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Orbital modulation of subtropical versus subantarctic moisture sources in the southeast Pacific mid-latitudes
Kaiser, J.; Schefuß, E.; Collins, J.; Garreaud, R.; Stuut, J.-B.W.; Ruggieri, N.; De Pol-Holz, R.; Lamy, F. (2024). Orbital modulation of subtropical versus subantarctic moisture sources in the southeast Pacific mid-latitudes. Nature Comm. 15(1): 7512. https://dx.doi.org/10.1038/s41467-024-51985-4
In: Nature Communications. Nature Publishing Group: London. ISSN 2041-1723; e-ISSN 2041-1723, meer
Peer reviewed article  
Beschikbaar in  Auteurs 
Author keywords
    Geochemistry; Palaeoclimate
Auteurs  Top 
  • Kaiser, J.
  • Schefuß, E.
  • Collins, J.
  • Garreaud, R.
  • Stuut, J.-B.W., meer
  • Ruggieri, N.
  • De Pol-Holz, R.
  • Lamy, F.
Abstract
    Reconstructing rainfall variability and moisture sources is a critical aspect to understand past and future hydroclimate dynamics. Here, we use changes in the deuterium content of land-plant leaf waxes from two marine sediment cores located off Chile to reconstruct changes in rainfall amount and variation in moisture sources over the last ~50 ka. The records indicate increased moisture in central Chile during precession maxima, but an obliquity modulation is evident in southern Chile. While the southern westerly winds are the dominant factor of precipitation in southern Chile by bringing moisture and perturbations from the extratropics, the subtropics represent an additional moisture source during precession maxima due to a stronger subtropical jet increasing moisture transport from the tropics to the mid-latitudes. These findings imply that a combination of orbital modulation of moisture sources and rainfall amount explains the last glacial moisture maximum and early Holocene moisture minimum in south-central Chile.
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