Climate Data for Latitude 58.75 Longitude 12.25

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

Locations

Download
Baståsen
Gålsjön
Högsbyn
Kabbo
Kroppefjäll
Liden
Lunnebo
Norra Båsane
Öjemossen
Råvarp
Runnsäter
Ryrs naturreservat
Skärbo
Skitne Väner
Skvalarn
Sörknatten
Stommebäcken
Tingvallamossen

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min TempF°20.820.324.531.539.647.051.349.944.537.629.923.8104 years
Mean TempF°25.926.331.639.949.857.061.059.152.043.534.929.0109 years
Max TempF°31.032.238.748.359.967.070.768.359.649.439.633.8107 years
FrostDays31.028.231.030.021.59.90.52.39.328.230.031.0109 years
WetDays19.112.912.211.010.812.412.413.714.215.617.317.3109 years
Precipitationin2.31.51.61.71.82.42.83.33.03.53.22.6109 years
Potential Evapotranspirationin0.30.41.22.23.64.54.53.32.00.80.30.211 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 58.75 Longitude 12.25
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 58.75 Longitude 12.25
Yearly Total Frost Days 1901 - 2009 Latitude 58.75 Longitude 12.25
Yearly Total Precipitation 1901 - 2009 (English) Latitude 58.75 Longitude 12.25
Yearly Total Wet Days 1901 - 2009 Latitude 58.75 Longitude 12.25
Yearly Total Potential Evapotranspiration 1912 - 2009 (English) Latitude 58.75 Longitude 12.25

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.