Climate Data for Latitude 54.75 Longitude -2.25

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

Locations

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Helbeck and Swindale Woods
Moor House – Upper Teesdale
Moor House-Upper Teesdale Biosphere Reserve
North Pennine Moors
North Pennine Moors
Tyne and Allen River Gravels
Tyne and Nent

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min TempF°30.229.831.834.538.944.148.048.044.740.034.331.2101 years
Mean TempF°34.734.737.541.547.051.955.455.251.245.639.235.9109 years
Max TempF°39.239.643.248.555.159.762.962.457.751.344.140.5109 years
FrostDays31.028.231.028.518.510.86.06.210.423.728.731.0109 years
WetDays22.116.819.017.816.613.716.116.617.020.120.221.0109 years
Precipitationin4.83.83.42.72.82.73.33.93.34.44.84.7109 years
Potential Evapotranspirationin0.30.51.11.62.52.82.92.41.50.90.40.381 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 54.75 Longitude -2.25
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 54.75 Longitude -2.25
Yearly Total Frost Days 1901 - 2009 Latitude 54.75 Longitude -2.25
Yearly Total Precipitation 1901 - 2009 (English) Latitude 54.75 Longitude -2.25
Yearly Total Wet Days 1901 - 2009 Latitude 54.75 Longitude -2.25
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude 54.75 Longitude -2.25

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.