Reversible record breaking and variability: Temperature distributions across the globe

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Abstract

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 a is suggested and studied for an ensemble of monthly temperature time series around the globe. Deviation of (α) (mean α) 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, (α) = -1.0, indicating decreasing variability. This value is an order of magnitude greater than the 3σ value of stationary simulations. Using the conventional best-fit Gaussian temperature distribution, the trend is associated with a change of about -0.2°C (106 yr)-1 in the standard deviation of interannual monthly mean temperature distributions (about 10%). © 2010 American Meteorological Society.

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Anderson, A., & Kostinski, A. (2010). Reversible record breaking and variability: Temperature distributions across the globe. Journal of Applied Meteorology and Climatology, 49(8), 1681–1691. https://doi.org/10.1175/2010JAMC2407.1

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