Dynamical Drivers of South American Monsoon Variability over the Last Millennium

Orrison, Rebecca; Vuille, Mathias

doi:10.1002/essoar.10505906.1

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Dipole Pattern In South American Hydroclimate1

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2021

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“…The model results presented here do not support enhanced rainfall over the Amazon basin as the cause of the LIA isotopic depletion pattern in the central Andes and southern Amazon. Instead, they support upstream rainout in the monsoon entrance region in northeastern South America, as has also been found in isotope-enabled simulations with CESM (Orrison & Vuille, 2020).…”

Section: Dipole Pattern In South American Hydroclimatesupporting

confidence: 71%

Data‐Model Comparisons of Tropical Hydroclimate Changes Over the Common Era

Atwood

Battisti

et al. 2021

Paleoceanog and Paleoclimatol

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The hydrologic cycle is expected to change in profound ways under continued increases in atmospheric greenhouse gas concentrations and yet our understanding of how regional rainfall patterns will respond to anthropogenic climate change remains highly uncertain. The short (spanning roughly half a century) and unevenly distributed precipitation records around the globe currently limit our ability to constrain models and thus make confident projections of future precipitation responses (Biasutti et al., 2018). However, the efficacy of the climate models used to project future climate can be tested against past records. In particular, the last 2,000 years, known as the Common Era, has been a major reconstruction target for the paleoclimate community over the last decade (

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Section: Dipole Pattern In South American Hydroclimatesupporting

confidence: 71%