Climate Data for Latitude 10.75 Longitude -61.25

Köppen climate classification: Am (Climate: equatorial; Precipitation: monsoonal)
 

Locations

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Caroni Swamp
Caroni Swamp Wildlife Sanctuary
Eastern Extension Matura Forest Reserve
Northern Range
Northern Range
Northern Range Wildlife Sanctuary
NRRB Forest Reserve
St David Forest Reserve
Valencia Wildlife Sactuary

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min TempF°67.867.768.670.172.071.971.571.571.771.571.069.3109 years
Mean TempF°75.976.176.978.479.578.778.578.979.379.078.376.9109 years
Max TempF°84.284.585.386.687.185.585.686.487.086.685.884.5109 years
FrostDays1.00.33.10.42.10.31.31.10.41.31.83.3109 years
WetDays14.65.47.54.121.527.929.629.223.624.228.923.3109 years
Precipitationin2.51.61.41.84.38.59.59.07.48.48.16.5109 years
Potential Evapotranspirationin3.83.94.84.74.73.84.04.13.93.83.43.6109 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 10.75 Longitude -61.25
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 10.75 Longitude -61.25
Yearly Total Frost Days 1901 - 2009 Latitude 10.75 Longitude -61.25
Yearly Total Precipitation 1901 - 2009 (English) Latitude 10.75 Longitude -61.25
Yearly Total Wet Days 1901 - 2009 Latitude 10.75 Longitude -61.25
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude 10.75 Longitude -61.25

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.