Climate Data for Latitude 59.25 Longitude 14.25

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

Locations

Download
Åråsviken-Vallholmen
Åråsvikens norra skärgård
Bay of Kilsviken
Fisksjön
Gullspångsälven
Inre Kilsviken
Nötön-Åråsviken
Östra Sälsjömossen
Vargavidderna
Värmlands Säby
Visnums stormosse

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min TempF°19.018.022.630.238.845.850.448.542.535.928.521.7108 years
Mean TempF°24.524.830.639.549.756.861.058.751.142.433.527.1109 years
Max TempF°29.731.338.648.860.767.771.669.059.849.038.432.4107 years
FrostDays31.028.231.030.025.913.80.63.812.430.230.031.0109 years
WetDays17.812.711.410.59.810.312.212.113.013.716.916.7109 years
Precipitationin1.51.11.21.51.72.32.73.32.42.42.21.8109 years
Potential Evapotranspirationin0.20.41.22.33.94.34.33.61.90.60.20.24 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 59.25 Longitude 14.25
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 59.25 Longitude 14.25
Yearly Total Frost Days 1901 - 2009 Latitude 59.25 Longitude 14.25
Yearly Total Precipitation 1901 - 2009 (English) Latitude 59.25 Longitude 14.25
Yearly Total Wet Days 1901 - 2009 Latitude 59.25 Longitude 14.25
Yearly Total Potential Evapotranspiration 1912 - 2009 (English) Latitude 59.25 Longitude 14.25

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.