Climate Data for Latitude 37.25 Longitude 15.25

Köppen climate classification: Csa (Climate: warm temperate; Precipitation: summer dry; Temperature: hot summer)
 

Locations

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Biviere di Lentini, tratto mediano e foce del Fiume Simeto e area antistante la foce
Saline di Augusta
Saline di Priolo
Saline di Siracusa e Fiume Ciane
Simeto mouth and middle course and Biviere di Lentini

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min Temp46.447.049.452.758.765.570.671.768.161.955.249.1109 years
Mean Temp51.152.054.958.565.072.277.678.474.167.460.353.8109 years
Max Temp55.957.260.464.471.479.184.685.380.172.965.458.4109 years
FrostDays13.613.70.52.05.01.04.06.02.06.08.04.11 years
WetDays13.09.38.25.93.21.50.60.92.76.99.411.1109 years
Precipitationin3.62.11.81.10.50.20.20.31.23.53.73.8109 years
Potential Evapotranspirationin1.51.82.73.54.86.07.16.44.53.02.01.4109 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 37.25 Longitude 15.25
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 37.25 Longitude 15.25
Yearly Total Frost Days 1954 - 2009 Latitude 37.25 Longitude 15.25
Yearly Total Precipitation 1901 - 2009 (English) Latitude 37.25 Longitude 15.25
Yearly Total Wet Days 1901 - 2009 Latitude 37.25 Longitude 15.25
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude 37.25 Longitude 15.25

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.