Climate Data for Latitude 58.25 Longitude 22.75

Köppen climate classification: Dfb (Climate: snow; Precipitation: fully humid; Temperature: warm summer)
 

Locations

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Allirahu
Kalli soo
Kasti bay
Kasti lahe
Koigi
Koigi
Põduste-Upa
Siiksaare-Oessaare
Siiksaare-Oessaare bays
Sutu bay
Sutu lahe
Tahula-Reo
Võrsna
West Estonian Archipelago Biosphere Reserve

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min TempF°23.721.724.933.140.949.956.356.048.841.334.027.9105 years
Mean TempF°27.625.929.738.447.556.162.161.454.145.437.431.5109 years
Max TempF°31.330.034.643.854.262.568.166.859.549.740.835.0108 years
FrostDays31.028.031.030.019.68.02.02.05.525.230.031.01 years
WetDays18.513.112.19.59.49.611.112.416.915.721.819.5109 years
Precipitationin1.51.11.11.21.31.62.62.72.62.52.31.8109 years
Potential Evapotranspirationin0.40.40.81.73.03.83.93.11.81.00.50.496 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 58.25 Longitude 22.75
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 58.25 Longitude 22.75
Yearly Total Frost Days 1902 - 2009 Latitude 58.25 Longitude 22.75
Yearly Total Precipitation 1901 - 2009 (English) Latitude 58.25 Longitude 22.75
Yearly Total Wet Days 1901 - 2009 Latitude 58.25 Longitude 22.75
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude 58.25 Longitude 22.75

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.