Low water drain dispenser -MN10q- (HAD)

Map 3.10 shows the mean low from flow dispensing MN10q in the form of a grid field representation in resolution 1 km². In the spatial distribution different influencing factors on the low are recognizable, as they are also contained in the applied parameters of multiple linear regression. The precipitation height (para metrised as median of the Som mer never the impact height) characterises the large-scale distribution. In the high altitudes of the Alps, where there are high rainfall (Atlas Tables 2.2 to 2.6) at relatively short dry periods (Atlas table 2.15) and low evaporation heights (Atlas Tables 2.12 and 2.13), low water drains increase to over 12 l/s·km². Also high values of 6 l/s·km² can be seen in the Prealpenland and in the range of altitudes of most low mountain ranges.