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    Coupled Interannual Variability of the Hadley and Ferrel Cells

    Source: Journal of Climate:;2018:;volume 031:;issue 012::page 4757
    Author:
    Zurita-Gotor, Pablo
    ,
    Álvarez-Zapatero, Pablo
    DOI: 10.1175/JCLI-D-17-0752.1
    Publisher: American Meteorological Society
    Abstract: AbstractThis work investigates the covariability in the strength of the Hadley and Ferrel cells on interannual time scales using reanalysis data. A significant correlation is found in both hemispheres only during boreal winter. For other seasons, only the outermost (subtropical) part of the Hadley cell is correlated with changes in the extratropical eddy momentum fluxes, as the eddies are unable to penetrate into the deep tropics. During boreal winter, the northern Hadley cell variability is driven by extratropical planetary momentum fluxes, but the mean meridional circulation response is primarily found below the level of maximum climatological outflow. Instead, at upper levels, changes in the zonal wind dominate the response to the anomalous eddy forcing. During austral winter, the southern Hadley cell is shielded from the extratropical eddy fluxes and its variability displays some of the characteristics of the angular momentum?conserving solution.
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      Coupled Interannual Variability of the Hadley and Ferrel Cells

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    contributor authorZurita-Gotor, Pablo
    contributor authorÁlvarez-Zapatero, Pablo
    date accessioned2019-09-19T10:10:21Z
    date available2019-09-19T10:10:21Z
    date copyright3/27/2018 12:00:00 AM
    date issued2018
    identifier otherjcli-d-17-0752.1.pdf
    identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4262346
    description abstractAbstractThis work investigates the covariability in the strength of the Hadley and Ferrel cells on interannual time scales using reanalysis data. A significant correlation is found in both hemispheres only during boreal winter. For other seasons, only the outermost (subtropical) part of the Hadley cell is correlated with changes in the extratropical eddy momentum fluxes, as the eddies are unable to penetrate into the deep tropics. During boreal winter, the northern Hadley cell variability is driven by extratropical planetary momentum fluxes, but the mean meridional circulation response is primarily found below the level of maximum climatological outflow. Instead, at upper levels, changes in the zonal wind dominate the response to the anomalous eddy forcing. During austral winter, the southern Hadley cell is shielded from the extratropical eddy fluxes and its variability displays some of the characteristics of the angular momentum?conserving solution.
    publisherAmerican Meteorological Society
    titleCoupled Interannual Variability of the Hadley and Ferrel Cells
    typeJournal Paper
    journal volume31
    journal issue12
    journal titleJournal of Climate
    identifier doi10.1175/JCLI-D-17-0752.1
    journal fristpage4757
    journal lastpage4773
    treeJournal of Climate:;2018:;volume 031:;issue 012
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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