Climate Data for Latitude 38.75 Longitude -0.25

Köppen climate classification: Csa (Climate: warm temperate; Precipitation: summer dry; Temperature: hot summer)
 

Locations

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Cabeço d'Or i la Grana
Ifac i Litoral de la Marina
Illots de Benidorm i Serra Gelada
Marina mountain ranges
Marjal de Pego-Oliva.
Montdúver-Marjal de la Safor
Muntanyes de la Marina
Pego-Oliva marshes

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min TempF°39.039.942.646.352.159.364.365.460.352.745.040.6109 years
Mean TempF°47.849.052.255.861.668.974.274.969.861.853.748.9109 years
Max TempF°56.658.261.865.471.178.684.284.679.471.062.457.4109 years
FrostDays20.417.113.25.43.24.83.73.64.37.110.811.5109 years
WetDays7.46.15.76.16.14.42.12.23.67.45.87.5109 years
Precipitationin0.81.01.01.31.20.70.30.51.61.91.61.3104 years
Potential Evapotranspirationin1.62.13.03.64.65.56.25.64.02.81.81.5109 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 38.75 Longitude -0.25
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 38.75 Longitude -0.25
Yearly Total Frost Days 1901 - 2009 Latitude 38.75 Longitude -0.25
Yearly Total Precipitation 1901 - 2009 (English) Latitude 38.75 Longitude -0.25
Yearly Total Wet Days 1901 - 2009 Latitude 38.75 Longitude -0.25
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude 38.75 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.