2012
DOI: 10.1007/s00704-012-0668-0
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Urban climate and clues of heat island events in the metropolitan area of Rio de Janeiro

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Cited by 44 publications
(32 citation statements)
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“…For instance, the urban area of Campinas increased from 12.3 km 2 in 1940 to 197.1 km 2 in 1990. In contrast, the city of Rio de Janeiro started to grow in the middle of the 19th century and the increase of urban area is more pronounced in the beginning of the 20th century, being less significant after the middle of the 20th century [ Marenga , ; Lucena et al ., ]. This difference can be seen by the population of cities in the beginning of the 20th century, because the urban area of a given city is linked to the size of its population, as suggested by Oke [].…”
Section: Thunderstorm Day Observations In Southeast Brazilmentioning
confidence: 99%
“…For instance, the urban area of Campinas increased from 12.3 km 2 in 1940 to 197.1 km 2 in 1990. In contrast, the city of Rio de Janeiro started to grow in the middle of the 19th century and the increase of urban area is more pronounced in the beginning of the 20th century, being less significant after the middle of the 20th century [ Marenga , ; Lucena et al ., ]. This difference can be seen by the population of cities in the beginning of the 20th century, because the urban area of a given city is linked to the size of its population, as suggested by Oke [].…”
Section: Thunderstorm Day Observations In Southeast Brazilmentioning
confidence: 99%
“…With one of the world's largest economies and the Amazon as the planet's biggest ecosystem, Brazil indicates a high vulnerability to the impacts of climate change. During the past decades, Brazil was confronted with an uprising trend in minimum and overall surface temperature, especially targeting urbanized areas (Lucena et al, 2013), and was challenged by one of the strongest El Niño Southern Oscillation events that occurred in 2015/2016 (Caminade et al, 2017). In the future, a further rise in warming trends and an increase in the occurrence of weather extremes like floods or droughts are presumed (WHO, 2015).…”
Section: Climatic Change Climate Variability and The Spread Of Neglementioning
confidence: 99%
“…This is a system of semipermanent high pressure, characterized by the presence of horizontal synoptic winds that rotate counterclockwise, vertical subsidence wind that generates divergence near the surface, clear sky, calm weather, and stable conditions, such that the SASA location and intensity change seasonally (Richter et al, 2008;Zeri et al, 2011). The influence of the SASA contributes to inhibit cloudiness and the advancement of high-latitude frontal systems in the region of interest (Lucena et al, 2012). Meteorological mesoscale and microscale systems, such as the sea breezes that act in the MARJ, can be hidden by the SASA system, but they are not totally destroyed as is the case when fronts pass by the area.…”
Section: Site Characterization Period Synoptic Analysis and Surface mentioning
confidence: 99%