Climate Data for Latitude 56.25 Longitude 13.25

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

Locations

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Århultsbäcken
Åstarpe mosse
Brandeborg
Djurholmamossen
Gällabjär
Herrevadskloster
Klinta hallar
Klövabäcken
Lärkesholmssjön
Liaängen
Linneröd
Såghuslund
Smedjebacken
Söderåsen
Traneröds mosse
Uggleskogen
Vallåsen DR
Värsjön
Vindrarp

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min TempF°25.324.728.534.041.348.352.951.846.540.433.928.7107 years
Mean TempF°29.929.734.742.451.557.961.760.654.146.438.432.9109 years
Max TempF°34.534.841.051.061.867.670.769.661.952.442.837.2107 years
FrostDays31.028.231.027.117.08.30.23.07.224.128.931.0109 years
WetDays20.912.113.011.610.811.613.314.113.814.718.218.3109 years
Precipitationin2.41.61.71.71.72.43.33.12.82.82.72.7109 years
Potential Evapotranspirationin0.20.41.22.23.64.14.13.32.00.90.30.231 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 56.25 Longitude 13.25
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 56.25 Longitude 13.25
Yearly Total Frost Days 1901 - 2009 Latitude 56.25 Longitude 13.25
Yearly Total Precipitation 1901 - 2009 (English) Latitude 56.25 Longitude 13.25
Yearly Total Wet Days 1901 - 2009 Latitude 56.25 Longitude 13.25
Yearly Total Potential Evapotranspiration 1902 - 2009 (English) Latitude 56.25 Longitude 13.25

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.