Climate Data for Latitude 37.75 Longitude 21.75

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

Locations

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Mount Erimanthos
Mount Foloi
OLYMPIA
OROPEDIO FOLOIS
OROS ERYMANTHOS
THALASSIA PERIOCHI KOLPOU KYPARISSIAS: AKR. KATAKOLO - KYPARISSIA
THINES KAI PARALIAKO DASOS ZACHAROS, LIMNI KAIAFA, STROFYLIA, KAKOVATOS

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min Temp38.238.640.945.351.357.762.162.858.152.646.541.1109 years
Mean Temp45.546.249.454.661.969.173.674.369.162.254.848.3109 years
Max Temp53.054.058.164.172.780.685.386.080.271.963.055.6109 years
FrostDays12.810.410.92.73.50.31.60.21.51.65.112.2109 years
WetDays10.09.28.36.66.53.02.01.42.45.68.211.3109 years
Precipitationin4.43.52.81.90.90.50.30.30.93.65.15.5108 years
Potential Evapotranspirationin1.11.52.43.24.55.76.65.94.12.51.41.0109 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 37.75 Longitude 21.75
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 37.75 Longitude 21.75
Yearly Total Frost Days 1901 - 2009 Latitude 37.75 Longitude 21.75
Yearly Total Precipitation 1901 - 2009 (English) Latitude 37.75 Longitude 21.75
Yearly Total Wet Days 1901 - 2009 Latitude 37.75 Longitude 21.75
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude 37.75 Longitude 21.75

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.