A numerical modelling investigation of the role of diabatic heating and cooling in the development of a mid-level vortex prior to tropical cyclogenesis – Part 1: The response to stratiform components of diabatic forcing

Mid-tropospheric mesoscale convective vortices have been often observed to precede tropical cyclogenesis. Moreover, recent cloud-resolving numerical modelling studies that are initialized with a weak cyclonic mid-tropospheric vortex sometimes show a considerable intensification of the mid-level circ...

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Published in:Atmospheric chemistry and physics 2018-10, Vol.18 (19), p.14393-14416
Main Authors: Nicholls, Melville E, Pielke Sr., Roger A, Wheeler, Donavan, Carrio, Gustavo, Smith, Warren P
Format: Article
Language:English
Subjects:
Adiabatic
Amplification
Angular momentum
Anvils
Ascent
Cells
Components
Computer simulation
Conservation
Conservation of angular momentum
Convective activity
Convective cells
Convective vortices
Cooling
Cyclogenesis
Cyclones
Diabatic cooling
Diabatic heating
Evaporation
Heating
Heating and cooling
Hydrometeors
Ice environments
Inflow
Mathematical models
Melting
Mesoscale convective vortices
Mesoscale vortexes
Microphysics
Modelling
Momentum
Numerical simulations
Ocean circulation
Physics
Removal
Simulation
Sublimation
Surface wind
Thermodynamic processes
Tropical climate
Tropical cyclogenesis
Tropical cyclones
Tropical depressions
Troposphere
Upper troposphere
Vortex motion
Vortices
Winds
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cited_by cdi_FETCH-LOGICAL-c483t-b97acb8934a5f5d6791dc29b9d71bca606e32b65f692c82bb4d68523969d13593
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description Mid-tropospheric mesoscale convective vortices have been often observed to precede tropical cyclogenesis. Moreover, recent cloud-resolving numerical modelling studies that are initialized with a weak cyclonic mid-tropospheric vortex sometimes show a considerable intensification of the mid-level circulation prior to the development of the strong cyclonic surface winds that characterize tropical cyclogenesis. The objective of this two-part study is to determine the processes that lead to the development of a prominent mid-level vortex during a simulation of the transformation of a tropical disturbance into a tropical depression, in particular the role of diabatic heating and cooling. For simplicity simulations are initialized from a quiescent environment. In this first part, results of the numerical simulation are described and the response to stratiform components of the diabatic forcing is investigated. In the second part, the contribution of diabatic heating in convective cells to the development of the mid-level vortex is examined.
doi_str_mv 10.5194/acp-18-14393-2018
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subjects Adiabatic
Amplification
Angular momentum
Anvils
Ascent
Cells
Components
Computer simulation
Conservation
Conservation of angular momentum
Convective activity
Convective cells
Convective vortices
Cooling
Cyclogenesis
Cyclones
Diabatic cooling
Diabatic heating
Evaporation
Heating
Heating and cooling
Hydrometeors
Ice environments
Inflow
Mathematical models
Melting
Mesoscale convective vortices
Mesoscale vortexes
Microphysics
Modelling
Momentum
Numerical simulations
Ocean circulation
Physics
Removal
Simulation
Sublimation
Surface wind
Thermodynamic processes
Tropical climate
Tropical cyclogenesis
Tropical cyclones
Tropical depressions
Troposphere
Upper troposphere
Vortex motion
Vortices
Winds
title A numerical modelling investigation of the role of diabatic heating and cooling in the development of a mid-level vortex prior to tropical cyclogenesis – Part 1: The response to stratiform components of diabatic forcing
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