Climate Data for Latitude 55.25 Longitude 10.25

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

Locations

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Arreskov Sø
Arreskov Sø
Odense Å med Hågerup Å, Sallinge Å og Lindved Å
Odense Fjord
Skove og søer syd for Brahetrolleborg
Skove ved Brahetrolleborg
Svanninge Bakker
Vestlige del af Avernakø

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min Temp29.528.831.836.944.350.254.154.249.844.037.532.1103 years
Mean Temp33.133.036.643.451.757.861.461.355.948.941.335.8109 years
Max Temp36.837.041.449.959.265.568.868.462.253.845.339.4109 years
FrostDays30.628.330.815.814.710.62.05.26.516.520.129.815 years
WetDays17.511.313.211.710.49.711.611.212.013.417.916.2109 years
Precipitationin1.91.41.41.41.62.02.42.62.12.42.42.0109 years
Potential Evapotranspirationin0.40.51.01.93.23.83.83.42.11.20.60.482 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 55.25 Longitude 10.25
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 55.25 Longitude 10.25
Yearly Total Frost Days 1902 - 2009 Latitude 55.25 Longitude 10.25
Yearly Total Precipitation 1901 - 2009 (English) Latitude 55.25 Longitude 10.25
Yearly Total Wet Days 1901 - 2009 Latitude 55.25 Longitude 10.25
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude 55.25 Longitude 10.25

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.