Complex North Atlantic Oscillation (NAO) index signal of historic North Atlantic storm-track changes

A. G. Dawson (Lead / Corresponding author), K. Hickey, T. Holt, L. Elliott, S. Dawson, I. D. L. Foster, P. Wadhams, I. Jonsdottir, J. Wilkinson, J. McKenna, N. R. Davis, D. E. Smith

    Research output: Contribution to journalArticlepeer-review

    58 Citations (Scopus)

    Abstract

    Previous reports have suggested a link between increased storminess in the North Atlantic during recent years with a period of time during which the North Atlantic Oscillation Index has been strongly positive. New analyses of late nineteenth-century gale-day data for meteorological stations in northern Scotland and western Ireland indicate that the relatively high storminess that characterized this period was associated with monthly NAO Index values that rarely exceeded +2 and, on several occasions, were strongly negative. It is speculated that this difference may reflect the influence of an expanded sea-ice cover in the Greenland Sea that caused a considerable southward displacement of the North Atlantic storm track during the late nineteenth century. Such changes imply that the polar atmospheric and oceanic fronts in the North Atlantic were displaced southward during the late nineteenth century.

    Original languageEnglish
    Pages (from-to)363-369
    Number of pages7
    JournalHolocene
    Volume12
    Issue number3
    DOIs
    Publication statusPublished - 1 Apr 2002

    Keywords

    • Climatic change
    • Gale days
    • Historic storms
    • Historical evidence
    • NAO Index
    • North Atlantic Oscillation
    • Sea ice

    Fingerprint

    Dive into the research topics of 'Complex North Atlantic Oscillation (NAO) index signal of historic North Atlantic storm-track changes'. Together they form a unique fingerprint.

    Cite this