Based on counts of record highs and lows, and employing reversibility in time, an approach to examining natural variability is proposed. The focus is on intrinsic variability; that is, variance separated from the trend in the mean. A variability index alpha is suggested and studied for an ensemble of monthly temperature time series around the globe. Deviation of <alpha > (mean alpha) from zero, for an ensemble of time series, signifies a variance trend in a distribution-independent manner. For 15 635 monthly temperature time series from different geographical locations (Global Historical Climatology Network), each time series about a century-long, <alpha > = -1.0, indicating decreasing variability. This value is an order of magnitude greater than the 3 sigma value of stationary simulations. Using the conventional best-fit Gaussian temperature distribution, the trend is associated with a change of about -0.2 degrees C (106 yr) (1) in the standard deviation of interannual monthly mean temperature distributions (about 10%).