Climate Data for Latitude 56.75 Longitude 14.25

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

Locations

Download
Almås
Åshuvud
Byvärma
Centrala Möckeln
Dihult
Hjälmsänga
Horsnäsamossen
Kronan
Kruseböke
Labbramsängen
Målaskogsberg
Ramsås
Stora Grönlid
Strandängar vid Garanshultasjön
Taglamyren
Vakö myr
Vedåsa

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min Temp23.422.426.332.640.547.652.150.645.238.932.727.0104 years
Mean Temp28.128.133.141.350.757.561.359.652.945.037.031.2109 years
Max Temp32.633.539.750.061.067.670.568.760.651.041.235.4109 years
FrostDays31.028.231.029.723.010.30.43.86.825.829.931.0109 years
WetDays21.513.212.211.010.411.112.913.213.414.419.219.3109 years
Precipitationin2.11.41.51.61.72.33.03.02.62.52.52.3109 years
Potential Evapotranspirationin0.20.41.12.23.84.44.43.52.11.00.30.232 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 56.75 Longitude 14.25
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 56.75 Longitude 14.25
Yearly Total Frost Days 1901 - 2009 Latitude 56.75 Longitude 14.25
Yearly Total Precipitation 1901 - 2009 (English) Latitude 56.75 Longitude 14.25
Yearly Total Wet Days 1901 - 2009 Latitude 56.75 Longitude 14.25
Yearly Total Potential Evapotranspiration 1902 - 2009 (English) Latitude 56.75 Longitude 14.25

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.