European phenological response to climate change matches the warming pattern

Annette Menzel, Tim H. Sparks(UK Centre for Ecology & Hydrology), Nicole Estrella, Elisabeth Koch(Central Institution for Meteorology and Geodynamics), Anto Aasa(University of Tartu), Rein Ahas(University of Tartu), KERSTIN ALM‐KÜBLER(Swedish Museum of Natural History), Peter Bissolli(Deutscher Wetterdienst), OL'GA BRASLAVSKÁ(Slovak Hydrometeorological Institute), Agrita Briede(University of Latvia), Frank‐M. Chmielewski(Humboldt-Universität zu Berlin), Zalika Črepinšek(University of Ljubljana), Yannick Curnel(Walloon Agricultural Research Centre), Åslög Dahl(Göteborgs Stads), Claudio Defila(Federal Office of Meteorology and Climatology MeteoSwiss), Alison Donnelly(Trinity College Dublin), YOLANDA FILELLA(Universitat Autònoma de Barcelona), K. Jatczak(Institute of Meteorology and Water Management), F. Måge(Norwegian University of Life Sciences), Antonio Mestre(Agencia Estatal de Meteorología), Øyvind Nordli(Norwegian Meteorological Institute), Josep Peñuelas(Universitat Autònoma de Barcelona), Pentti Pirinen(Finnish Meteorological Institute), Viera Remisová(Slovak Hydrometeorological Institute), Helfried Scheifinger(Central Institution for Meteorology and Geodynamics), Martin Stříž(Czech Hydrometeorological Institute), Andreja Sušnik(Slovenian Environment Agency), A.J.H. van Vliet(Wageningen University & Research), FRANS‐EMIL WIELGOLASKI(University of Oslo), SUSANNE ZACH(Central Institution for Meteorology and Geodynamics), Ana Žust(Slovenian Environment Agency)
Global Change Biology
July 6, 2006
Cited by 3,133Open Access
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Abstract

Abstract Global climate change impacts can already be tracked in many physical and biological systems; in particular, terrestrial ecosystems provide a consistent picture of observed changes. One of the preferred indicators is phenology, the science of natural recurring events, as their recorded dates provide a high‐temporal resolution of ongoing changes. Thus, numerous analyses have demonstrated an earlier onset of spring events for mid and higher latitudes and a lengthening of the growing season. However, published single‐site or single‐species studies are particularly open to suspicion of being biased towards predominantly reporting climate change‐induced impacts. No comprehensive study or meta‐analysis has so far examined the possible lack of evidence for changes or shifts at sites where no temperature change is observed. We used an enormous systematic phenological network data set of more than 125 000 observational series of 542 plant and 19 animal species in 21 European countries (1971–2000). Our results showed that 78% of all leafing, flowering and fruiting records advanced (30% significantly) and only 3% were significantly delayed, whereas the signal of leaf colouring/fall is ambiguous. We conclude that previously published results of phenological changes were not biased by reporting or publication predisposition: the average advance of spring/summer was 2.5 days decade −1 in Europe. Our analysis of 254 mean national time series undoubtedly demonstrates that species' phenology is responsive to temperature of the preceding months (mean advance of spring/summer by 2.5 days°C −1 , delay of leaf colouring and fall by 1.0 day°C −1 ). The pattern of observed change in spring efficiently matches measured national warming across 19 European countries (correlation coefficient r =−0.69, P <0.001).


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