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    Intraseasonal and Seasonal-to-Interannual Indian Ocean Convection and Hemispheric Teleconnections

    Source: Journal of Climate:;2013:;volume( 026 ):;issue: 022::page 8850
    Author:
    Hoell, Andrew
    ,
    Barlow, Mathew
    ,
    Saini, Roop
    DOI: 10.1175/JCLI-D-12-00306.1
    Publisher: American Meteorological Society
    Abstract: eep tropical convection over the Indian Ocean leads to intense diabatic heating, a main driver of the climate system. The Northern Hemisphere circulation and precipitation associated with intraseasonal and seasonal-to-interannual components of the leading pattern of Indian Ocean convection are investigated for November?April 1979?2008. The leading pattern of Indian Ocean convection is separated into intraseasonal and seasonal-to-interannual components by filtering an index of outgoing longwave radiation at 33?105 days and greater than 105 days, yielding Madden?Julian oscillation (MJO)- and El Niño?Southern Oscillation (ENSO)-influenced patterns, respectively. Observations and barotropic Rossby wave ray tracing experiments suggest that Indian Ocean convection can influence the ENSO-related hemispheric teleconnection pattern in addition to the regional Asian teleconnection. Equivalent barotropic circulation anomalies throughout the Northern Hemisphere subtropics are associated with both seasonal-to-interannual Indian Ocean convection and ENSO. The hemispheric teleconnection associated with seasonal-to-interannual Indian Ocean convection is investigated with ray tracing, which suggests that forcing over the Indian Ocean can propagate eastward across the hemisphere and back to Asia. The relationship between the seasonal-to-interannual component of Indian Ocean convection and ENSO is investigated in terms of a gradient in sea surface temperatures (SST) over the equatorial western Pacific Ocean. When the western Pacific SST gradient is strong during ENSO, strong Maritime Continent precipitation extends further westward into the Indian Ocean, which is accompanied by enhanced tropospheric Asian circulation, similar to the seasonal-to-interannual component of Indian Ocean convection. Analysis of the three strongest interannual convection seasons shows that the strong Indian Ocean pattern of ENSO can dominate individual seasons.
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      Intraseasonal and Seasonal-to-Interannual Indian Ocean Convection and Hemispheric Teleconnections

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    contributor authorHoell, Andrew
    contributor authorBarlow, Mathew
    contributor authorSaini, Roop
    date accessioned2017-06-09T17:06:42Z
    date available2017-06-09T17:06:42Z
    date copyright2013/11/01
    date issued2013
    identifier issn0894-8755
    identifier otherams-79544.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4222336
    description abstracteep tropical convection over the Indian Ocean leads to intense diabatic heating, a main driver of the climate system. The Northern Hemisphere circulation and precipitation associated with intraseasonal and seasonal-to-interannual components of the leading pattern of Indian Ocean convection are investigated for November?April 1979?2008. The leading pattern of Indian Ocean convection is separated into intraseasonal and seasonal-to-interannual components by filtering an index of outgoing longwave radiation at 33?105 days and greater than 105 days, yielding Madden?Julian oscillation (MJO)- and El Niño?Southern Oscillation (ENSO)-influenced patterns, respectively. Observations and barotropic Rossby wave ray tracing experiments suggest that Indian Ocean convection can influence the ENSO-related hemispheric teleconnection pattern in addition to the regional Asian teleconnection. Equivalent barotropic circulation anomalies throughout the Northern Hemisphere subtropics are associated with both seasonal-to-interannual Indian Ocean convection and ENSO. The hemispheric teleconnection associated with seasonal-to-interannual Indian Ocean convection is investigated with ray tracing, which suggests that forcing over the Indian Ocean can propagate eastward across the hemisphere and back to Asia. The relationship between the seasonal-to-interannual component of Indian Ocean convection and ENSO is investigated in terms of a gradient in sea surface temperatures (SST) over the equatorial western Pacific Ocean. When the western Pacific SST gradient is strong during ENSO, strong Maritime Continent precipitation extends further westward into the Indian Ocean, which is accompanied by enhanced tropospheric Asian circulation, similar to the seasonal-to-interannual component of Indian Ocean convection. Analysis of the three strongest interannual convection seasons shows that the strong Indian Ocean pattern of ENSO can dominate individual seasons.
    publisherAmerican Meteorological Society
    titleIntraseasonal and Seasonal-to-Interannual Indian Ocean Convection and Hemispheric Teleconnections
    typeJournal Paper
    journal volume26
    journal issue22
    journal titleJournal of Climate
    identifier doi10.1175/JCLI-D-12-00306.1
    journal fristpage8850
    journal lastpage8867
    treeJournal of Climate:;2013:;volume( 026 ):;issue: 022
    contenttypeFulltext
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