程重组机制,导致海洋气氛 - 陆地系统,热量交换的相互关系变化已经发现了大气循环和天气形成制度。

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