Climate Data for Latitude 57.25 Longitude 15.75

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

Locations

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Björnnäset
Drags udde
Emåns vattensystem i Kalmar län
Högarp
Högeruda-Skinnskälla
Hulingen
Ideboås
Kraskögle
Ryngen
Sällevadsån (östra)
Sällevadsån (västra)
Stenbergsmo
Stensryd

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min TempF°22.921.925.331.940.047.752.550.945.638.832.226.1106 years
Mean TempF°27.727.431.840.049.557.061.359.552.944.636.730.6109 years
Max TempF°32.232.838.348.059.066.470.268.160.250.541.035.0107 years
FrostDays31.028.231.030.020.310.10.34.36.622.230.031.0109 years
WetDays17.512.910.89.69.09.011.810.912.112.720.418.4109 years
Precipitationin1.61.11.21.31.61.92.62.62.11.92.01.9108 years
Potential Evapotranspirationin0.20.41.12.23.84.54.43.52.11.10.40.225 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 57.25 Longitude 15.75
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 57.25 Longitude 15.75
Yearly Total Frost Days 1901 - 2009 Latitude 57.25 Longitude 15.75
Yearly Total Precipitation 1901 - 2009 (English) Latitude 57.25 Longitude 15.75
Yearly Total Wet Days 1901 - 2009 Latitude 57.25 Longitude 15.75
Yearly Total Potential Evapotranspiration 1907 - 2009 (English) Latitude 57.25 Longitude 15.75

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.