Abstract
This paper studied the Earth’s ozone thickness fluctuations by treating it as a non-Markovian process. Using white noise calculus and superimposed with the MSD of the empirical data, the theoretical Mean Square Displacement (MSD) is calculated. Results showed that ozone thickness fluctuations follow the non-Markovian trend, which captures the sinusoidal behavior of MSD vs. time graph for empirical data statistics at larger time.
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