title: Anomalies of temperature and annual runoff of the Danube River in the wide range of solar variability scales
abstract: Analyzed is the variability of precipitation in the area of the southern coast of the Crimea and the Danube River catchment as well as of the Danube River runoff. It is demonstrated that minimum precipitation and minimum runoff of the Danube River were observed in the years with the minimum of the quasicentennial cycle of solar activity (1879–1933), when the index of North Atlantic Oscillation (NAO) was maximum. The precipitation and the Danube River runoff were maximum in the years with the qua
journal: Russian Meteorology and Hydrology