Climate Data for Latitude 50.25 Longitude 10.25

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

Locations

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Bayerische Hohe Rhön
Grenzstreifen am Galgenberg - Milzgrund - Warthügel
Haßbergetrauf und Bundorfer Wald
Laubwälder und Magerrasen im Grabfeldgau

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min TempF°24.825.731.237.245.250.453.953.147.239.833.328.0102 years
Mean TempF°30.032.139.146.354.860.163.262.356.247.238.332.4108 years
Max TempF°35.038.446.955.464.569.872.671.665.254.743.436.9108 years
FrostDays31.028.230.814.53.91.70.60.65.418.627.531.0109 years
WetDays17.614.313.813.714.914.114.114.412.111.714.816.5109 years
Precipitationin1.61.41.61.72.42.82.82.51.91.71.71.8109 years
Potential Evapotranspirationin0.30.61.52.43.64.04.33.62.31.20.60.374 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 50.25 Longitude 10.25
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 50.25 Longitude 10.25
Yearly Total Frost Days 1901 - 2009 Latitude 50.25 Longitude 10.25
Yearly Total Precipitation 1901 - 2009 (English) Latitude 50.25 Longitude 10.25
Yearly Total Wet Days 1901 - 2009 Latitude 50.25 Longitude 10.25
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude 50.25 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.