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    New Insights on the Formation and Breaking Mechanism of Convective Cyclonic Cones in the South Adriatic Pit during Winter 2018

    Source: Journal of Physical Oceanography:;2022:;volume( 052 ):;issue: 009::page 2049
    Author:
    A. Pirro
    ,
    E. Mauri
    ,
    R. Gerin
    ,
    R. Martellucci
    ,
    P. Zuppelli
    ,
    P. M. Poulain
    DOI: 10.1175/JPO-D-21-0108.1
    Publisher: American Meteorological Society
    Abstract: The deepwater formation in the northern part of the South Adriatic Pit (Mediterranean Sea) is investigated using a unique oceanographic dataset. In situ data collected by a glider along the Bari–Dubrovnik transect captured the mixing and the spreading/restratification phase of the water column in winter 2018. After a period of about 2 weeks from the beginning of the mixing phase, a homogeneous convective area of ∼300-m depth breaks up due to the baroclinic instability process in cyclonic cones made of geostrophically adjusted fluid. The base of these cones is located at the bottom of the mixed layer, and they extend up to the theoretical critical depth
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      New Insights on the Formation and Breaking Mechanism of Convective Cyclonic Cones in the South Adriatic Pit during Winter 2018

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4289766
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    • Journal of Physical Oceanography

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    contributor authorA. Pirro
    contributor authorE. Mauri
    contributor authorR. Gerin
    contributor authorR. Martellucci
    contributor authorP. Zuppelli
    contributor authorP. M. Poulain
    date accessioned2023-04-12T18:29:43Z
    date available2023-04-12T18:29:43Z
    date copyright2022/09/01
    date issued2022
    identifier otherJPO-D-21-0108.1.pdf
    identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4289766
    description abstractThe deepwater formation in the northern part of the South Adriatic Pit (Mediterranean Sea) is investigated using a unique oceanographic dataset. In situ data collected by a glider along the Bari–Dubrovnik transect captured the mixing and the spreading/restratification phase of the water column in winter 2018. After a period of about 2 weeks from the beginning of the mixing phase, a homogeneous convective area of ∼300-m depth breaks up due to the baroclinic instability process in cyclonic cones made of geostrophically adjusted fluid. The base of these cones is located at the bottom of the mixed layer, and they extend up to the theoretical critical depth
    publisherAmerican Meteorological Society
    titleNew Insights on the Formation and Breaking Mechanism of Convective Cyclonic Cones in the South Adriatic Pit during Winter 2018
    typeJournal Paper
    journal volume52
    journal issue9
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/JPO-D-21-0108.1
    journal fristpage2049
    journal lastpage2068
    page2049–2068
    treeJournal of Physical Oceanography:;2022:;volume( 052 ):;issue: 009
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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