Migration of the painted lady butterfly, Vanessa cardui, to north-eastern Spain is aided by African wind currents



    1. Butterfly Monitoring Scheme, Museu de Granollers de Ciències Naturals, Francesc Macià, 51, E-08402 Granollers, Spain;
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    1. Department of Physics and Nuclear Engineering, Universitat Politècnica de Catalunya, Avda Victor Balaguer s/n, E-08800 Vilanova i la Geltrú, Spain; and
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    1. Center for Ecological Research and Forestry Applications, Edifici C, Universitat Autònoma de Barcelona, 08193 Bellaterra, Barcelona, Spain
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Constantí Stefanescu, Butterfly Monitoring Scheme, Museu de Granollers de Ciències Naturals, Francesc Macià, 51, E-08402 Granollers, Spain. E-mail: canliro@teleline.es


  • 1Thousands of records of migratory butterfly species such as Vanessa cardui flying just above ground-level on fixed compass bearings have led to the common belief that these insects migrate within the so-called ‘flight-boundary layer’, where movements are relatively independent of the wind.
  • 2Given the selective advantages of windborne migration and the existence of a number of observations of flights of V. cardui from the upper levels of the atmosphere, we tested the hypothesis that migration from North Africa to southern Europe in this species is influenced by synoptic-scale wind currents.
  • 3Even with modern technology, it is extremely difficult to observe high-altitude flights directly, so we rely on an indirect approach that examines whether or not arrival peaks in north-eastern Spain are associated with winds blowing from Africa.
  • 4Arrivals of V. cardui were determined for the spring period (1 March–27 June, 1997–2006) at 79 sites in the Catalan Butterfly Monitoring Scheme. Wind patterns were described on the basis of synoptic-scale maps, transport models and back-trajectories calculated for each day of the spring period.
  • 5We found a strong association between migration and winds from North Africa, both for the whole data set (1997–2006; χ2 = 4·7, P = 0·03) and for a restricted data set that excludes years in which the species was very scarce (χ2 = 7·26, P = 0·007).
  • 6Episodes of massive northward migration within the species’ flight-boundary layer also coincided with spells of winds from North Africa, suggesting a connection between low-altitude (observational) and high-altitude flights (inferred from wind patterns).
  • 7Finally, on the assumption that migration in V. cardui is windborne, a source–receptor transport model applied to spring abundance data in north-eastern Spain enables us to identify the most probable population source areas in North Africa.