Climate Data for Latitude 46.75 Longitude 0.25

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

Locations

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FORET DE MOULIERE, LANDES DU PINAIL, BOIS DU DEFENS, DU FOU ET DE LA ROCHE DE BRAN
Le Pinail, Forêt de Moulière et bois du Défens
Plaine de Saint-Jean-de-Sauves
Plaines de Mirebeau et de Neuville-du-Poitou
PLAINES DU MIREBALAIS ET DU NEUVILLOIS

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min Temp34.234.437.240.946.851.655.054.850.845.138.335.4103 years
Mean Temp39.741.145.550.056.462.165.765.760.853.544.740.5109 years
Max Temp45.248.053.959.266.372.676.576.670.862.051.145.8109 years
FrostDays27.623.820.86.81.31.51.63.24.86.317.122.7109 years
WetDays16.213.415.213.716.99.89.08.610.612.815.414.9109 years
Precipitationin2.42.12.12.02.41.91.71.82.02.62.82.7109 years
Potential Evapotranspirationin0.61.01.92.83.64.45.04.32.91.60.70.5107 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 46.75 Longitude 0.25
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 46.75 Longitude 0.25
Yearly Total Frost Days 1901 - 2009 Latitude 46.75 Longitude 0.25
Yearly Total Precipitation 1901 - 2009 (English) Latitude 46.75 Longitude 0.25
Yearly Total Wet Days 1901 - 2009 Latitude 46.75 Longitude 0.25
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude 46.75 Longitude 0.25

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.