Climate Data for Latitude 52.25 Longitude 4.75

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

Locations

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Broekvelden/Vettenbroek
De Wilck
De Wilck
Ilperveld, Varkensland and Twiske
Ilperveld, Varkensland en Twiske
Nieuwkoopse Plassen
Nieuwkoopse Plassen
Oostzanerveld
Reeuwijkse Plassen

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min TempF°32.532.235.539.546.051.154.754.650.644.738.634.6106 years
Mean TempF°36.637.241.646.754.058.862.262.157.750.743.238.6109 years
Max TempF°40.842.147.854.062.166.769.769.664.956.747.842.7109 years
FrostDays28.627.119.615.77.34.01.32.75.712.516.228.33 years
WetDays20.312.718.512.513.914.013.413.915.417.222.221.0109 years
Precipitationin2.71.82.11.71.92.32.93.03.13.33.32.9109 years
Potential Evapotranspirationin0.40.71.42.23.43.63.73.32.11.20.60.377 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 52.25 Longitude 4.75
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 52.25 Longitude 4.75
Yearly Total Frost Days 1902 - 2009 Latitude 52.25 Longitude 4.75
Yearly Total Precipitation 1901 - 2009 (English) Latitude 52.25 Longitude 4.75
Yearly Total Wet Days 1901 - 2009 Latitude 52.25 Longitude 4.75
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude 52.25 Longitude 4.75

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.