• Login
    View Item 
    •   DSpace Home
    • Institute's contributions
    • Scholarly literature
    • View Item
    •   DSpace Home
    • Institute's contributions
    • Scholarly literature
    • View Item
    JavaScript is disabled for your browser. Some features of this site may not work without it.

    Role of subsurface layer temperature inversion in cyclone induced warming in the northern Bay of Bengal

    Thumbnail
    View/Open
    10902.pdf (1.276Mb)
    Date
    2023
    Author
    Anand, P.
    Jimna, J.C.M.
    Nair, A.P.
    Suresh, I.
    Suneel, V.
    Gopika, S.
    Pankajakshan, T.
    Metadata
    Show full item record
    Abstract
    Subsurface Layer Temperature Inversion (SLTI) is a prominent physical process occurring in the Bay of Bengal (BoB) during winter. BoB also witnesses intense cyclones during winter (post-monsoon). Sidr is a category-5 cyclone that occurred in the BoB during 11–15 November 2007. The present study emphasises bringing out the effect of SLTI on SST warming. This paper uses observations and modelling to present SLTI's role in surface layer post-cyclone warming. In the absence of SLTI, the cyclone induces surface cooling. However, in the case of a surface layer with SLTI, instead of cooling, sea surface warming of < 0.5 °C is observed near the head bay, where SLTI is prominent. Model results and observations suggest the role of entrainment and warming of the surface layer.
    URI
    https://doi.org/10.1016/J.DYNATMOCE.2023.101389
    http://drs.nio.res.in/drs/handle/2264/9107
    Collections
    • Scholarly literature [9074]

    DSpace software copyright © 2002-2016  DuraSpace
    Contact Us | Send Feedback
    Theme by 
    Atmire NV
     

     

    Browse

    All of DSpaceCommunities & CollectionsBy Issue DateAuthorsTitlesSubjectsThis CollectionBy Issue DateAuthorsTitlesSubjects

    My Account

    LoginRegister

    DSpace software copyright © 2002-2016  DuraSpace
    Contact Us | Send Feedback
    Theme by 
    Atmire NV