Abstract

Capsule Evidence for earlier spring migration of Tringa sandpipers after warmer winters, but no clear pattern concerning autumn migration timing. Aim To analyse the timing of migration of three Tringa sandpipers between 1966 and 2002 with respect to recent global warming on a local and a hemispheric scale. Methods I analysed long-term migration timing variation in Greenshank Tringa nebularia, Spotted Redshank T. erythropus and Wood Sandpiper T. glareola at four Central European staging sites. Variation in passage onset, median and end per migration period was analysed using stepwise regression with respect to variation in (i) local abundance, residence time and age-dependent abundance as an estimate of breeding success and (ii) climate at the staging sites, snowmelt at the presumed central breeding area and the North Atlantic Oscillation (NAO). Results All three species consistently showed an overall spring migration advance and autumn migration delay. Autumn passage timing varied with both climatic conditions at the breeding area and breeding success, while in 43% of all cases spring passage correlated with local and hemispheric climate variation. Conclusion The distinction between population dynamic and climatic effects on timing of autumn migration requires separate data for local adult and juvenile passage or a larger sample of sites. In spring, the data strongly suggest a flexible response of migration timing to local weather conditions and the hemispheric variation of the North Atlantic Oscillation. This indicates that even long-distance migrants are able to adjust their overall migration pattern to fluctuating environmental conditions on a phenotypic basis.

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