Climate Data for Latitude 52.25 Longitude -9.75

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

Locations

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Akeragh, Banna and Barrow Harbour SPA
Castlemaine Harbour
Castlemaine Harbour SPA
Kerry Head SPA
Killarney National Park
Killarney National Park SPA
Tralee Bay and Barrow Harbour

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min Temp37.937.338.940.644.749.252.352.149.745.741.139.3109 years
Mean Temp42.442.244.346.851.055.258.158.055.450.945.743.6109 years
Max Temp47.047.249.753.057.461.363.963.961.156.250.448.1109 years
FrostDays23.224.517.915.52.00.20.40.31.35.916.020.2109 years
WetDays24.621.321.516.518.316.716.521.220.324.625.124.6109 years
Precipitationin6.14.64.13.23.43.03.64.04.55.55.96.5109 years
Potential Evapotranspirationin0.60.91.52.12.83.03.02.61.91.30.70.5107 years
Yearly Average Temperatures 1901 - 2009 (English) Latitude 52.25 Longitude -9.75
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 52.25 Longitude -9.75
Yearly Total Frost Days 1901 - 2009 Latitude 52.25 Longitude -9.75
Yearly Total Precipitation 1901 - 2009 (English) Latitude 52.25 Longitude -9.75
Yearly Total Wet Days 1901 - 2009 Latitude 52.25 Longitude -9.75
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude 52.25 Longitude -9.75

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.