This study quantiﬁes the impact of atmospheric rivers (ARs) on precipitation in southern South America. An AR detection algorithm was developed based on integrated water vapor transport (IVT) from 6-hourly CFSR reanalysis data over a 16-yr period (2001–16). AR landfalls were linked to precipitation using a comprehensive observing network that spanned large variations in terrain along and across the Andes from 278 to 558S, including some sites with hourly data. Along the Paciﬁc (west) coast, AR landfalls are most frequent between 388 and 508S, averaging 35–40 days yr21. This decreases rapidly to the south and north of this maximum, as well as to the east of the Andes. Landfalling ARs are more frequent in winter/spring (summer/fall) to the north (south) of ;438S. ARs contribute 45%–60% of the annual precipitation in subtropical Chile (378–328S) and 40%–55% along the midlatitude west coast (378–478S). These values signiﬁcantly exceed those in western North America, likely due to the Andes being taller. In subtropical and midlatitude regions, roughly half of all events with top-quartile precipitation rates occur under AR conditions. Median daily and hourly precipitation in ARs is 2–3 times that of other storms. The results of this study extend knowledge of the key roles of ARs on precipitation, weather, and climate in the South American region. They enable comparisons with other areas globally, provide context for speciﬁc events, and support local nowcasting and forecasting.