Table 1.
Process | Stratiform rainfall | Soil moisture excess | Snowmelt | Rain on snow | Convective rainfall |
---|---|---|---|---|---|
Overall relevance (% of all floods) | 31.0 | 26.0 | 21.5 | 18.1 | 3.4 |
Average trend of relevance (% per decade) | 0.49 | 1.55 | −1.65 | −0.41 | −0.06 |
Average flood synchrony scale (distance as % of station average) | 92.0 * | 113.2 * | 93.6 * | 107.2 * | 73.9 * |
Average flood magnitude (% of station average) | 100.7 ** | 103.2 * | 97.0 * | 98.0 * | 98.8 ** |
Note. Floods that are generated by different processes have significantly different spatial extents (synchrony scales). The large‐extent soil moisture related floods have increased in frequency. The average scaled flood magnitudes are almost independent of the flood generation process
Synchrony scales and flood magnitudes significantly different from the overall mean (p = 0.001).
No significance.