Climate Data for Latitude 49.75 Longitude 4.25

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

Locations

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Confluent des vallées de la Meuse et de la Chiers
Forêts de Thiérache : Hirson et Saint-Michel
Haute vallée de l'Eau Noire (Chimay; Couvin)
Vallées de l'Oise et de la Wartoise (Chimay; Momignies)

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min TempF°30.430.434.138.144.549.952.952.647.942.236.231.9100 years
Mean TempF°35.636.942.247.755.060.263.563.257.950.341.937.2109 years
Max TempF°40.843.750.457.465.670.774.373.867.958.647.942.4108 years
FrostDays30.728.024.611.35.30.53.94.43.613.522.229.671 years
WetDays19.114.917.115.115.814.012.513.014.115.817.818.5109 years
Precipitationin3.12.52.62.32.62.72.92.82.63.03.43.3109 years
Potential Evapotranspirationin0.40.81.62.63.64.04.33.72.41.30.50.391 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 49.75 Longitude 4.25
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 49.75 Longitude 4.25
Yearly Total Frost Days 1901 - 2009 Latitude 49.75 Longitude 4.25
Yearly Total Precipitation 1901 - 2009 (English) Latitude 49.75 Longitude 4.25
Yearly Total Wet Days 1901 - 2009 Latitude 49.75 Longitude 4.25
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude 49.75 Longitude 4.25

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.