Rains and Showers in OTREC; Weak Temperature Gradient Modeling

Abstract Rainfall in the tropics has been shown to be produced either by isolated but intense convective systems (showers regime) or widespread but weaker systems (rains regime). We examine significant rainfall systems observed in the OTREC project (Organization of Tropical East Pacific Convection)...

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Main Authors: D. J. Raymond, Ž. Stone, S. Sentić
Format: Article
Language:English
Published: American Geophysical Union (AGU) 2024-03-01
Series:Journal of Advances in Modeling Earth Systems
Online Access:https://doi.org/10.1029/2023MS003980
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author D. J. Raymond
Ž. Stone
S. Sentić
author_facet D. J. Raymond
Ž. Stone
S. Sentić
author_sort D. J. Raymond
collection DOAJ
description Abstract Rainfall in the tropics has been shown to be produced either by isolated but intense convective systems (showers regime) or widespread but weaker systems (rains regime). We examine significant rainfall systems observed in the OTREC project (Organization of Tropical East Pacific Convection) in order to tease out the physical mechanisms differentiating these two regimes. We find that rains occur in very moist environments, typically with weak conditional instability. In contrast, showers develop in drier environments with larger instability. Spectral weak temperature gradient numerical calculations show that showers are associated with episodic rainfall separated by significant quiescent periods, whereas rains produce continuous simulated rainfall after a spinup period. Mass flux profiles of showers and rains are very different, resulting in different effects on the large scale environment.
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spelling doaj.art-1e0b3600bb9a47eda6036daa799ba26a2024-04-04T21:25:34ZengAmerican Geophysical Union (AGU)Journal of Advances in Modeling Earth Systems1942-24662024-03-01163n/an/a10.1029/2023MS003980Rains and Showers in OTREC; Weak Temperature Gradient ModelingD. J. Raymond0Ž. Stone1S. Sentić2Physics Department and Climate and Weather Consortium New Mexico Tech Socorro NM USAPhysics Department and Climate and Weather Consortium New Mexico Tech Socorro NM USAPhysics Department and Climate and Weather Consortium New Mexico Tech Socorro NM USAAbstract Rainfall in the tropics has been shown to be produced either by isolated but intense convective systems (showers regime) or widespread but weaker systems (rains regime). We examine significant rainfall systems observed in the OTREC project (Organization of Tropical East Pacific Convection) in order to tease out the physical mechanisms differentiating these two regimes. We find that rains occur in very moist environments, typically with weak conditional instability. In contrast, showers develop in drier environments with larger instability. Spectral weak temperature gradient numerical calculations show that showers are associated with episodic rainfall separated by significant quiescent periods, whereas rains produce continuous simulated rainfall after a spinup period. Mass flux profiles of showers and rains are very different, resulting in different effects on the large scale environment.https://doi.org/10.1029/2023MS003980
spellingShingle D. J. Raymond
Ž. Stone
S. Sentić
Rains and Showers in OTREC; Weak Temperature Gradient Modeling
Journal of Advances in Modeling Earth Systems
title Rains and Showers in OTREC; Weak Temperature Gradient Modeling
title_full Rains and Showers in OTREC; Weak Temperature Gradient Modeling
title_fullStr Rains and Showers in OTREC; Weak Temperature Gradient Modeling
title_full_unstemmed Rains and Showers in OTREC; Weak Temperature Gradient Modeling
title_short Rains and Showers in OTREC; Weak Temperature Gradient Modeling
title_sort rains and showers in otrec weak temperature gradient modeling
url https://doi.org/10.1029/2023MS003980
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AT zstone rainsandshowersinotrecweaktemperaturegradientmodeling
AT ssentic rainsandshowersinotrecweaktemperaturegradientmodeling