Climate Data for Latitude 50.25 Longitude 1.75

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

Locations

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Dunes de Merlimont
Estuaires picards : baies de Somme et d'Authie
Marais arrière-littoraux Picards
Marais arrières littoraux picards
Marais de Balançon
Marais de Balançon et de Villiers

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min Temp35.235.037.741.147.352.055.855.852.246.740.336.7104 years
Mean Temp39.339.743.848.054.559.363.063.159.352.845.140.8109 years
Max Temp43.544.549.955.061.966.870.270.566.558.949.945.0109 years
FrostDays28.026.219.78.81.41.71.03.07.06.515.819.07 years
WetDays18.714.515.414.214.611.711.911.212.415.618.016.6109 years
Precipitationin2.51.82.01.92.01.92.32.12.33.03.22.8109 years
Potential Evapotranspirationin0.50.81.62.43.43.84.03.72.51.50.70.5104 years
Yearly Average Temperatures 1901 - 2009 (English) Latitude 50.25 Longitude 1.75
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 50.25 Longitude 1.75
Yearly Total Frost Days 1907 - 2009 Latitude 50.25 Longitude 1.75
Yearly Total Precipitation 1901 - 2009 (English) Latitude 50.25 Longitude 1.75
Yearly Total Wet Days 1901 - 2009 Latitude 50.25 Longitude 1.75
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude 50.25 Longitude 1.75

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.