Climate Data for Latitude 52.25 Longitude 14.75

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

Locations

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Dolina Ilanki
Dolina Pliszki
Dorchetal
Fauler See / Markendorfer Wald
Fledermausquartier Brauereikeller Frankfurt (Oder)
Klautzke-See und Waldmoore mit Kobbelke
Pohlitzer Mühlenfließ
Priesterschlucht
Torfowiska Sulowskie
Torfowisko Mlodno
Trautzke-Seen und Moore
Trockenhänge Lawitz
Ujscie Ilanki
Zeisigberg

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min Temp25.727.232.538.647.152.956.455.249.842.535.129.0108 years
Mean Temp30.532.639.247.256.762.265.664.557.949.039.633.3109 years
Max Temp35.338.046.055.866.471.674.973.866.255.644.237.7109 years
WetDays16.211.612.111.211.712.513.013.112.211.615.116.7109 years
Precipitationin1.51.31.31.62.02.42.72.71.61.51.61.7109 years
Potential Evapotranspirationin0.40.61.52.64.14.44.74.02.51.30.60.484 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 52.25 Longitude 14.75
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 52.25 Longitude 14.75
Yearly Total Precipitation 1901 - 2009 (English) Latitude 52.25 Longitude 14.75
Yearly Total Wet Days 1901 - 2009 Latitude 52.25 Longitude 14.75
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude 52.25 Longitude 14.75

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.