Climate Data for Latitude 39.75 Longitude 20.25

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

Locations

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Area of Oriokastro, Lake Delvinaki, Meropis forest, Gormou valley and Mounts Kasidiaris and Douskon
Kalamas estuary
Kalamas gorge
Mount Paramithias
Mounts Tsamanta, Filiaton, Pharmakovouni, and Megali Rahi
ORI TSAMANTA, FILIATON, FARMAKOVOUNI, MEGALI RACHI
OROS DOUSKON, ORAIOKASTRO, DASOS MEROPIS, KOILADA GORMOU, LIMNI DELVINAKIOU
STENA PARAKALAMOU
YGROTOPOS EKVOLON KALAMA KAI NISOS PRASOUDI

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min Temp35.036.540.245.552.058.061.762.156.950.744.038.0108 years
Mean Temp42.744.749.355.263.069.974.775.168.760.852.445.6109 years
Max Temp50.552.958.465.074.181.987.988.380.670.960.953.2109 years
FrostDays20.415.712.44.22.11.01.03.06.05.317.115.91 years
WetDays12.010.910.810.78.44.72.82.53.27.612.413.2109 years
Precipitationin6.65.84.03.42.00.80.50.62.55.47.18.2109 years
Potential Evapotranspirationin0.91.32.23.14.55.66.75.83.82.11.10.8109 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 39.75 Longitude 20.25
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 39.75 Longitude 20.25
Yearly Total Frost Days 1978 - 2009 Latitude 39.75 Longitude 20.25
Yearly Total Precipitation 1901 - 2009 (English) Latitude 39.75 Longitude 20.25
Yearly Total Wet Days 1901 - 2009 Latitude 39.75 Longitude 20.25
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude 39.75 Longitude 20.25

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.