Climate Data for Latitude 4.75 Longitude -73.75

Köppen climate classification: Cfb (Climate: warm temperate; Precipitation: fully humid; Temperature: warm summer)
 

Locations

Download
Chingaza Natural National Park and surrounding areas
Cuencas Río Blanco y Negro National Protective Forests Reserves
Gravilleras del Valle del Río Siecha
Parque Nacional Natural Chingaza

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min TempF°44.345.246.848.248.147.346.346.245.746.646.845.2109 years
Mean TempF°55.355.856.356.656.154.954.154.654.755.455.855.2109 years
Max TempF°66.466.665.965.064.262.662.063.063.864.464.965.3109 years
FrostDays5.41.72.61.34.24.14.94.61.22.75.22.8109 years
WetDays5.67.813.122.228.329.930.826.021.621.619.78.2109 years
Precipitationin1.01.62.84.85.15.25.33.72.94.73.91.9109 years
Potential Evapotranspirationin3.22.93.02.62.62.52.72.82.72.72.62.9109 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 4.75 Longitude -73.75
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 4.75 Longitude -73.75
Yearly Total Frost Days 1901 - 2009 Latitude 4.75 Longitude -73.75
Yearly Total Precipitation 1901 - 2009 (English) Latitude 4.75 Longitude -73.75
Yearly Total Wet Days 1901 - 2009 Latitude 4.75 Longitude -73.75
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude 4.75 Longitude -73.75

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.