Climate Data for Latitude 53.25 Longitude 6.25

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

Locations

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Duinen Schiermonnikoog
Engelsmanplaat
Fochteloërveen and Lake Esmeer
Fochteloërveen en Esmeer
Lake Leekstermeer
Lauwersmeer
Lauwersmeer
Leekstermeergebied
Schiermonnikoog
Van Oordt's Mersken
Van Oordt's Mersken

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min Temp30.931.134.238.144.649.954.153.849.643.637.633.6105 years
Mean Temp35.235.940.345.552.957.761.761.656.949.742.237.6109 years
Max Temp39.540.846.553.161.465.669.469.664.455.847.041.7109 years
FrostDays27.028.024.517.610.47.31.31.75.217.620.127.93 years
WetDays20.513.617.913.914.614.515.416.217.218.223.122.6109 years
Precipitationin2.81.92.01.82.02.53.23.22.93.13.02.9109 years
Potential Evapotranspirationin0.40.61.32.13.23.43.53.22.01.10.50.367 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 53.25 Longitude 6.25
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 53.25 Longitude 6.25
Yearly Total Frost Days 1902 - 2009 Latitude 53.25 Longitude 6.25
Yearly Total Precipitation 1901 - 2009 (English) Latitude 53.25 Longitude 6.25
Yearly Total Wet Days 1901 - 2009 Latitude 53.25 Longitude 6.25
Yearly Total Potential Evapotranspiration 1902 - 2009 (English) Latitude 53.25 Longitude 6.25

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.