Climate Data for Latitude 50.75 Longitude 7.75

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

Locations

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Brölbach
Eulenbruchs Wald
Heiden und Magerrasen Trupbach
Kesselsiefen u. Galgenberg
Quellmoor bei Neuenhähnen
Rosbachtal
Steinbruch Imhausen
Stollen bei Morsbach-Schlechtingen
Wiesen bei Dreisel

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min Temp28.929.733.939.046.251.054.553.949.342.635.830.8103 years
Mean Temp33.034.640.647.155.059.963.162.457.048.840.134.8109 years
Max Temp37.339.747.455.363.869.071.970.964.955.044.438.7109 years
FrostDays31.028.227.012.13.25.72.95.96.714.023.530.9109 years
WetDays17.913.115.715.815.715.515.415.014.914.115.917.7109 years
Precipitationin2.52.02.12.12.32.93.12.92.42.32.52.7109 years
Potential Evapotranspirationin0.40.71.62.63.63.94.23.62.31.30.60.4100 years
Yearly Average Temperatures 1901 - 2009 (English) Latitude 50.75 Longitude 7.75
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 50.75 Longitude 7.75
Yearly Total Frost Days 1901 - 2009 Latitude 50.75 Longitude 7.75
Yearly Total Precipitation 1901 - 2009 (English) Latitude 50.75 Longitude 7.75
Yearly Total Wet Days 1901 - 2009 Latitude 50.75 Longitude 7.75
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude 50.75 Longitude 7.75

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.