Climate Data for Latitude 40.75 Longitude 0.25

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

Locations

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Lower course of the river Matarraña-Ribarroja
Pass of Beceite-Turmell mountain
PUERTOS DE BECEITE
Secans del Montsià
Serra de Godall
Sistema Prelitoral meridional
Tinença de Benifassà, Turmell i Vallivana

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min Temp35.837.240.244.250.657.462.663.258.150.241.937.7108 years
Mean Temp43.745.950.054.160.767.973.773.768.059.350.045.0109 years
Max Temp51.754.759.964.070.978.584.884.277.968.558.352.5109 years
FrostDays27.224.514.011.85.04.73.04.26.810.116.922.1109 years
WetDays6.55.45.37.18.36.64.54.15.66.75.96.2109 years
Precipitationin0.90.91.31.62.11.40.41.02.32.21.71.5105 years
Potential Evapotranspirationin1.52.03.13.95.05.97.06.24.12.81.71.4109 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 40.75 Longitude 0.25
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 40.75 Longitude 0.25
Yearly Total Frost Days 1901 - 2009 Latitude 40.75 Longitude 0.25
Yearly Total Precipitation 1901 - 2009 (English) Latitude 40.75 Longitude 0.25
Yearly Total Wet Days 1901 - 2009 Latitude 40.75 Longitude 0.25
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude 40.75 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.