Atmospheric flows exhibit selfsimilar fractal spacetime fluctuations manifested as the fractal geometry to global cloud cover pattern and inverse power law form for power spectra of meteorological parameters such as windspeed, temperature, rainfall etc. Inverse power law form for power spectra indicate long-range spacetime correlations or non-local connections and is a signature of selforganised criticality generic to dynamical systems in nature such as river flows, population dynamics, heart beat patterns etc. The author has developed a general systems theory which predicts the observed selforganised criticality as a signature of quantumlike chaos in dynamical systems. The model predictions are (i) The fractal fluctuations can be resolved into an overall logarithmic spiral trajectory with the quasiperiodic Penrose tiling pattern for the internal structure. (ii) The probability distribution represents the power (variance) spectrum for fractal fluctuations and follows universal inverse power law form incorporating the golden mean. Such a result that the additive amplitudes of eddies when squared represent probability distribution is observed in the subatomic dynamics of quantum systems such as the electron or photon. Therefore the irregular or unpredictable fractal fluctuations exhibit quantumlike chaos. (iii) Atmospheric aerosols are held in suspension by the vertical velocity distribution (spectrum). The atmospheric aerosol size spectrum is derived in terms of the universal inverse power law characterizing atmospheric eddy energy spectrum. Model predicted spectrum is in agreement with the following two experimentally determined atmospheric aerosol data sets, (i) SAFARI 2000 CV-580 Aerosol Data, Dry Season 2000 (CARG) (ii) World Data Centre Aerosols data sets for the three stations Ny {\AA}lesund, Pallas and Hohenpeissenberg.
翻译:大气流动呈现自相近的分形空间时间波动,表现为对全球云层覆盖模式的分形几何测量以及风速、温度、降雨等气象参数的电源光谱反电法形式。电力光谱反电法形式显示的是长距离空间时间相关关系或非局部连接,是自然动态系统(如河流流动、人口动态、心脏跳动模式等)的自我组织临界特征的标志。作者开发了一个一般系统理论,该理论预测了观察到的自组织临界度,这是动态系统中类似量级的混乱的特征。模型预测是:(一) 碎形波动可以溶解成一个总体对数螺旋性轨轨,而内部结构则是半周期性平流平面平面平面平面平面平面平面平面平面平面。