Temporal variability of the Buenos Aires, Argentina, urban heat island

This paper describes the statistical characteristics and temporal variability of the urban heat island (UHI) intensity in Buenos Aires using 32-year surface meteorological data with 1-h time intervals. Seasonal analyses show that the UHI intensity is strongest during summer months and an "inver...

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Autor principal: Camilloni, I.
Otros Autores: Barrucand, M.
Formato: Capítulo de libro
Lenguaje:Inglés
Publicado: Springer-Verlag Wien 2012
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100 1 |a Camilloni, I. 
245 1 0 |a Temporal variability of the Buenos Aires, Argentina, urban heat island 
260 |b Springer-Verlag Wien  |c 2012 
270 1 0 |m Camilloni, I.; Departamento de Ciencias de la Atmósfera y los Océanos, Facultad de Ciencias Exactas y Naturales, Centro de Investigaciones del Mar y la Atmósfera, Universidad de Buenos Aires-Consejo Nacional de Investigaciones Científicas y Técnicas, Buenos Aires, Argentina; email: ines@cima.fcen.uba.ar 
506 |2 openaire  |e Política editorial 
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520 3 |a This paper describes the statistical characteristics and temporal variability of the urban heat island (UHI) intensity in Buenos Aires using 32-year surface meteorological data with 1-h time intervals. Seasonal analyses show that the UHI intensity is strongest during summer months and an "inverse" effect is found frequently during the afternoon hours of the same season. During winter, the UHI effect is in the minimal. The interannual trend and the seasonal variation of the UHI for the main synoptic hours for a longer record of 48 years are studied and associated to changes in meteorological factors as low-level circulation and cloud amount. Despite the population growth, it was found a negative trend in the nocturnal UHI intensity that could be explained by a decline of near clear-sky conditions, a negative trend in the calm frequencies and an increase in wind speed. Urban to rural temperature differences and rural temperatures are negatively correlated for diurnal and nocturnal hours both for annual and seasonal scales. This result is due to the lower interannual variability of urban temperatures in comparison to rural ones. © 2011 Springer-Verlag.  |l eng 
593 |a Departamento de Ciencias de la Atmósfera y los Océanos, Facultad de Ciencias Exactas y Naturales, Centro de Investigaciones del Mar y la Atmósfera, Universidad de Buenos Aires-Consejo Nacional de Investigaciones Científicas y Técnicas, Buenos Aires, Argentina 
593 |a Departamento de Ciencias de la Atmósfera y los Océanos, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires-Consejo Nacional de Investigaciones Científicas y Técnicas, Buenos Aires, Argentina 
690 1 0 |a AIR TEMPERATURE 
690 1 0 |a ANNUAL VARIATION 
690 1 0 |a ATMOSPHERIC CIRCULATION 
690 1 0 |a DIURNAL VARIATION 
690 1 0 |a HEAT ISLAND 
690 1 0 |a SEASONAL VARIATION 
690 1 0 |a STATISTICAL ANALYSIS 
690 1 0 |a TEMPORAL VARIATION 
651 4 |a ARGENTINA 
651 4 |a BUENOS AIRES [ARGENTINA] 
700 1 |a Barrucand, M. 
773 0 |d Springer-Verlag Wien, 2012  |g v. 107  |h pp. 47-58  |k n. 1-2  |p Theor. Appl. Climatol.  |x 0177798X  |w (AR-BaUEN)CENRE-7012  |t Theoretical and Applied Climatology 
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