Climate Data for Latitude -25.25 Longitude -48.75

Köppen climate classification: Cfa (Climate: warm temperate; Precipitation: fully humid; Temperature: hot summer)
 

Locations

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Baixo Curso do Rio Nhundiaquara
Pico Paraná State Park
Roberto Ribas Lange State Park
Serra da Baitaca State Park
Serra do Mar State Environmental Protection Area
Serra do Marumbi

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min TempF°63.363.362.558.653.550.549.751.553.156.058.060.8109 years
Mean TempF°71.871.670.967.062.559.458.660.761.064.166.068.7109 years
Max TempF°80.479.979.375.571.668.567.770.069.072.374.176.7109 years
FrostDays4.94.93.72.08.45.54.33.74.52.24.93.3109 years
WetDays28.526.327.617.114.413.012.013.718.726.125.428.1109 years
Precipitationin8.97.67.33.74.03.53.12.94.55.24.86.0109 years
Potential Evapotranspirationin4.13.53.52.72.21.92.02.52.83.43.83.9109 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude -25.25 Longitude -48.75
Monthly Mean Temperatures 1901 - 2009 (English) Latitude -25.25 Longitude -48.75
Yearly Total Frost Days 1901 - 2009 Latitude -25.25 Longitude -48.75
Yearly Total Precipitation 1901 - 2009 (English) Latitude -25.25 Longitude -48.75
Yearly Total Wet Days 1901 - 2009 Latitude -25.25 Longitude -48.75
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude -25.25 Longitude -48.75

Climate data provided by CRU TS 3.1 - University of East Anglia Climate Research Unit (CRU). [Phil Jones, Ian Harris]. CRU Time Series (TS) high resolution gridded datasets, [Internet]. NCAS British Atmospheric Data Centre, 2008, Accessed: 28-July-2011
Charting software provided by pChart - a PHP class to build charts.
Köppen climate classification provided by Kottek, M., J. Grieser, C. Beck, B. Rudolf, and F. Rubel, 2006: World Map of Köppen-Geiger Climate Classification updated. Meteorol. Z., 15, 259-263
The calculation method for the potential evapotranspiration is the FAO grass reference equation (Ekstrom et al., 2007, which is based on Allen et al., 1994). It is a variant of the Penman Monteith method using TMP, TMN, TMX, VAP, CLD.