Climate Data for Latitude 49.75 Longitude 3.25

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

Locations

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Atlantic mixed forests ecoregion
Forêts picardes : massif de Saint-Gobain
Forêts picardes : massif de Saint-Gobain
Le Marais d'Isle
Moyenne vallée de l'Oise
Vallée de l'Oise de Thourotte à Vendeuil

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min TempF°32.533.036.540.246.551.554.654.350.144.137.834.1106 years
Mean TempF°37.238.844.049.156.161.364.664.359.451.743.338.5109 years
Max TempF°41.944.851.658.165.871.374.774.568.859.348.843.1109 years
FrostDays28.326.118.86.04.02.23.84.45.18.916.427.611 years
WetDays18.614.616.814.816.013.512.212.013.215.617.417.1109 years
Precipitationin2.11.81.91.92.22.32.42.22.12.42.52.5109 years
Potential Evapotranspirationin0.50.81.72.73.74.14.43.92.61.40.60.493 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 49.75 Longitude 3.25
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 49.75 Longitude 3.25
Yearly Total Frost Days 1902 - 2009 Latitude 49.75 Longitude 3.25
Yearly Total Precipitation 1901 - 2009 (English) Latitude 49.75 Longitude 3.25
Yearly Total Wet Days 1901 - 2009 Latitude 49.75 Longitude 3.25
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude 49.75 Longitude 3.25

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.