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    Rain triggers seasonal stratification in a temperate shelf sea


    Jardine, J. E. and Palmer, M. and Mahaffey, C. and Holt, J. and Wakelin, S. L. and Düsterhus, Andre and Sharples, J. and Wihsgott, J. (2023) Rain triggers seasonal stratification in a temperate shelf sea. Nature Communications, 14 (3182). pp. 1-12. ISSN 2041-1723

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    Abstract

    The North Atlantic Storm Track acts as a conveyor belt for extratropical cyclones that frequently deliver high winds and rainfall to northwest European shelf seas. Storms are primarily considered detrimental to shelf sea stratification due to wind-driven mixing countering thermal buoyancy, but their impact on shelf scale stratification cycles remains poorly understood. Here, we show that storms trigger stratification through enhanced surface buoyancy from rainfall. A multidecadal model confirms that rainfall contributed to triggering seasonal stratification 88% of the time from 1982 to 2015. Stratification could be further modulated by large-scale climate oscillations, such as the Atlantic Multidecadal Variability (AMV), with stratification onset dates being twice as variable during a positive AMV phase than a negative one. Further insights into how changing storm activity will impact shelf seas are discussed beyond the current view of increasing wind-driven mixing, with significant implications for marine productivity and ecosystem function.

    Item Type: Article
    Keywords: rain; triggers; season stratification; temperate shelf sea;
    Academic Unit: Faculty of Social Sciences > Geography
    Faculty of Social Sciences > Research Institutes > Irish Climate Analysis and Research Units, ICARUS
    Item ID: 17449
    Identification Number: https://doi.org/10.1038/s41467-023-38599-y
    Depositing User: André Düsterhus
    Date Deposited: 17 Aug 2023 14:56
    Journal or Publication Title: Nature Communications
    Publisher: Nature Publshing Group
    Refereed: Yes
    URI:
    Use Licence: This item is available under a Creative Commons Attribution Non Commercial Share Alike Licence (CC BY-NC-SA). Details of this licence are available here

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