Climate Data for Latitude 59.75 Longitude 18.75

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

Locations

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Ålandet
Ängsö
Bellberget
Björinge
Borudamyren
Edsbro Kyrksjö
Hamnudden
Karlsdalsmossen
Långsjön
Malmsjön
Mossbottnarna
Norra Malma
Råda
Rimsjöskogen
Rörvik
Samnäsfjärden
Södra Råda
Ströjan
Svartkärret

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min TempF°24.422.325.532.140.349.156.055.448.841.334.128.0104 years
Mean TempF°28.226.530.437.646.455.361.560.453.445.037.331.6109 years
Max TempF°31.830.435.143.052.561.567.065.457.948.740.435.0104 years
FrostDays31.028.331.029.716.88.43.01.02.119.328.831.048 years
WetDays17.713.010.99.57.28.810.912.814.713.318.317.0109 years
Precipitationin1.31.00.91.11.01.42.02.51.81.81.91.5109 years
Potential Evapotranspirationin0.30.41.01.73.14.04.23.32.01.20.60.478 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 59.75 Longitude 18.75
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 59.75 Longitude 18.75
Yearly Total Frost Days 1902 - 2009 Latitude 59.75 Longitude 18.75
Yearly Total Precipitation 1901 - 2009 (English) Latitude 59.75 Longitude 18.75
Yearly Total Wet Days 1901 - 2009 Latitude 59.75 Longitude 18.75
Yearly Total Potential Evapotranspiration 1903 - 2009 (English) Latitude 59.75 Longitude 18.75

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.