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    Axisymmetric Constraints on Cross-Equatorial Hadley Cell Extent

    Source: Journal of the Atmospheric Sciences:;2019:;volume 076:;issue 006::page 1547
    Author:
    Hill, Spencer A.
    ,
    Bordoni, Simona
    ,
    Mitchell, Jonathan L.
    DOI: 10.1175/JAS-D-18-0306.1
    Publisher: American Meteorological Society
    Abstract: AbstractWe consider the relevance of known constraints from each of Hide?s theorem, the angular momentum?conserving (AMC) model, and the equal-area model on the extent of cross-equatorial Hadley cells. These theories respectively posit that a Hadley circulation must span all latitudes where the radiative?convective equilibrium (RCE) absolute angular momentum satisfies or or where the RCE absolute vorticity satisfies ; all latitudes where the RCE zonal wind exceeds the AMC zonal wind; and over a range such that depth-averaged potential temperature is continuous and that energy is conserved. The AMC model requires knowledge of the ascent latitude , which needs not equal the RCE forcing maximum latitude . Whatever the value of , we demonstrate that an AMC cell must extend at least as far into the winter hemisphere as the summer hemisphere. The equal-area model predicts , always placing it poleward of . As is moved poleward (at a given thermal Rossby number), the equal-area-predicted Hadley circulation becomes implausibly large, while both and become increasingly displaced poleward of the minimal cell extent based on Hide?s theorem (i.e., of supercritical forcing). In an idealized dry general circulation model, cross-equatorial Hadley cells are generated, some spanning nearly pole to pole. All homogenize angular momentum imperfectly, are roughly symmetric in extent about the equator, and appear in extent controlled by the span of supercritical forcing.
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      Axisymmetric Constraints on Cross-Equatorial Hadley Cell Extent

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    contributor authorHill, Spencer A.
    contributor authorBordoni, Simona
    contributor authorMitchell, Jonathan L.
    date accessioned2019-10-05T06:51:47Z
    date available2019-10-05T06:51:47Z
    date copyright3/18/2019 12:00:00 AM
    date issued2019
    identifier otherJAS-D-18-0306.1.pdf
    identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4263658
    description abstractAbstractWe consider the relevance of known constraints from each of Hide?s theorem, the angular momentum?conserving (AMC) model, and the equal-area model on the extent of cross-equatorial Hadley cells. These theories respectively posit that a Hadley circulation must span all latitudes where the radiative?convective equilibrium (RCE) absolute angular momentum satisfies or or where the RCE absolute vorticity satisfies ; all latitudes where the RCE zonal wind exceeds the AMC zonal wind; and over a range such that depth-averaged potential temperature is continuous and that energy is conserved. The AMC model requires knowledge of the ascent latitude , which needs not equal the RCE forcing maximum latitude . Whatever the value of , we demonstrate that an AMC cell must extend at least as far into the winter hemisphere as the summer hemisphere. The equal-area model predicts , always placing it poleward of . As is moved poleward (at a given thermal Rossby number), the equal-area-predicted Hadley circulation becomes implausibly large, while both and become increasingly displaced poleward of the minimal cell extent based on Hide?s theorem (i.e., of supercritical forcing). In an idealized dry general circulation model, cross-equatorial Hadley cells are generated, some spanning nearly pole to pole. All homogenize angular momentum imperfectly, are roughly symmetric in extent about the equator, and appear in extent controlled by the span of supercritical forcing.
    publisherAmerican Meteorological Society
    titleAxisymmetric Constraints on Cross-Equatorial Hadley Cell Extent
    typeJournal Paper
    journal volume76
    journal issue6
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/JAS-D-18-0306.1
    journal fristpage1547
    journal lastpage1564
    treeJournal of the Atmospheric Sciences:;2019:;volume 076:;issue 006
    contenttypeFulltext
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