空气温度、相对湿度和露点温度的动态转变和最大可预测性的证据

Abidemi E. Adeniji, Adewoyin D. Adeyinka
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引用次数: 0

摘要

监测和预测气候现象是全球关注的主要问题,因为它对人们的生活和环境造成了毁灭性的影响。因此,有必要了解控制气候现象动态演变的自然过程。本文分析了2012年1月1日至12月31日,由大气研究中心(CAR)在Nsukka站以5分钟为单位采集的气温和相对湿度数据。露点温度是根据空气温度和相对湿度的实际读数,采用适当的经验关系式计算出来的。本文采用平均互信息法(AMI)、伪近邻法(FNN)和李雅普诺夫指数法(Lyapunov index)研究了这些气象参数的动态变化和过渡,以及它们与整体动态状态的时间偏差。结果表明,气温、相对湿度和露点温度所需的动态模型分别具有4-5维、4-6维和4-5维。在气温、相对湿度和露点温度时间序列上分别观察到正李雅普诺夫指数和负李雅普诺夫指数。这表明这些气象时间序列的混沌行为存在固有的周期性,导致从混沌性(正Lyapunov指数)到周期性(负Lyapunov指数),再到混沌性(正Lyapunov指数)的过渡。因此,这些结果提供了关于气候转变、最大可预测性以及制定天气预报模式的额外信息。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Evidence of dynamical transition and maximum predictability of air temperature, relative humidity and dew point temperature
Monitoring and predicting the climatic phenomenon are the major global concern because of its devasting effects on people's lives and their environments. As a result of this, there is a need to understand the natural processes that control the dynamic evolution of the climatic phenomenon. Air temperature and relative humidity data collected from Nsukka station by the Centre for Atmospheric Research (CAR), measured in 5 minutes time steps from 1st January till 31st December, 2012 have been analysed. Dew point temperature was calculated from the actual readings of air temperature and relative humidity using appropriate empirical relation. In this paper, Average Mutual Information (AMI), False Nearest Neighbour (FNN) and Lyapunov Exponent methods were used to study changes and transitions in the dynamics of these meteorological parameters or temporal deviations from their overall dynamical regimes. The results show that the dynamic model needed to describe the data has 4-5 dimensions for air temperature, 4-6 for relative humidity and 4-5 for dew point temperature. Positive and negative Lyapunov exponents were observed in the air temperature, relative humidity and dew point temperature time series. This indicates that there exists periodicity inherent in the chaotic behaviour of these meteorological time series, causing a transition from chaoticity (positive Lyapunov exponent) to periodicity (negative Lyapunov exponent) and thereafter to chaoticity (positive Lyapunov exponent). The results, therefore, provide additional information about the climate transitions, maximum predictability and also, for formulating a weather prediction model.
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