Eulerian Correlation of Temperature in the Atmosphere and Oceans

Abstract

TOMODA'S method for calculating the correlation coefficients R(t)has been applied to temperature analysis in the atmosphere and oceans. The results show that the temperature fluctuations are caused by turbulence m=4/3, diurnal variation m =2, and some factor related to temperature durability m=1, being represented R(t)∼1- (t/T₀)^m,The maximum passage time of turbulence was T₀=30 hr.