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    Madden–Julian Oscillation Impacts on Australian Temperatures and Extremes

    Source: Journal of Climate:;2022:;volume( 036 ):;issue: 002::page 335
    Author:
    Andrew G. Marshall
    ,
    Matthew C. Wheeler
    ,
    Tim Cowan
    DOI: 10.1175/JCLI-D-22-0413.1
    Publisher: American Meteorological Society
    Abstract: We assess seasonally varying impacts of the Madden–Julian oscillation (MJO) on Australian maximum and minimum temperature anomalies and extremes, and their modulation by El Niño–Southern Oscillation (ENSO), for the period June 1974–May 2022. Our composite-based approach uses observed temperatures from the Australian Gridded Climate Data, and 850-hPa wind data from the NCEP–NCAR reanalysis, to show how relationships to temperature and circulation evolve over the eight-phase life cycle of the MJO, which we derive from the real-time multivariate MJO index. The MJO has significant impacts on Australian temperatures and winds in all parts of the country at various times throughout the year, and to varying degrees. Two of the most pronounced impacts are 1) daytime warming across southeastern Australia in MJO phase 3 during spring associated with a strong anomalous anticyclone and 2) nighttime cooling over Queensland in MJO phase 7 during winter associated with anomalous advection of cool dry continental air. La Niña acts to significantly lessen both of these impacts, while El Niño enhances both the phase 3 warming over southern Australia in spring and the phase 7 overnight cooling over southern Queensland in winter. We show how the MJO can combine with El Niño and La Niña to have strong compounding influences, thus highlighting the importance of understanding interactions between multiple modes of climate variability and how they relate to Australian temperatures and extremes.
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      Madden–Julian Oscillation Impacts on Australian Temperatures and Extremes

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    contributor authorAndrew G. Marshall
    contributor authorMatthew C. Wheeler
    contributor authorTim Cowan
    date accessioned2023-04-12T18:41:02Z
    date available2023-04-12T18:41:02Z
    date copyright2022/12/21
    date issued2022
    identifier otherJCLI-D-22-0413.1.pdf
    identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4290066
    description abstractWe assess seasonally varying impacts of the Madden–Julian oscillation (MJO) on Australian maximum and minimum temperature anomalies and extremes, and their modulation by El Niño–Southern Oscillation (ENSO), for the period June 1974–May 2022. Our composite-based approach uses observed temperatures from the Australian Gridded Climate Data, and 850-hPa wind data from the NCEP–NCAR reanalysis, to show how relationships to temperature and circulation evolve over the eight-phase life cycle of the MJO, which we derive from the real-time multivariate MJO index. The MJO has significant impacts on Australian temperatures and winds in all parts of the country at various times throughout the year, and to varying degrees. Two of the most pronounced impacts are 1) daytime warming across southeastern Australia in MJO phase 3 during spring associated with a strong anomalous anticyclone and 2) nighttime cooling over Queensland in MJO phase 7 during winter associated with anomalous advection of cool dry continental air. La Niña acts to significantly lessen both of these impacts, while El Niño enhances both the phase 3 warming over southern Australia in spring and the phase 7 overnight cooling over southern Queensland in winter. We show how the MJO can combine with El Niño and La Niña to have strong compounding influences, thus highlighting the importance of understanding interactions between multiple modes of climate variability and how they relate to Australian temperatures and extremes.
    publisherAmerican Meteorological Society
    titleMadden–Julian Oscillation Impacts on Australian Temperatures and Extremes
    typeJournal Paper
    journal volume36
    journal issue2
    journal titleJournal of Climate
    identifier doi10.1175/JCLI-D-22-0413.1
    journal fristpage335
    journal lastpage357
    page335–357
    treeJournal of Climate:;2022:;volume( 036 ):;issue: 002
    contenttypeFulltext
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