Climate Data for Latitude 42.25 Longitude 0.75

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

Locations

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EL TURBÓN Y SIERRA DE SÍS
La Faiada de Malpàs i Cambatiri
Montsech and Montgai mountains
Sant Gervás mountains
Serres del Montsec, Sant Mamet i Mitjana
Turbón-Espés-Sis
Vall Alta de Serradell-Serra de Sant Gervàs

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min TempF°28.529.533.337.143.750.154.955.250.943.234.730.2105 years
Mean TempF°35.237.542.346.353.460.966.566.360.651.641.936.3109 years
Max TempF°41.845.451.355.763.371.778.377.570.560.249.242.4109 years
FrostDays31.028.229.019.99.65.85.62.45.614.027.031.0109 years
WetDays8.78.09.111.711.49.46.96.47.28.98.88.3109 years
Precipitationin1.71.72.22.93.62.81.72.42.82.62.62.1107 years
Potential Evapotranspirationin1.01.52.53.14.25.36.55.63.82.41.40.9109 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 42.25 Longitude 0.75
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 42.25 Longitude 0.75
Yearly Total Frost Days 1901 - 2009 Latitude 42.25 Longitude 0.75
Yearly Total Precipitation 1901 - 2009 (English) Latitude 42.25 Longitude 0.75
Yearly Total Wet Days 1901 - 2009 Latitude 42.25 Longitude 0.75
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude 42.25 Longitude 0.75

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.