Climate Data for Latitude 52.75 Longitude 5.75

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

Locations

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De Weerribben
Ketelmeer en Vossemeer
Lake Fluessen, Vogelhoek and Morra
Lake Ketelmeer
Lake Oudegaasterbrekken
Lake Witte and Zwarte Brekken
Lake Zwartemeer
Rottige Meenthe and Brandemeer
Zwarte Meer

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min Temp31.831.834.838.445.350.354.554.149.943.938.034.6106 years
Mean Temp36.036.641.145.953.758.162.162.057.149.942.738.6109 years
Max Temp40.241.547.453.562.166.069.870.064.556.147.642.6109 years
FrostDays27.828.023.814.38.94.01.71.74.715.419.231.03 years
WetDays20.712.918.613.214.114.614.415.416.417.222.522.1109 years
Precipitationin2.41.81.81.82.02.53.23.12.82.82.72.7109 years
Potential Evapotranspirationin0.40.71.42.23.33.43.63.32.11.20.60.481 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 52.75 Longitude 5.75
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 52.75 Longitude 5.75
Yearly Total Frost Days 1902 - 2009 Latitude 52.75 Longitude 5.75
Yearly Total Precipitation 1901 - 2009 (English) Latitude 52.75 Longitude 5.75
Yearly Total Wet Days 1901 - 2009 Latitude 52.75 Longitude 5.75
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude 52.75 Longitude 5.75

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.