Climate Data for Latitude 53.25 Longitude 13.75

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

Locations

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Bollwinwiesen/Großer Gollinsee
Buchheide (Templiner Forst)
Charlottenhöhe
Eiskellerberge - Os bei Malchow
Großer Briesensee
Grumsiner Forst/Redernswalde
Köhntoptal
Kölpinsee
Kronhorst-Groß Fredenwalde
Kuhzer See/Jakobshagen
Labüskewiesen
Lübbesee
Platkowsee-Netzowsee-Metzelthin
Polsensee
Schwemmpfuhl
Suckower Haussee
Uckermärkische Seenlandschaft
Vietmannsdorfer Heide
Winkel

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min Temp26.326.731.437.945.851.855.554.449.041.734.829.8105 years
Mean Temp30.832.038.145.955.160.764.163.156.948.039.133.7108 years
Max Temp35.537.344.854.164.469.672.971.865.054.443.537.7109 years
FrostDays31.028.231.014.98.41.80.30.11.311.027.031.0109 years
WetDays18.111.912.511.011.312.313.813.312.311.715.716.6109 years
Precipitationin1.71.31.41.51.92.52.62.51.81.61.81.9109 years
Potential Evapotranspirationin0.40.51.42.54.04.24.53.82.41.20.50.478 years
Yearly Average Temperatures 1901 - 2009 (English) Latitude 53.25 Longitude 13.75
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 53.25 Longitude 13.75
Yearly Total Frost Days 1901 - 2009 Latitude 53.25 Longitude 13.75
Yearly Total Precipitation 1901 - 2009 (English) Latitude 53.25 Longitude 13.75
Yearly Total Wet Days 1901 - 2009 Latitude 53.25 Longitude 13.75
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude 53.25 Longitude 13.75

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.