Climate Data for Latitude 53.75 Longitude 9.75

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

Locations

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Binnendünen Nordoe
Feerner Moor
Holmer Sandberge und Buttermoor
Mühlenberger Loch/Neßsand
NSG Tävsmoor / Haselauer Moor
Rapfenschutzgebiet Hamburger Stromelbe
Schnaakenmoor
Unterelbe bis Wedel

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min TempF°29.229.833.138.245.551.054.954.649.843.336.931.7108 years
Mean TempF°33.334.439.045.854.059.262.962.657.049.341.135.5109 years
Max TempF°37.539.145.153.562.667.671.070.664.455.445.539.3108 years
FrostDays31.028.031.015.39.25.32.02.01.517.427.431.01 years
WetDays18.012.913.413.712.213.814.915.914.014.017.417.5109 years
Precipitationin2.41.61.91.82.12.53.43.22.62.72.72.6109 years
Potential Evapotranspirationin0.40.61.32.23.63.94.03.62.21.20.50.373 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 53.75 Longitude 9.75
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 53.75 Longitude 9.75
Yearly Total Frost Days 1965 - 2009 Latitude 53.75 Longitude 9.75
Yearly Total Precipitation 1901 - 2009 (English) Latitude 53.75 Longitude 9.75
Yearly Total Wet Days 1901 - 2009 Latitude 53.75 Longitude 9.75
Yearly Total Potential Evapotranspiration 1902 - 2009 (English) Latitude 53.75 Longitude 9.75

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.