Climate Data for Latitude 45.25 Longitude 11.25

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

Locations

Download
Boscone island
Isola Boscone
Palude del Brusà - Le Vallette
Palude del Busatello
Palude del Feniletto - Sguazzo del Vallese
Palude di Pellegrina
Paludi di Ostiglia
Sguazzo di Rivalunga

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min TempF°27.230.437.144.151.858.862.261.955.647.037.829.5107 years
Mean TempF°33.738.246.053.561.868.872.571.965.155.444.335.6108 years
Max TempF°40.246.054.962.971.778.982.882.074.663.950.841.8108 years
FrostDays31.028.220.88.73.72.36.82.67.613.726.831.0109 years
WetDays8.98.29.710.512.210.97.49.17.98.610.69.1109 years
Precipitationin1.71.61.92.32.82.92.12.52.53.22.92.0109 years
Potential Evapotranspirationin0.40.81.82.84.14.85.34.62.91.50.60.3109 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 45.25 Longitude 11.25
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 45.25 Longitude 11.25
Yearly Total Frost Days 1901 - 2009 Latitude 45.25 Longitude 11.25
Yearly Total Precipitation 1901 - 2009 (English) Latitude 45.25 Longitude 11.25
Yearly Total Wet Days 1901 - 2009 Latitude 45.25 Longitude 11.25
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude 45.25 Longitude 11.25

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.