Waves and climate change in the north-east Atlantic

Judith Wolf, David K. Woolf

    Research output: Contribution to journalArticle

    66 Citations (Scopus)

    Abstract

    Wave height in the North Atlantic has been observed to increase over the last quarter-century, based on monthly-mean data derived from observations. Empirical models have linked a large part of this increase in wave height with the North Atlantic Oscillation. Wave models provide a tool to study impacts of various climate change scenarios and investigate physical explanations of statistical results. In this case we use a wave model of the NE Atlantic. Model tests were carried out, using synthetic wind fields, varying the strength of the prevailing westerly winds and the frequency and intensity of storms, the location of storm tracks and the storm propagation speed. The strength of the westerly winds is most effective at increasing mean and maximum monthly wave height. The frequency, intensity, track and speed of storms have little effect on the mean wave height but intensity, track and speed significantly affect maximum wave height.

    Original languageEnglish
    Pages (from-to)L06604-L06604
    Number of pages4
    JournalGeophysical Research Letters
    Volume33
    Issue number6
    DOIs
    Publication statusPublished - 18 Mar 2006

    Cite this