18The climate of Chilean Patagonia is strongly influenced by the southern westerlies, which 19 control the amount and latitudinal distribution of precipitation in the southern Andes. In 20 austral summer, the Southern Westerly Wind Belt (SWWB) is restricted to the high latitudes. 21It expands northward in winter, which results in a strong precipitation seasonality between 22 ~35 and 45°S. Here, we present a new precipitation seasonality proxy record from Quitralco 23 fjord (46°S), where relatively small latitudinal shifts in the SWWB result in large changes in 24 precipitation seasonality. Our 1400 yr record is based on sedimentological and geochemical 25 data obtained on a sediment core collected in front of a small river that drains the 26 2 Patagonian Andes, which makes this site particularly sensitive to changes in river discharge. 27Our results indicate Fe/Al and Ti/Al values that are low between 600 and 1200 CE, increasing 28 at 1200-1500 CE, and high between 1500 and 1950 CE. Increasing Fe/Al and Ti/Al values 29 reflect a decrease in mean sediment grain-size from 30 to 20 µm, which is interpreted as a 30 decrease in seasonal floods resulting from an equatorward shift of the SWWB. Our results 31 suggest that, compared to present-day conditions, the SWWB was located in a more 32 poleward position before 1200 CE. It gradually shifted towards the equator in 1200-1500 CE, 33where it remained in a sustained position until 1950 CE. This pattern is consistent with most 34 precipitation records from central and southern Chile. The comparison of our record with 35 published regional sea surface temperature (SST) reconstructions for the late Holocene 36shows that equatorward shifts in the SWWB are systematically coeval with decreasing SSTs 37 and vice versa, which resembles fluctuations over glacial-interglacial timescales. We argue 38 that the synchronicity between SST and SWWB changes during the last 1400 years 39 represents the response of the SWWB to temperature changes in the Southern Hemisphere. 40
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Keywords 42Southern westerlies, inorganic geochemistry, paleohydrology, paleohydroclimatology, fjord 43 sediments, southern South America, Chilean Patagonia 44 45
Introduction 46The southern westerlies are the prevailing winds at the mid latitudes of the Southern 47Hemisphere, blowing between the subtropical anticyclone and the cyclonic subpolar air 48 masses. The Southern Westerly Wind Belt (SWWB) extends roughly between 30 and 60ºS, 49and it exhibits latitudinal variations at seasonal to glacial-interglacial timescales. Due to the 50 3 absence of continental barriers in the Southern Ocean, the SWWB directly controls the 51 strength of the Antarctic Circumpolar Current (ACC), which in turn affects the release of CO 2 52 from the deep ocean up to the atmosphere, particularly on glacial-interglacial timescales 53 (Anderson et al., 2009). In addition to modulating the strength of the ACC, the SWWB also 54 controls the amount of precipitation on the windward side of the mountain ranges located 55 along its ...