Climate Data for Latitude 52.25 Longitude 9.25

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

Locations

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Begatal
Emmer
Hamel und Nebenbäche
Mausohr-Quartiere Wesergebirge
Mausohr-Wochenstube bei Barsinghausen
Rinderweide
Schaumburger Wald
Steinhuder Meer
Teufelsbad
Vogelschutzgebiet 'Weseraue'

Averages (English) Metric

TypeUnitsJanFebMarAprMayJunJulAugSepOctNovDecPeriod
Min TempF°28.328.832.937.745.450.554.153.749.042.335.930.7106 years
Mean TempF°32.634.139.646.254.459.562.862.356.848.740.134.6109 years
Max TempF°36.939.246.254.863.568.671.671.064.855.344.538.6109 years
FrostDays30.828.130.115.15.31.60.50.81.813.625.030.7109 years
WetDays17.613.313.914.113.414.514.815.513.913.015.417.7109 years
Precipitationin2.21.71.71.82.22.52.92.82.22.12.22.3109 years
Potential Evapotranspirationin0.40.71.42.33.63.84.13.52.21.20.50.372 years
Yearly Average Temperatures 2010 - 2009 (English) Latitude 52.25 Longitude 9.25
Monthly Mean Temperatures 1901 - 2009 (English) Latitude 52.25 Longitude 9.25
Yearly Total Frost Days 1901 - 2009 Latitude 52.25 Longitude 9.25
Yearly Total Precipitation 1901 - 2009 (English) Latitude 52.25 Longitude 9.25
Yearly Total Wet Days 1901 - 2009 Latitude 52.25 Longitude 9.25
Yearly Total Potential Evapotranspiration 1901 - 2009 (English) Latitude 52.25 Longitude 9.25

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.