Climate Data for Latitude 36.75 Longitude -5.75

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

Locations

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Bornos reservoir
COLA DEL EMBALSE DE ARCOS
COLA DEL EMBALSE DE BORNOS
COMPLEJO ENDORREICO DE ESPERA
COMPLEJO ENDORREICO LEBRIJA-LAS CABEZAS
Lebrija, Las Cabezas and Espera lagoons
Medina-Sidonia

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min TempF°43.244.947.550.354.660.264.566.063.056.849.944.8109 years
Mean TempF°50.852.856.259.564.570.976.677.773.365.657.752.1109 years
Max TempF°58.460.765.068.774.581.688.789.483.674.665.559.5109 years
FrostDays12.513.911.13.91.72.43.94.74.74.45.78.7101 years
WetDays8.610.19.97.45.32.10.50.92.16.38.29.7109 years
Precipitationin2.83.22.92.01.00.40.10.10.62.63.63.487 years
Potential Evapotranspirationin1.82.23.44.15.56.58.17.55.43.72.21.7109 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 36.75 Longitude -5.75
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 36.75 Longitude -5.75
Yearly Total Frost Days 1901 - 2009 Latitude 36.75 Longitude -5.75
Yearly Total Precipitation 1901 - 2009 (English) Latitude 36.75 Longitude -5.75
Yearly Total Wet Days 1901 - 2009 Latitude 36.75 Longitude -5.75
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude 36.75 Longitude -5.75

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.