Influence of the NAO on the northwestern Mediterranean wave climate

Authors

  • Bartomeu Cañellas IMEDEA (CSIC-UIB)
  • Alejandro Orfila IMEDEA (CSIC-UIB)
  • Fernando Méndez Environmental Hydraulic Institute, IH Cantabria, Universidad de Cantabria
  • Alberto Álvarez IMEDEA (CSIC-UIB)
  • Joaquín Tintoré IMEDEA (CSIC-UIB)

DOI:

https://doi.org/10.3989/scimar.2010.74n1055

Keywords:

teleconnections, wave climate, NAO, EOF, Mediterranean Sea, variability

Abstract


This study examines teleconnections between the North Atlantic Oscillation (NAO) and the wave climate of the northwestern Mediterranean Sea (NWM), defined by the monthly mean significant wave height (SWH) and the 95th percentile significant wave height (95th percentile SWH), in the period ranging from 1958 to 2001. The data analyzed comes from the multidecadal hindcast over Europe carried out during the HIPOCAS project. In order to avoid fictitious cross-correlations, data were prewhitened by fitting a p-order autoregressive model. To split the temporal and spatial variability, an EOF encoding technique was applied to residuals before searching for teleconnections. We found the northwestern Mediterranean wave climate to be influenced by the North Atlantic Oscillation (NAO) with an instantaneous response. When the NAO is in its positive phase, positive anomalies in the SWH and the 95th percentile SWH appear in the area between the Balearic Islands, the Gulf of Lions and the Catalonian coast.

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Published

2010-03-30

How to Cite

1.
Cañellas B, Orfila A, Méndez F, Álvarez A, Tintoré J. Influence of the NAO on the northwestern Mediterranean wave climate. Sci. mar. [Internet]. 2010Mar.30 [cited 2024Mar.28];74(1):55-64. Available from: https://scientiamarina.revistas.csic.es/index.php/scientiamarina/article/view/1129

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