Climate Data for Latitude 60.25 Longitude 18.25

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

Locations

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Ängskär, Bondskäret
Aspdalssjön
Björnsundet-Storkärren
Blåkulla
Borgskogen
Bruksdammen
Dansbol
Edskärret
Ekbäcken-Jämnbromossen
Fagerön
Forsmarksbruk
Grundsjön
Kallriga
Kavarö
Klövängen
Långalma
Mässmyrfallet
Olas skifte
Skaten-Rångsen
Vickelsjön

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min Temp22.820.824.331.639.948.955.354.347.539.932.926.9105 years
Mean Temp27.025.529.937.747.055.961.659.952.744.136.330.5109 years
Max Temp30.930.235.543.854.263.067.965.658.048.339.634.0105 years
FrostDays31.028.331.030.018.97.73.03.33.022.429.931.048 years
WetDays16.711.610.69.37.28.611.013.414.712.817.716.3109 years
Precipitationin1.41.00.91.21.21.52.12.82.01.81.91.6109 years
Potential Evapotranspirationin0.30.41.01.83.34.24.33.31.91.10.50.462 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 60.25 Longitude 18.25
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 60.25 Longitude 18.25
Yearly Total Frost Days 1902 - 2009 Latitude 60.25 Longitude 18.25
Yearly Total Precipitation 1901 - 2009 (English) Latitude 60.25 Longitude 18.25
Yearly Total Wet Days 1901 - 2009 Latitude 60.25 Longitude 18.25
Yearly Total Potential Evapotranspiration 1903 - 2009 (English) Latitude 60.25 Longitude 18.25

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.