Abstract
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.
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Acknowledgements
The authors would like to thank the Civil Engineering Program of the Alberto Luiz Coimbra Institute of Postgraduate Studies and Research in Engineering (COPPE)—part of the Universidade Federal do Rio de Janeiro (UFRJ)—for their support, particularly offered through the Laboratory of Water Resources and Environmental Studies (LABH2O), as well as the Meteorology and Atmospheric Physics editorial board for their revisions. The authors would also like to recognize the support of the Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES), which helped fund this work through CAPES Call 27/2013—Pró-Equipamentos Institucional and CAPES/MEC Call No. 03/2015—BRICS; we further thank the Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq), which helped fund this work through CNPq Universal Call for Papers No. 14/2013—Proceeding No. 485136/2013-9 and CNPq Call No. 12/2016—Proceeding No. 306944/2016-2; the National Secretariat of Higher Education (SESu)—part of the Ministry of Education (MEC) (2010–2016) (PET CIVIL UFRJ); the Fundação de Amparo à Pesquisa do Estado do Rio de Janeiro (FAPERJ), which helped fund this work through Project FAPERJ—Pensa RiovCall 34/2014 (2014–2018)—E-26/010.002980/2014, FAPERJ No. E_12/2015 and FAPERJ nº E-22/2016; as well as the Brazilian Ministry of Science and Technology (MCT), through its Financier of Studies and Projects (FINEP) and in particular its CT-HIDRO Fund (2005–2016), which is focused on researching rainfall–runoff and atmospheric modeling, water and energy balances, and extreme flood and drought events. This study was financed in part by the Coordenação de Aperfeiçoamento de Pessoal de Nível Superior- Brasil (CAPES)—Finance Code 001.
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da Silva, F.P., Rotunno Filho, O.C., Justi da Silva, M.G.A. et al. Observed and estimated atmospheric thermodynamic instability using radiosonde observations over the city of Rio de Janeiro, Brazil. Meteorol Atmos Phys 132, 297–314 (2020). https://doi.org/10.1007/s00703-019-00688-3
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DOI: https://doi.org/10.1007/s00703-019-00688-3