Climate Data for Latitude 60.75 Longitude 17.25

Köppen climate classification: Dfb (Climate: snow; Precipitation: fully humid; Temperature: warm summer)
 

Locations

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Bläcktärnsjön
Brännan
Grinduga
Gustavsmurarna
Hådells gammelskog
Håmansmaren
Harkskärsfjärden
Igelsjön
Limön
Marma
Matyxsjön
Orarna
Ormön
Sävasjön
Sörsundet
Styggmurarna
Testeboån
Testeboån-nedre
Testeboåns delta
Vitgrund-Norrskär

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min TempF°19.819.122.630.938.847.353.651.944.937.629.923.9107 years
Mean TempF°24.824.929.437.346.054.560.658.751.242.834.128.5109 years
Max TempF°29.830.836.343.853.261.967.765.757.748.038.232.9107 years
FrostDays31.028.231.030.025.211.20.11.98.929.430.031.0109 years
WetDays15.511.210.69.87.78.911.813.714.212.316.314.8109 years
Precipitationin1.61.11.11.41.51.92.73.12.32.02.01.8109 years
Potential Evapotranspirationin0.20.40.91.83.13.84.03.01.80.80.30.325 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 60.75 Longitude 17.25
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 60.75 Longitude 17.25
Yearly Total Frost Days 1901 - 2009 Latitude 60.75 Longitude 17.25
Yearly Total Precipitation 1901 - 2009 (English) Latitude 60.75 Longitude 17.25
Yearly Total Wet Days 1901 - 2009 Latitude 60.75 Longitude 17.25
Yearly Total Potential Evapotranspiration 1907 - 2009 (English) Latitude 60.75 Longitude 17.25

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.