Zur Sommerwitterung in der Bundesrepublik Deutschland
DOI:
https://doi.org/10.3112/erdkunde.1984.03.03Keywords:
meteorology, climatology, Germany, weatherAbstract
The analysis of the spatial and temporal patterns of the summer time weather in the FRG presents a map of the mean annual numbers of days of summer-time weather. It is evident that the 50th parallel nearly separates a region with summer temperatures above average (Southern Germany) from a region with summer temperatures below average (Northern Germany). The analysis further identifies years of maximum similarity of summer-time weather by means of a PCA (principal component analysis) - followed by an analysis of spatial patterns of these similarities in time. Two main boundaries of summer-time weather appear according to the number of days with a maximum temperature >25°C and the number of days with precipitation >0,1 mm: the Main and Nahe valleys and the northern boundary of the Rheinisches Schiefergebirge. Southwestern Germany mostly shows a marked affinity with Northern Germany.Downloads
Published
1984-09-30
How to Cite
Frankenberg, P. (1984). Zur Sommerwitterung in der Bundesrepublik Deutschland. ERDKUNDE, 38(3), 177–187. https://doi.org/10.3112/erdkunde.1984.03.03
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