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    Ocean submesoscale fronts induce diabatic heating and convective precipitation within storms by Félix Vivant, Lia Siegelman, Patrice Klein, Hector S. Torres, Dimitris Menemenlis, Andrea M. Molod

    Published 2025-01-01
    “…Additionally, ocean submesoscale fronts, with temperature gradients of 5 °C per 10 km, induce a secondary circulation reaching 4 km within the troposphere, which enhances diabatic processes and convective precipitations within storms. …”
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