Cold surges and dust events: Establishing the link between the East Asian Winter Monsoon and the Chinese loess record

Karl-Heinz Wyrwoll, J. Wei, Z. Lin, Y. Shao, F. He

    Research output: Contribution to journalArticle

    2 Citations (Scopus)

    Abstract

    © 2016The Chinese loess/palaeosol succession is one of the most comprehensive and intensively studied archives of Neogene and Quaternary global palaeoclimate events. Its stratigraphic details are widely recognised to indicate close links to the history and function of the East Asian Winter Monsoon (EAWM) – one of the most active components of the Earth's climate system. But the formal meteorological links between the EAWM and dust emission, both in the present day and in the past, have not been established and with it, the veracity of the loess record as an indicator of the EAWM questioned. Here we show that present day major dust events over northern China, while largely occurring during spring, are nevertheless ‘conditioned’ by the strength of the preceding EAWM. We also demonstrate, for the first time, a close link between the occurrence of dust events and the strength of the EAWM. From these findings, linked to global-scale climate model simulations, we conclude that the Chinese loess succession provides a convincing proxy record of the strength of the East Asian Winter Monsoon.
    Original languageEnglish
    Pages (from-to)102-108
    JournalQuaternary Science Reviews
    Volume149
    DOIs
    Publication statusPublished - 2016

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    loess
    dust
    monsoon
    climate
    major event
    winter
    event
    present
    simulation model
    China
    history
    dust emissions
    climate models
    paleosol
    paleoclimate
    Neogene
    cold
    Cold
    Asia
    Winter

    Cite this

    @article{0e0cbbfc98df4832a849cfeeca56d75a,
    title = "Cold surges and dust events: Establishing the link between the East Asian Winter Monsoon and the Chinese loess record",
    abstract = "{\circledC} 2016The Chinese loess/palaeosol succession is one of the most comprehensive and intensively studied archives of Neogene and Quaternary global palaeoclimate events. Its stratigraphic details are widely recognised to indicate close links to the history and function of the East Asian Winter Monsoon (EAWM) – one of the most active components of the Earth's climate system. But the formal meteorological links between the EAWM and dust emission, both in the present day and in the past, have not been established and with it, the veracity of the loess record as an indicator of the EAWM questioned. Here we show that present day major dust events over northern China, while largely occurring during spring, are nevertheless ‘conditioned’ by the strength of the preceding EAWM. We also demonstrate, for the first time, a close link between the occurrence of dust events and the strength of the EAWM. From these findings, linked to global-scale climate model simulations, we conclude that the Chinese loess succession provides a convincing proxy record of the strength of the East Asian Winter Monsoon.",
    author = "Karl-Heinz Wyrwoll and J. Wei and Z. Lin and Y. Shao and F. He",
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    language = "English",
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    pages = "102--108",
    journal = "Quaternary Science Reviews",
    issn = "0277-3791",
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    Cold surges and dust events: Establishing the link between the East Asian Winter Monsoon and the Chinese loess record. / Wyrwoll, Karl-Heinz; Wei, J.; Lin, Z.; Shao, Y.; He, F.

    In: Quaternary Science Reviews, Vol. 149, 2016, p. 102-108.

    Research output: Contribution to journalArticle

    TY - JOUR

    T1 - Cold surges and dust events: Establishing the link between the East Asian Winter Monsoon and the Chinese loess record

    AU - Wyrwoll, Karl-Heinz

    AU - Wei, J.

    AU - Lin, Z.

    AU - Shao, Y.

    AU - He, F.

    PY - 2016

    Y1 - 2016

    N2 - © 2016The Chinese loess/palaeosol succession is one of the most comprehensive and intensively studied archives of Neogene and Quaternary global palaeoclimate events. Its stratigraphic details are widely recognised to indicate close links to the history and function of the East Asian Winter Monsoon (EAWM) – one of the most active components of the Earth's climate system. But the formal meteorological links between the EAWM and dust emission, both in the present day and in the past, have not been established and with it, the veracity of the loess record as an indicator of the EAWM questioned. Here we show that present day major dust events over northern China, while largely occurring during spring, are nevertheless ‘conditioned’ by the strength of the preceding EAWM. We also demonstrate, for the first time, a close link between the occurrence of dust events and the strength of the EAWM. From these findings, linked to global-scale climate model simulations, we conclude that the Chinese loess succession provides a convincing proxy record of the strength of the East Asian Winter Monsoon.

    AB - © 2016The Chinese loess/palaeosol succession is one of the most comprehensive and intensively studied archives of Neogene and Quaternary global palaeoclimate events. Its stratigraphic details are widely recognised to indicate close links to the history and function of the East Asian Winter Monsoon (EAWM) – one of the most active components of the Earth's climate system. But the formal meteorological links between the EAWM and dust emission, both in the present day and in the past, have not been established and with it, the veracity of the loess record as an indicator of the EAWM questioned. Here we show that present day major dust events over northern China, while largely occurring during spring, are nevertheless ‘conditioned’ by the strength of the preceding EAWM. We also demonstrate, for the first time, a close link between the occurrence of dust events and the strength of the EAWM. From these findings, linked to global-scale climate model simulations, we conclude that the Chinese loess succession provides a convincing proxy record of the strength of the East Asian Winter Monsoon.

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