Climate Data for Latitude 37.25 Longitude -7.25

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

Locations

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Castro Marim
Isla Cristina and Ayamonte marshes and Prado lagoon
MARISMAS DE ISLA CRISTINA
MARISMAS DEL RIO PIEDRAS Y FLECHA DEL ROMPIDO
River Piedras marshes and Rompido sandbank
Sapais de Castro Marim
West Andévalo

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min TempF°45.546.148.952.157.162.566.467.063.658.051.046.6109 years
Mean TempF°52.753.756.960.565.771.576.177.072.766.358.553.6109 years
Max TempF°59.961.464.968.974.480.585.987.281.974.766.160.6109 years
FrostDays7.06.93.70.23.13.73.42.54.95.92.94.914 years
WetDays10.012.310.28.15.92.10.40.81.96.88.29.9109 years
Precipitationin2.82.22.51.61.00.40.00.10.62.43.23.3105 years
Potential Evapotranspirationin1.72.13.24.05.46.27.47.05.13.52.11.6109 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 37.25 Longitude -7.25
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 37.25 Longitude -7.25
Yearly Total Frost Days 1910 - 2009 Latitude 37.25 Longitude -7.25
Yearly Total Precipitation 1901 - 2009 (English) Latitude 37.25 Longitude -7.25
Yearly Total Wet Days 1901 - 2009 Latitude 37.25 Longitude -7.25
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude 37.25 Longitude -7.25

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.