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Experimental Testing the Regulator Mechanisms of Local Climate Evolution

机译:实验测试局部气候演变的调节机制

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A climate system represents a nonlinear system to convert solar energy. So, involving both the bifurcation theory and the control theory into the research concerning regulator mechanisms of local climate evolution can give interesting results. For example, five years ago so-called HDS- hypothesis was proposed, in accordance with which local climate dynamics is determined by natural competition between the amplitude quantization (restricted by the temperature Hysteresis) and the time quantization (caused by the Double Synchronization). The conceptual model of local climate dynamics from this hypothesis (so-called HDS-model) first provided building bifurcation diagrams by processing the data of meteorological observations and also explained the phenomenon of the interannual variability from the bifurcation consequences. Here we discuss the HDS-hypothesis in order to find a way to soften the problem known within the limits of the traditional climatology, namely: how to research evolution of local climate dynamics under the essential scarcity of the data necessary to analysis. We use the electronic setup, mathematical model of which is equivalent to the HDS-model. We focus on complex behaviors when fast alternations of averaged meteorological variables (temperature, pressure, precipitation, and so on) can occur, which are not supposed to consider in the context of the traditional hypothesis on local climate dynamics. We compare the dynamics evolution made by the mathematical modeling with the observations made for both electronic and natural real systems. From the control theory, these results show striking similarity between the HDS- dynamics and local climate dynamics; from the climate theory, these results continue the novel interdisciplinary exploring in the local dynamics evolution.
机译:气候系统代表一种转换太阳能的非线性系统。因此,将分叉理论和控制理论都纳入到有关局部气候演变的调控机制的研究中,可以得出有趣的结果。例如,五年前提出了所谓的HDS假说,根据该假说,当地的气候动力学是由幅度量化(受温度滞后限制)和时间量化(由双重同步引起)之间的自然竞争来确定的。基于该假设的局部气候动力学概念模型(所谓的HDS模型)首先通过处理气象观测数据来提供建筑物分叉图,还解释了由分叉后果引起的年际变化现象。在这里,我们讨论HDS假设,以便找到一种方法来软化在传统气候学范围内已知的问题,即:如何在分析所必需的数据基本匮乏的情况下研究局部气候动力学的演变。我们使用电子装置,其数学模型等效于HDS模型。当平均气象变量(温度,压力,降水等)发生快速变化时,我们将重点放在复杂的行为上,而在传统的本地气候动态假设中,这是不应该考虑的。我们将数学建模的动力学演化与对电子和自然真实系统的观测结果进行比较。从控制理论来看,这些结果表明,HDS动力学与局部气候动力学之间具有惊人的相似性。从气候理论出发,这些结果继续了对局部动力学演化的新的跨学科探索。

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