Climate Data for Latitude -25.75 Longitude -54.25

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

Locations

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Parque Nacional do Iguaçu
Parque Nacional Iguazú
Parque Nacional Iguazú y alrededores
Parque Provincial Urugua-í
Parque Provincial Uruzú y Reserva Forestal San Jorge
Urugua-í Provincial Park

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min Temp67.467.565.159.653.950.849.652.055.358.862.365.8109 years
Mean Temp78.277.775.769.963.860.660.363.466.570.474.077.1109 years
Max Temp89.088.086.580.373.970.571.174.977.882.085.988.5109 years
FrostDays3.05.02.05.67.54.64.11.74.04.12.06.02 years
WetDays14.615.610.37.37.16.25.26.99.411.910.011.0109 years
Precipitationin6.46.04.95.96.65.44.44.15.07.76.15.4109 years
Potential Evapotranspirationin5.24.34.13.22.21.72.22.83.34.55.25.8109 years
Yearly Average Temperatures 1901 - 2009 (English) Latitude -25.75 Longitude -54.25
Monthly Mean Temperatures 1901 - 2009 (English) Latitude -25.75 Longitude -54.25
Yearly Total Frost Days 1913 - 2009 Latitude -25.75 Longitude -54.25
Yearly Total Precipitation 1901 - 2009 (English) Latitude -25.75 Longitude -54.25
Yearly Total Wet Days 1901 - 2009 Latitude -25.75 Longitude -54.25
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude -25.75 Longitude -54.25

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.