Abstract
Autoregressive logistic regression models have been successfully applied in medical and pharmacology research fields, and in simple models to analyze weather types. The main purpose of this paper is to introduce a general framework to study atmospheric circulation patterns capable of dealing simultaneously with: seasonality, interannual variability, long-term trends, and autocorrelation of different orders. To show its effectiveness on modeling performance, daily atmospheric circulation patterns identified from observed sea level pressure fields over the Northeastern Atlantic, have been analyzed using this framework. Model predictions are compared with probabilities from the historical database, showing very good fitting diagnostics. In addition, the fitted model is used to simulate the evolution over time of atmospheric circulation patterns using Monte Carlo method. Simulation results are statistically consistent with respect to the historical sequence in terms of (1) probability of occurrence of the different weather types, (2) transition probabilities and (3) persistence. The proposed model constitutes an easy-to-use and powerful tool for a better understanding of the climate system.
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Acknowledgments
This work was partially funded by projects “AMVAR” (CTM2010-15009), “GRACCIE” (CSD2007-00067, CONSOLIDER-INGENIO 2010), “IMAR21” (BIA2011-2890) and “PLVMA” (TRA2011-28900) from the Spanish Ministry MICINN, “MARUCA” (E17/08) from the Spanish Ministry MF and “C3E” (200800050084091) from the Spanish Ministry MAMRM. The support of the EU FP7 Theseus “Innovative technologies for safer European coasts in a changing climate”, contract ENV.2009-1, n. 244104, is also gratefully acknowledged. Y. Guanche is indebted to the Spanish Ministry of Science and Innovation for the funding provided in the FPI Program (BES-2009-027228). R. Mínguez is also indebted to the Spanish Ministry MICINN for the funding provided within the “Ramon y Cajal” program.
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Guanche, Y., Mínguez, R. & Méndez, F.J. Autoregressive logistic regression applied to atmospheric circulation patterns. Clim Dyn 42, 537–552 (2014). https://doi.org/10.1007/s00382-013-1690-3
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DOI: https://doi.org/10.1007/s00382-013-1690-3