Climate Data for Latitude 57.25 Longitude -3.75

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

Locations

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Abernethy Forest
Anagach Wood
Cairngorms
Cairngorms
Carn nan Tri-Tighearnan
Kinveachy Forest
Kinveachy Forest
Loch Vaa
Moidach More
River Spey
River Spey: Insh Marshes
Slochd

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min Temp28.127.229.932.637.242.646.245.542.237.732.429.1104 years
Mean Temp33.633.736.440.445.850.954.053.449.444.137.934.5108 years
Max Temp39.040.042.948.254.559.361.961.356.650.643.539.8108 years
FrostDays31.028.231.030.026.412.87.57.413.426.330.031.0109 years
WetDays23.519.021.618.818.415.316.418.020.421.923.623.3109 years
Precipitationin4.02.93.02.52.72.63.13.53.34.44.14.0109 years
Potential Evapotranspirationin0.50.61.11.72.62.92.92.41.61.10.50.4100 years
Yearly Average Temperatures 1901 - 2009 (English) Latitude 57.25 Longitude -3.75
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 57.25 Longitude -3.75
Yearly Total Frost Days 1901 - 2009 Latitude 57.25 Longitude -3.75
Yearly Total Precipitation 1901 - 2009 (English) Latitude 57.25 Longitude -3.75
Yearly Total Wet Days 1901 - 2009 Latitude 57.25 Longitude -3.75
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude 57.25 Longitude -3.75

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.