Climate Data for Latitude 49.75 Longitude 19.25

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

Locations

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Babia Gora Mountain
Beskid Maly
Beskid Slaski
Brzeszcze ponds
Dolina Dolnej Skawy
Dolina Dolnej Soly
Kosciól w Radziechowach
Lower Skawa River Valley
Lower Sola River Valley
Stawy w Brzeszczach

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min TempF°18.420.726.533.742.447.951.150.244.237.329.622.7108 years
Mean TempF°24.827.634.743.252.757.961.360.453.645.535.227.9109 years
Max TempF°30.934.642.852.763.167.971.670.763.253.740.933.0107 years
FrostDays31.028.231.029.717.53.83.43.110.821.130.031.0109 years
WetDays15.614.414.113.114.315.515.513.511.311.315.318.0109 years
Precipitationin1.81.71.92.63.85.05.74.73.22.42.42.1109 years
Potential Evapotranspirationin0.50.71.52.33.53.84.13.52.31.40.60.497 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 49.75 Longitude 19.25
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 49.75 Longitude 19.25
Yearly Total Frost Days 1901 - 2009 Latitude 49.75 Longitude 19.25
Yearly Total Precipitation 1901 - 2009 (English) Latitude 49.75 Longitude 19.25
Yearly Total Wet Days 1901 - 2009 Latitude 49.75 Longitude 19.25
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude 49.75 Longitude 19.25

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.