Climate Data for Latitude 45.75 Longitude 11.75

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

Locations

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Campazzi di Onigo
Ex Cave di Casale - Vicenza
Grave e Zone umide della Brenta
Massiccio del Grappa
Middle course of River Brenta
Mount Grappa
Prai di Castello di Godego
Settolo Basso

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min TempF°24.527.033.240.047.454.257.157.051.242.734.326.5106 years
Mean TempF°31.334.741.748.756.463.266.666.260.050.940.933.2109 years
Max TempF°38.142.450.157.465.772.576.275.668.959.247.639.8108 years
FrostDays31.028.228.115.08.54.65.64.58.917.729.231.0109 years
WetDays9.18.310.611.914.013.410.911.59.49.410.49.2109 years
Precipitationin2.01.92.32.83.43.73.33.43.23.63.42.3109 years
Potential Evapotranspirationin0.50.81.62.43.64.24.54.02.61.40.50.4109 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 45.75 Longitude 11.75
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 45.75 Longitude 11.75
Yearly Total Frost Days 1901 - 2009 Latitude 45.75 Longitude 11.75
Yearly Total Precipitation 1901 - 2009 (English) Latitude 45.75 Longitude 11.75
Yearly Total Wet Days 1901 - 2009 Latitude 45.75 Longitude 11.75
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude 45.75 Longitude 11.75

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.