The precipitation diurnal cycle (PDC) varies with the season and location. Its link to large-scale weather circulations has been studied in different regions. However, comparable information is lacking for Central Europe. Two decades of hourly precipitation data were combined with records of objective weather patterns over Germany, focusing on the general atmospheric wind directions (WD). The PDC is characterized by the frequency and the average amount of hourly precipitation. The precipitation frequency generally has two peaks: one in the morning and the other in the afternoon. The morning peak of the precipitation amount is small compared to that of the afternoon peak. Remarkably, WD has a prominent influence on the PDC. Days with southwesterly WD have a high afternoon peak and a lower morning peak, while days with northwesterly WD have a high morning peak and a lower afternoon peak. Furthermore, the seasonal variations of PDC are dominated by the seasonal frequency of WD classes. This study presents a general overview of the PDC in Germany with regard to its variation with seasonality, geographical location, elevation, and WD.
IntroductionGlobally, the diurnal amplitude variation of the precipitation frequency exceeds 20% of the mean daily values [1]. The precipitation diurnal cycle (PDC) emerges from fluctuations in global radiation. This is evident, especially in the tropics, where solar forcing is at its maximum. The PDC in mid-and high latitudes is influenced by frontal systems and topography, among other factors [1][2][3]. The PDC and its temporal and spatial variations have been addressed on global and local scales using the vast amount of precipitation records available at high resolution. Studying and understanding the PDC are important because of its applications in atmospheric science and hydrology. It interacts with the changes in surface temperatures, cloud formation processes, and boundary layer development [4][5][6], and affects the trace gas concentrations [7]. PDC influences the risk of floods and must be taken into consideration in hydrological models and designs [8,9]. Furthermore, it aids in the development of numerical weather models, which struggle to improve their representation of the PDC [10][11][12]. Such a challenge has been studied recently [13][14][15][16], particularly because the accuracy of a climate model on a daily scale reflects its quality in properly representing the physical processes or in parameterizing them.