Climate Data for Latitude 50.75 Longitude -1.25

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

Locations

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Briddlesford Copses
Emer Bog
Isle of Wight Downs
Portsmouth Harbour
River Itchen
Solent and Isle of Wight Lagoons
Solent Maritime
Solent Marshes and Southampton Water
South Wight Maritime

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min TempF°37.036.338.140.846.751.555.355.552.347.941.638.4108 years
Mean TempF°41.040.843.647.453.458.361.862.158.553.046.342.6109 years
Max TempF°45.245.449.254.260.365.368.568.864.758.351.046.9109 years
FrostDays26.725.524.717.86.03.30.30.25.911.615.523.4109 years
WetDays17.512.513.711.812.29.09.09.510.514.615.916.1109 years
Precipitationin3.62.52.42.02.11.92.12.62.63.83.93.8109 years
Potential Evapotranspirationin0.50.81.42.13.13.63.73.32.11.30.60.5104 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 50.75 Longitude -1.25
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 50.75 Longitude -1.25
Yearly Total Frost Days 1901 - 2009 Latitude 50.75 Longitude -1.25
Yearly Total Precipitation 1901 - 2009 (English) Latitude 50.75 Longitude -1.25
Yearly Total Wet Days 1901 - 2009 Latitude 50.75 Longitude -1.25
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude 50.75 Longitude -1.25

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.