Abstract. The study of El Niño–Southern Oscillation (ENSO)’s role in modifying past climates can provide valuable insights into the sensitivity of the present-day hydroclimate to changing ENSO characteristics. In this study, a water isotope-enabled atmospheric general circulation model (ECHAM4.6) is utilized to examine the impact of two aspects of mid-Holocene ENSO characteristics on South American precipitation and precipitation δ18O: 1) Reduced amplitude of ENSO variability (relative to present-day) and 2) a mid-Holocene La Niña-like mean state in tropical Pacific sea-surface temperatures (SST), but with modern-day ENSO variability. Additionally, we conducted a lower Southern Hemisphere summertime insolation (SHSI) experiment to investigate the role of orbital forcing. Our results show that decreased ENSO variability results in a minor change in the climatological precipitation. In contrast, a La Niña-like mean state results in an east–west dipole pattern of rainfall change comparable to the effect of lower SHSI; however, the dipole pattern is not mirrored in precipitation δ18O. The experiments suggest that mid-Holocene western Amazon δ18O is influenced by reduced SHSI by decreasing precipitation seasonality and drives positive δ18O anomalies, while ENSO mean state changes suppress winter precipitation, leading to negative δ18O anomalies. These opposing effects highlight the additional role of global SST feedbacks in shaping western Amazon δ18O. In contrast, in the northeastern Amazon, both SHSI and ENSO mean state changes directly influence precipitation δ18O, resulting in strong negative δ18O anomalies. Overall, these findings emphasize the combined effects of ENSO variability, tropical Pacific SSTs, and orbital forcing on South American precipitation and δ18O during the mid-Holocene.
Wong et al. (Fri,) studied this question.