Climate Data for Latitude 59.75 Longitude 16.25

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

Locations

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Askö-Tidö
Djupebo
Fermansbo urskog
Fläckebo
Fläcksjön
Gnien
Gorgen
Gussjön
Häggholmen
Höskovsmossen
Lia
Nötmyran
Överskälby
River Svartån
Rörbosjön
Rövallsmossen och Stingsmossen
Strömsholm
Vitmossen
Vrenninge

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min TempF°19.218.523.030.538.245.650.649.242.535.628.722.9103 years
Mean TempF°24.624.830.538.948.455.460.058.250.441.633.127.5108 years
Max TempF°29.730.937.847.458.765.469.667.458.347.637.532.2106 years
FrostDays31.028.231.030.028.711.20.92.813.130.730.031.0109 years
WetDays15.711.110.69.68.79.312.813.113.412.516.615.0109 years
Precipitationin1.41.01.01.31.52.22.93.02.22.01.91.7109 years
Potential Evapotranspirationin0.10.41.22.33.63.83.53.41.80.40.10.22 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 59.75 Longitude 16.25
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 59.75 Longitude 16.25
Yearly Total Frost Days 1901 - 2009 Latitude 59.75 Longitude 16.25
Yearly Total Precipitation 1901 - 2009 (English) Latitude 59.75 Longitude 16.25
Yearly Total Wet Days 1901 - 2009 Latitude 59.75 Longitude 16.25
Yearly Total Potential Evapotranspiration 1938 - 2009 (English) Latitude 59.75 Longitude 16.25

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.