Climate Data for Latitude -22.25 Longitude 166.75

Köppen climate classification: Aw (Climate: equatorial; Precipitation: winter dry)
 

Locations

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de la Haute Yate Special Fauna Reserve
Massifs du Grand Sud - entre le mont Humboldt et la rivière Bleue
Massifs du Grand Sud: entre le mont Humboldt et la rivière Bleue
Parc Territorial de la Riviere Bleue Territorial Park
Plaine des Lacs
Port Boisé

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min Temp71.171.670.868.264.962.460.160.261.164.066.869.5109 years
Mean Temp76.276.675.472.769.667.265.165.366.569.472.174.6109 years
Max Temp81.381.780.077.374.372.070.270.472.074.977.579.7109 years
FrostDays0.30.20.30.21.02.01.01.00.10.20.30.31 years
WetDays18.016.221.816.814.814.015.612.712.111.510.914.7109 years
Precipitationin5.75.67.24.53.53.73.33.12.21.92.64.0109 years
Potential Evapotranspirationin5.04.24.23.53.02.62.73.23.64.44.75.1109 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude -22.25 Longitude 166.75
Monthly Mean Temperatures 1901 - 2009 (English) Latitude -22.25 Longitude 166.75
Yearly Total Frost Days 1956 - 2009 Latitude -22.25 Longitude 166.75
Yearly Total Precipitation 1901 - 2009 (English) Latitude -22.25 Longitude 166.75
Yearly Total Wet Days 1901 - 2009 Latitude -22.25 Longitude 166.75
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude -22.25 Longitude 166.75

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.