Climate Data for Latitude 53.25 Longitude 10.75

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

Locations

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Drawehn
Kammmolch-Biotop Mührgehege/Oetzendorf
Langenlehsten
Lohn
Nüssauer Heide
Ostheide bei Himbergen und Bad Bodenteich
Rotbauchunken-Vorkommen Strothe/Almstorf
Stecknitz-Delvenau

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min TempF°28.729.132.938.345.951.755.655.350.243.036.731.6103 years
Mean TempF°33.133.938.945.754.159.563.362.857.349.041.035.3108 years
Max TempF°37.338.745.053.262.467.571.070.564.455.045.239.1109 years
FrostDays30.628.230.313.95.54.60.20.10.913.923.330.5109 years
WetDays17.812.912.613.011.913.414.615.112.412.215.816.6109 years
Precipitationin1.91.41.71.72.12.52.92.72.21.92.12.1109 years
Potential Evapotranspirationin0.40.61.32.33.64.04.23.62.31.20.60.484 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 53.25 Longitude 10.75
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 53.25 Longitude 10.75
Yearly Total Frost Days 1901 - 2009 Latitude 53.25 Longitude 10.75
Yearly Total Precipitation 1901 - 2009 (English) Latitude 53.25 Longitude 10.75
Yearly Total Wet Days 1901 - 2009 Latitude 53.25 Longitude 10.75
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude 53.25 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.