Climate Data for Latitude 40.75 Longitude 21.25

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

Locations

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ETHNIKOS DRYMOS PRESPON
Lake Kastoria (Orestiada)
Lake Mikri Prespa
Lake Mikri Prespa and Lake Megali Prespa
Lake Prespa
LIMNI KASTORIAS
ORI VARNOUNTA
OROS VERNON - KORYFI VITSI
Prespa National Park

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min Temp22.624.529.936.844.249.954.354.148.440.633.226.3105 years
Mean Temp29.231.938.446.154.761.266.466.259.450.040.932.8108 years
Max Temp35.939.446.955.665.272.678.578.570.659.448.639.3107 years
FrostDays31.028.230.28.13.01.81.00.43.16.223.431.0109 years
WetDays10.89.610.411.410.67.44.63.94.07.010.711.3109 years
Precipitationin2.71.82.12.22.61.61.41.11.52.83.33.3109 years
Potential Evapotranspirationin0.81.11.92.94.04.85.65.03.32.01.10.8109 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 40.75 Longitude 21.25
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 40.75 Longitude 21.25
Yearly Total Frost Days 1901 - 2009 Latitude 40.75 Longitude 21.25
Yearly Total Precipitation 1901 - 2009 (English) Latitude 40.75 Longitude 21.25
Yearly Total Wet Days 1901 - 2009 Latitude 40.75 Longitude 21.25
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude 40.75 Longitude 21.25

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.