Climate Data for Latitude 6.25 Longitude 80.25

Köppen climate classification: Af (Climate: equatorial; Precipitation: fully humid)
 

Locations

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Dediyagala Forest Reserve
Delgoda / Kudumiriya / Kobahadukanda
Dellawa / Diyadawa
Kanneliya Forest Reserve
Kanneliya Forest Reserve
Morapitiya-Runakanda
Nakiyadeniya / Kanneliya / Dediyagala
Sinharaja
Sinharaja Forest Reserve
Yagirala

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min TempF°70.571.072.574.475.875.674.974.774.373.572.271.8109 years
Mean TempF°78.178.780.181.080.980.179.779.479.479.178.478.3109 years
Max TempF°85.786.587.887.786.184.784.684.384.484.984.784.9109 years
FrostDays7.15.36.15.28.56.12.67.95.66.48.69.6107 years
WetDays3.31.93.910.08.89.87.97.88.115.314.87.6109 years
Precipitationin3.83.14.99.812.78.97.96.310.013.812.57.2109 years
Potential Evapotranspirationin5.04.85.44.74.44.24.34.54.24.13.94.3109 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 6.25 Longitude 80.25
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 6.25 Longitude 80.25
Yearly Total Frost Days 1901 - 2009 Latitude 6.25 Longitude 80.25
Yearly Total Precipitation 1901 - 2009 (English) Latitude 6.25 Longitude 80.25
Yearly Total Wet Days 1901 - 2009 Latitude 6.25 Longitude 80.25
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude 6.25 Longitude 80.25

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.