Climate Data for Latitude 54.75 Longitude 8.75

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

Locations

Download
Gotteskoog-Gebiet
NSG Bordelumer Heide und Langenhorner Heide mit Umgebung
Süderlügumer Binnendünen
Tøndermarsken, Magisterkog and Rudbøl Sø
Vidå med tilløb, Rudbøl Sø og Magisterkogen
Vidåen, Tøndermarsken og Saltvandssøen

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min Temp29.329.332.537.544.450.054.154.049.743.536.831.8103 years
Mean Temp33.433.637.844.452.557.861.561.556.249.041.035.8109 years
Max Temp37.437.943.151.560.765.768.969.062.854.745.339.7109 years
FrostDays30.328.031.016.712.78.02.32.14.313.924.030.48 years
WetDays18.412.414.313.712.313.114.315.817.318.620.919.3109 years
Precipitationin2.61.71.91.71.92.43.13.63.23.53.22.7109 years
Potential Evapotranspirationin0.40.51.12.03.33.73.73.42.11.10.40.366 years
Yearly Average Temperatures 1901 - 2009 (English) Latitude 54.75 Longitude 8.75
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 54.75 Longitude 8.75
Yearly Total Frost Days 1902 - 2009 Latitude 54.75 Longitude 8.75
Yearly Total Precipitation 1901 - 2009 (English) Latitude 54.75 Longitude 8.75
Yearly Total Wet Days 1901 - 2009 Latitude 54.75 Longitude 8.75
Yearly Total Potential Evapotranspiration 1902 - 2009 (English) Latitude 54.75 Longitude 8.75

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.