Climate Data for Latitude 56.75 Longitude 16.75

Köppen climate classification: Cfb (Climate: warm temperate; Precipitation: fully humid; Temperature: warm summer)
 

Locations

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Åkerby-Runstens sjömarker
Äleklintabrottet
Björnsbodar
Borga hage
Coastal areas of eastern Öland island
Djurstadträsk
Egby sjömarker
Gårdby sandstäpp
Gillsättra
Halltorp
Husvalla sjömarker
Ismanstorp
Jordtorpsåsen
Kapelludden
Karås
Karum
Lenstad-Tävelsrum
Petgärde träsk
Rönnerum-Abbantorp
Rösselkärret
Ryd
Skede mosse
Slottsalvaret
Störlinge sjömarker
Strandtorp
Vanserum-Bäck-Övetorp

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min TempF°26.125.228.234.441.449.454.653.948.341.334.629.0107 years
Mean TempF°30.229.833.841.249.857.462.561.555.146.838.833.0109 years
Max TempF°34.334.339.448.158.365.770.569.362.152.443.137.0108 years
FrostDays31.028.031.030.019.39.01.05.76.220.830.031.02 years
WetDays17.212.010.68.87.97.710.410.712.112.420.917.0109 years
Precipitationin1.31.01.01.11.31.52.12.21.81.51.71.6109 years
Potential Evapotranspirationin0.30.51.12.13.54.14.23.52.21.10.40.353 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 56.75 Longitude 16.75
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 56.75 Longitude 16.75
Yearly Total Frost Days 1902 - 2009 Latitude 56.75 Longitude 16.75
Yearly Total Precipitation 1901 - 2009 (English) Latitude 56.75 Longitude 16.75
Yearly Total Wet Days 1901 - 2009 Latitude 56.75 Longitude 16.75
Yearly Total Potential Evapotranspiration 1902 - 2009 (English) Latitude 56.75 Longitude 16.75

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.