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Potential vorticity patterns in Mediterranean “hurricanes”
Author(s) -
Miglietta M. M.,
Cerrai D.,
Laviola S.,
Cattani E.,
Levizzani V.
Publication year - 2017
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1002/2017gl072670
Subject(s) - potential vorticity , troposphere , diabatic , cyclone (programming language) , stratosphere , atmospheric sciences , climatology , anomaly (physics) , vorticity , geology , vortex , positive vorticity advection , jet stream , convection , tropical cyclone , environmental science , baroclinity , meteorology , jet (fluid) , physics , mechanics , condensed matter physics , field programmable gate array , computer science , computer hardware , adiabatic process , thermodynamics
The potential vorticity (PV) anomalies due to the intrusion of dry stratospheric air and those generated by the tropospheric diabatic latent heating are qualitatively analyzed for five Mediterranean tropical‐like cyclones (also known as Medicanes). Model simulations show the presence of an upper level PV streamer in the early stages of the cyclone, located on the left exit of a jet stream, and a middle‐low level PV anomaly generated by the convection developing around the low‐level vortex. In the mature stage, the upper level PV anomaly around the cyclone evolves differently for each case and appears somehow dependent on the lifetime. Only for the 2006 Medicane, the PV anomalies form an intense PV tower extending continuously from the lower troposphere to the lower stratosphere.