Long-term predictability of mean daily temperature data

W. von Bloh, M. C. Romano, Marco Thiel

Research output: Contribution to journalArticle

18 Citations (Scopus)

Abstract

We quantify the long-term predictability of global mean daily temperature data by means of the Renyi entropy of second order K-2. We are interested in the yearly amplitude fluctuations of the temperature. Hence, the data are low-pass filtered. The obtained oscillatory signal has a more or less constant frequency, depending on the geographical coordinates, but its amplitude fluctuates irregularly. Our estimate of K-2 quantifies the complexity of these amplitude fluctuations. We compare the results obtained for the CRU data set (interpolated measured temperature in the years 1901-2003 with 0.5 degrees resolution, Mitchell et al., 2005(1)) with the ones obtained for the temperature data from a coupled ocean-atmosphere global circulation model (AOGCM, calculated at DKRZ). Furthermore, we compare the results obtained by means of K-2 with the linear variance of the temperature data.
Original languageEnglish
Pages (from-to)471-479
Number of pages9
JournalNonlinear Processes in Geophysics
Volume12
Issue number4
DOIs
Publication statusPublished - 2005

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temperature
Temperature
entropy
oceans
Entropy
atmospheres
atmosphere
ocean
estimates

Keywords

  • recurrence plot
  • climate change
  • attractors
  • dynamics
  • Pacific
  • weather
  • model
  • flow

Cite this

Long-term predictability of mean daily temperature data. / von Bloh, W.; Romano, M. C.; Thiel, Marco.

In: Nonlinear Processes in Geophysics, Vol. 12, No. 4, 2005, p. 471-479.

Research output: Contribution to journalArticle

von Bloh, W. ; Romano, M. C. ; Thiel, Marco. / Long-term predictability of mean daily temperature data. In: Nonlinear Processes in Geophysics. 2005 ; Vol. 12, No. 4. pp. 471-479.
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