Climate Data for Latitude 50.75 Longitude 16.75

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

Locations

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Góry Bardzkie
Kamionki
Masyw Slezy
Mietkow reservoir
Muszkowicki Las Bukowy
Ostoja Nietoperzy Gór Sowich
Przeplatki nad Bystrzyca
Skalki Stoleckie
Wzgórza Kielczynskie
Zbiornik Mietkowski

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min Temp21.923.629.436.244.950.454.052.947.139.832.326.0102 years
Mean Temp27.129.536.244.954.659.863.562.555.546.636.830.2109 years
Max Temp32.335.143.153.664.269.273.172.164.053.541.434.5107 years
FrostDays31.028.231.027.210.50.60.60.53.815.730.031.0109 years
WetDays15.012.212.911.912.813.914.313.111.211.415.117.1109 years
Precipitationin1.51.41.51.83.03.43.93.62.11.81.81.8109 years
Potential Evapotranspirationin0.50.71.52.63.94.14.63.92.51.50.70.596 years
Yearly Average Temperatures 1901 - 2009 (English) Latitude 50.75 Longitude 16.75
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 50.75 Longitude 16.75
Yearly Total Frost Days 1901 - 2009 Latitude 50.75 Longitude 16.75
Yearly Total Precipitation 1901 - 2009 (English) Latitude 50.75 Longitude 16.75
Yearly Total Wet Days 1901 - 2009 Latitude 50.75 Longitude 16.75
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude 50.75 Longitude 16.75

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.