Climate Data for Latitude 28.25 Longitude -16.75

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


Acantilados de Santo Domingo
Arico pine woodland
Canary Islands dry woodlands and forests ecoregion
Corona Forestal
El Médano coast
Garachico rocky islet
Los Gigantes coastal cliff
Montaña Roja
Mountain of Agua, gully of Los Cochinos and gully of Cuevas Negras
Rasca lava fields-Guaza mountain-Las Mesas plain
Rasca y Guaza
Roque de Garachico
Santo Domingo coastal cliffs
Tágara gully
Teide National Park
Tigaiga slope
Vilaflor pine woodland

Averages (English) Metric

Min Temp49.749.651.052.153.557.460.662.361.458.855.451.9109 years
Mean Temp54.855.056.857.959.663.567.569.067.864.660.656.8109 years
Max Temp59.960.562.864.065.869.874.475.874.270.565.861.8109 years
FrostDays9.713. years
WetDays7. years
Precipitationin1. years
Potential Evapotranspirationin2. years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 28.25 Longitude -16.75
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 28.25 Longitude -16.75
Yearly Total Frost Days 1901 - 2009 Latitude 28.25 Longitude -16.75
Yearly Total Precipitation 1901 - 2009 (English) Latitude 28.25 Longitude -16.75
Yearly Total Wet Days 1901 - 2009 Latitude 28.25 Longitude -16.75
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude 28.25 Longitude -16.75

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.