Climate Data for Latitude 36.75 Longitude -5.25

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

Locations

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Líjar mountain range-Zaframagon crag
Mountain ranges of Ronda, Bermeja and Crestellina
PEÑON DE ZAFRAMAGON
Reserva de Grazalema
SIERRA DE GRAZALEMA
SIERRA DE HORNACHUELOS
Ubrique and Grazalema mountain ranges

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min TempF°40.341.544.046.951.657.662.363.760.053.546.541.8109 years
Mean TempF°47.849.552.756.161.768.674.575.470.362.354.249.1109 years
Max TempF°55.557.561.565.571.979.786.987.380.771.261.956.5109 years
FrostDays17.820.514.38.81.83.95.74.94.67.09.513.7108 years
WetDays8.09.510.58.05.82.40.91.02.46.48.49.8109 years
Precipitationin2.83.42.82.21.30.60.20.20.82.53.23.295 years
Potential Evapotranspirationin1.92.23.23.95.36.58.07.45.33.52.11.8109 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 36.75 Longitude -5.25
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 36.75 Longitude -5.25
Yearly Total Frost Days 1901 - 2009 Latitude 36.75 Longitude -5.25
Yearly Total Precipitation 1901 - 2009 (English) Latitude 36.75 Longitude -5.25
Yearly Total Wet Days 1901 - 2009 Latitude 36.75 Longitude -5.25
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude 36.75 Longitude -5.25

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.