Tornado Seasonality in Central‐Southern Chile

Abstract Tornado records in Chile show an apparent seasonality with a peak between May and June. We study this seasonality in central‐south and austral Chile by analyzing three indicators of tornado environments: vorticity generation parameter (VGP), storm‐relative helicity (SRH) and mean relative h...

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Main Authors: V. Caballero‐Morán, R. Rondanelli
Format: Article
Language:English
Published: Wiley 2025-01-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1029/2024GL110900
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author V. Caballero‐Morán
R. Rondanelli
author_facet V. Caballero‐Morán
R. Rondanelli
author_sort V. Caballero‐Morán
collection DOAJ
description Abstract Tornado records in Chile show an apparent seasonality with a peak between May and June. We study this seasonality in central‐south and austral Chile by analyzing three indicators of tornado environments: vorticity generation parameter (VGP), storm‐relative helicity (SRH) and mean relative humidity RH‾. Annual cycles of VGP, SRH and RH‾ show favorable conditions during the fall in the central‐south region, well correlated with the records in the area, and associated with maximum values of low‐level (0–1 km) and deep‐layer (0–6 km) wind shear, and relatively high values of most unstable CAPE. In the austral region, favorable conditions occur during the summer, in the presence of maximum deep‐layer wind shear and maximum values of the most unstable CAPE. Analysis of temperature, wind, and humidity were performed to understand the mechanisms that lead to the development of these conditions in these two regions.
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institution Kabale University
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spelling doaj-art-1f7a9291ec9f43dda468b1864f378e342025-01-20T13:05:57ZengWileyGeophysical Research Letters0094-82761944-80072025-01-01521n/an/a10.1029/2024GL110900Tornado Seasonality in Central‐Southern ChileV. Caballero‐Morán0R. Rondanelli1Department of Geophysics Universidad de Chile Santiago ChileDepartment of Geophysics Universidad de Chile Santiago ChileAbstract Tornado records in Chile show an apparent seasonality with a peak between May and June. We study this seasonality in central‐south and austral Chile by analyzing three indicators of tornado environments: vorticity generation parameter (VGP), storm‐relative helicity (SRH) and mean relative humidity RH‾. Annual cycles of VGP, SRH and RH‾ show favorable conditions during the fall in the central‐south region, well correlated with the records in the area, and associated with maximum values of low‐level (0–1 km) and deep‐layer (0–6 km) wind shear, and relatively high values of most unstable CAPE. In the austral region, favorable conditions occur during the summer, in the presence of maximum deep‐layer wind shear and maximum values of the most unstable CAPE. Analysis of temperature, wind, and humidity were performed to understand the mechanisms that lead to the development of these conditions in these two regions.https://doi.org/10.1029/2024GL110900tornadoessevere weathercentral southern Chilevorticity generation parametercold‐season tornadoesseasonality
spellingShingle V. Caballero‐Morán
R. Rondanelli
Tornado Seasonality in Central‐Southern Chile
Geophysical Research Letters
tornadoes
severe weather
central southern Chile
vorticity generation parameter
cold‐season tornadoes
seasonality
title Tornado Seasonality in Central‐Southern Chile
title_full Tornado Seasonality in Central‐Southern Chile
title_fullStr Tornado Seasonality in Central‐Southern Chile
title_full_unstemmed Tornado Seasonality in Central‐Southern Chile
title_short Tornado Seasonality in Central‐Southern Chile
title_sort tornado seasonality in central southern chile
topic tornadoes
severe weather
central southern Chile
vorticity generation parameter
cold‐season tornadoes
seasonality
url https://doi.org/10.1029/2024GL110900
work_keys_str_mv AT vcaballeromoran tornadoseasonalityincentralsouthernchile
AT rrondanelli tornadoseasonalityincentralsouthernchile