Exceptional European warmth of autumn 2006 and winter 2007: Historical context, the underlying dynamics, and its phenological impacts

Jürg Luterbacher, Mark A. Liniger, Annette Menzel, Nicole Estrella, Paul M. Della‐Marta, Christian Pfister, This Rutishauser, Elena Xoplaki

Geophysical Research Letters · 2007 · 202 citations · 24 references

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TL;DR

Autumn 2006 and winter 2007 were the warmest in over 500 years, with widespread European surface‑air‑temperature anomalies reaching up to three standard deviations from normal. The warmth was driven by strong anticyclonic conditions and southwest warm‑air advection, leading to partial second flowering or extended flowering into winter for some species and an earlier flowering of early‑spring species after winter 2007.

Abstract

Updated European averaged autumn and winter surface air temperature (SAT) timeseries indicate that the autumn 2006 and winter 2007 were extremely likely (>95%) the warmest for more than 500 years. In both seasons, the European SAT anomaly is widespread with anomalies up to three standard deviations from normal. The anomalous warmth is associated with strong anticyclonic conditions and warm air advection from south west. Phenological impacts related to this warmth included some plant species having a partial second flowering or extended flowering till the beginning of winter. Species that typically flower in early spring were found to have a distinct earlier flowering after winter 2007.

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