Observed and estimated atmospheric thermodynamic instability using radiosonde observations over the city of Rio de Janeiro, Brazil
Autor: | Otto Corrêa Rotunno Filho, Maria Gertrudes Alvarez Justi da Silva, Gisele Dornelles Pires, Fabricio Polifke da Silva, Rafael João Sampaio, Afonso Augusto Magalhães de Araújo |
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Rok vydání: | 2019 |
Předmět: |
Atmospheric Science
010504 meteorology & atmospheric sciences Advection 0208 environmental biotechnology Storm Context (language use) 02 engineering and technology 01 natural sciences 020801 environmental engineering law.invention Atmosphere Depth sounding law Climatology Radiosonde Environmental science South Atlantic Convergence Zone 0105 earth and related environmental sciences Morning |
Zdroj: | Meteorology and Atmospheric Physics. 132:297-314 |
ISSN: | 1436-5065 0177-7971 |
Popis: | Estimating critical weather conditions for the generation of storms with heavy rainfall represents one of the main challenges in the scientific community, especially in the warm season. While the use of radiosonde data is a possible option, an important limitation for achieving reliable forecasting of extreme rainfall events is undoubtedly low spatio-temporal resolution. As such, this research work endeavored to provide a special contribution by analyzing radiosonde data specifically collected for such evaluation applied to a tropical area, namely the city of Rio de Janeiro, Brazil. In that context, we applied a method recommended by previously reviewed literature consisting of replacing air temperature of a sounding probe launched in the morning (12 UTC) with forecasted values using data observed in the afternoon in order to gauge the method. Data points measured by radiosondes launched in the afternoon (between 12 and 7 pm local time) were used to evaluate the proposed method. The results showed that the atmosphere presented the highest heating rates in the atmospheric layer closest to the surface during the afternoon for diurnal clouds (DC) days. Similar behaviour was observed for the days of the South Atlantic Convergence Zone (SACZ). For days with frontal system (FS) presence, however, lower temperature values were observed in the afternoon in relation to the measured by morning soundings. Winds presented northeast and southwest components leading to the occurrence of warm and cold advection, respectively, in the analyzed region. Thermodynamic variables tended to be overestimated in relation to observed field results in most of the analyzed days. |
Databáze: | OpenAIRE |
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