Climate Data for Latitude 53.25 Longitude 9.75

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

Locations

Download
Auetal und Nebentäler
Este-Unterlauf
Fischbeker Heide
Großes Moor bei Wistedt
Lüneburger Heide
Moore bei Buxtehude
Moore bei Sittensen
Moorgürtel
Schwarzes Moor und Seemoor

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min TempF°28.529.232.837.845.150.654.354.149.342.836.331.1104 years
Mean TempF°33.034.239.145.954.159.362.762.456.949.040.735.1109 years
Max TempF°37.439.245.554.063.268.171.270.964.655.345.239.2109 years
FrostDays30.628.130.314.77.24.50.20.12.115.523.430.8109 years
WetDays17.913.213.113.812.514.114.916.313.713.316.417.6109 years
Precipitationin2.31.61.81.92.12.63.23.12.52.52.42.4109 years
Potential Evapotranspirationin0.40.61.32.33.63.94.03.62.21.20.50.376 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 53.25 Longitude 9.75
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 53.25 Longitude 9.75
Yearly Total Frost Days 1901 - 2009 Latitude 53.25 Longitude 9.75
Yearly Total Precipitation 1901 - 2009 (English) Latitude 53.25 Longitude 9.75
Yearly Total Wet Days 1901 - 2009 Latitude 53.25 Longitude 9.75
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude 53.25 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.