Atmospheric thermodynamics and dynamics during convective, stratiform and nonprecipitating clouds over the metropolitan area of Rio de Janeiro – Brazil

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Main Author: Fabricio Polifke Da Silva
Format: Artículo científico
Language:en
Published: Universidad Nacional Autónoma de México 2022
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author Fabricio Polifke Da Silva
author_facet Fabricio Polifke Da Silva
contents Atmospheric thermodynamics and dynamics during convective, stratiform and nonprecipitating clouds over the metropolitan area of Rio de Janeiro – Brazil Fabricio Polifke Da Silva Otto Corrêa Rotunno Filho Maria Gertrudes Alvarez Justi Da Silva Rafael João Sampaio Gisele Dornelles Pires Afonso Augusto Magalhães De Araújo Biología Clouds Rainfall Radiosonde Reflectivity Physical mechanisms involved in the development and forecast of clouds and precipitation are both quite complex and dependent on the local atmospheric environment, especially when severe weather conditions are imminent. Research aimed at understanding the environmental mechanisms favorable to the different atmospheric scenarios can help operational weather forecasters to issue warnings. This paper provides qualitative and quantitative contributions from radiosondes, radar, and numerical simulations to evaluate the formation of convective, stratiform, and nonprecipitating clouds over the metropolitan area of Rio de Janeiro, Brazil. The convective available potential energy (CAPE) and lifted index (LI), showed higher values on convective days (CAPE = 2600 J.Kg–1 and LI = –4 ºC), followed by nonprecipitating (CAPE = 1500 J.Kg–1 and LI = –2 ºC) and stratiform cloud days (CAPE = 1400 J.Kg–1 and LI = –1.5 ºC). High wind convergence was observed at low- (1000–850 hPa) and mid- (850–700 hPa) levels on convective days (–16.5 s–1 and –9.6 s–1, respectively). In contrast, wind divergence at the same levels was observed on stratiform (6.4 s–1 and 6.9 s–1) and nonprecipitating (9.7 s–1 and 7.3 s–1) days. Higher wind divergence (8.3 s–1) was observed on convective days at upper levels (300–200 hPa) compared with stratiform (3.2 s–1) and nonprecipitating (2.8 s–1) days. Results show a coupling of wind convergence, moisture and energy in the lower troposphere and divergence at upper levels on convective days. Despite moisture availability on stratiform days and thermodynamic energy on nonprecipitating days, the respective coupling between these conditions and dynamic triggers was not observed. 2022 artículo científico 0187-6236 https://www.redalyc.org/articulo.oa?id=56581609007 https://www.redalyc.org/journal/565/56581609007/ https://www.redalyc.org/journal/565/56581609007/html/ https://www.redalyc.org/journal/565/56581609007/56581609007.epub https://www.redalyc.org/journal/565/56581609007/movil 10.20937/ATM.52832 en http://www.redalyc.org/revista.oa?id=565 Atmósfera application/pdf Universidad Nacional Autónoma de México Atmósfera (México) Num.2 Vol.35
format Artículo científico
id redalyc_56581609007
institution Redalyc
language en
publishDate 2022
publisher Universidad Nacional Autónoma de México
spellingShingle Atmospheric thermodynamics and dynamics during convective, stratiform and nonprecipitating clouds over the metropolitan area of Rio de Janeiro – Brazil
Fabricio Polifke Da Silva
Biología
Clouds
Rainfall
Radiosonde
Reflectivity
Atmospheric thermodynamics and dynamics during convective, stratiform and nonprecipitating clouds over the metropolitan area of Rio de Janeiro – Brazil Fabricio Polifke Da Silva Otto Corrêa Rotunno Filho Maria Gertrudes Alvarez Justi Da Silva Rafael João Sampaio Gisele Dornelles Pires Afonso Augusto Magalhães De Araújo Biología Clouds Rainfall Radiosonde Reflectivity Physical mechanisms involved in the development and forecast of clouds and precipitation are both quite complex and dependent on the local atmospheric environment, especially when severe weather conditions are imminent. Research aimed at understanding the environmental mechanisms favorable to the different atmospheric scenarios can help operational weather forecasters to issue warnings. This paper provides qualitative and quantitative contributions from radiosondes, radar, and numerical simulations to evaluate the formation of convective, stratiform, and nonprecipitating clouds over the metropolitan area of Rio de Janeiro, Brazil. The convective available potential energy (CAPE) and lifted index (LI), showed higher values on convective days (CAPE = 2600 J.Kg–1 and LI = –4 ºC), followed by nonprecipitating (CAPE = 1500 J.Kg–1 and LI = –2 ºC) and stratiform cloud days (CAPE = 1400 J.Kg–1 and LI = –1.5 ºC). High wind convergence was observed at low- (1000–850 hPa) and mid- (850–700 hPa) levels on convective days (–16.5 s–1 and –9.6 s–1, respectively). In contrast, wind divergence at the same levels was observed on stratiform (6.4 s–1 and 6.9 s–1) and nonprecipitating (9.7 s–1 and 7.3 s–1) days. Higher wind divergence (8.3 s–1) was observed on convective days at upper levels (300–200 hPa) compared with stratiform (3.2 s–1) and nonprecipitating (2.8 s–1) days. Results show a coupling of wind convergence, moisture and energy in the lower troposphere and divergence at upper levels on convective days. Despite moisture availability on stratiform days and thermodynamic energy on nonprecipitating days, the respective coupling between these conditions and dynamic triggers was not observed. 2022 artículo científico 0187-6236 https://www.redalyc.org/articulo.oa?id=56581609007 https://www.redalyc.org/journal/565/56581609007/ https://www.redalyc.org/journal/565/56581609007/html/ https://www.redalyc.org/journal/565/56581609007/56581609007.epub https://www.redalyc.org/journal/565/56581609007/movil 10.20937/ATM.52832 en http://www.redalyc.org/revista.oa?id=565 Atmósfera application/pdf Universidad Nacional Autónoma de México Atmósfera (México) Num.2 Vol.35
title Atmospheric thermodynamics and dynamics during convective, stratiform and nonprecipitating clouds over the metropolitan area of Rio de Janeiro – Brazil
topic Biología
Clouds
Rainfall
Radiosonde
Reflectivity
url https://www.redalyc.org/articulo.oa?id=56581609007
https://www.redalyc.org/journal/565/56581609007/
https://www.redalyc.org/journal/565/56581609007/html/
https://www.redalyc.org/journal/565/56581609007/56581609007.epub
https://www.redalyc.org/journal/565/56581609007/movil