Climatic Change

, Volume 107, Issue 3, pp 267–276

On long range dependence in global surface temperature series

An editorial comment
Article

DOI: 10.1007/s10584-010-9998-z

Cite this article as:
Mann, M.E. Climatic Change (2011) 107: 267. doi:10.1007/s10584-010-9998-z

Abstract

Long Range Dependence (LRD) scaling behavior has been argued to characterize long-term surface temperature time series. LRD is typically measured by the so-called “Hurst” coefficient, “H”. Using synthetic temperature time series generated by a simple climate model with known physics, I demonstrate that the values of H obtained for observational temperature time series can be understood in terms of the linear response to past estimated natural and anthropogenic external radiative forcing combined with the effects of random white noise weather forcing. The precise value of H is seen to depend on the particular noise realization. The overall distribution obtained over an ensemble of noise realizations is seen to be a function of the relative amplitude of external forcing and internal stochastic variability and additionally in climate “proxy” records, the amount of non-climatic noise present. There is no obvious reason to appeal to more exotic physics for an explanation of the apparent scaling behavior in observed temperature data.

Supplementary material

10584_2010_9998_MOESM1_ESM.doc (121 kb)
(PDF 121 kb)

Copyright information

© Springer Science+Business Media B.V. 2010

Authors and Affiliations

  1. 1.Department of Meteorology and Earth and Environmental Systems InstitutePennsylvania State UniversityUniversity ParkUSA

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