Climate Data for Latitude 55.25 Longitude 10.75

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

Locations

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Kajbjerg Skov
Odense Fjord
Sprogø and Halsskov Rev
Søer ved Tårup og Klintholm
Urup Dam, Brabæk Mose, Birkende Mose og Illemose
Vresen and sea area between Fyn and Langeland

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min TempF°30.329.632.338.045.851.956.256.351.945.639.033.5105 years
Mean TempF°33.533.036.443.251.758.062.061.656.549.442.136.5109 years
Max TempF°36.736.340.548.657.864.267.967.161.353.545.339.6108 years
FrostDays30.828.231.014.814.99.11.95.63.715.016.928.89 years
WetDays17.711.513.311.710.410.212.111.712.213.918.015.8109 years
Precipitationin1.71.21.31.31.51.82.32.32.12.22.31.8109 years
Potential Evapotranspirationin0.50.51.01.93.23.73.93.42.21.20.70.592 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 55.25 Longitude 10.75
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 55.25 Longitude 10.75
Yearly Total Frost Days 1902 - 2009 Latitude 55.25 Longitude 10.75
Yearly Total Precipitation 1901 - 2009 (English) Latitude 55.25 Longitude 10.75
Yearly Total Wet Days 1901 - 2009 Latitude 55.25 Longitude 10.75
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude 55.25 Longitude 10.75

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.