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AMOC-forced southward migration of the ITCZ under a warm climate background

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Kraft, Laura ; Campos, Marilia C. ; Nascimento, Rodrigo A. ; Dias, Bruna B. ; Crivellari, Stefano ; Kochhann, Marcus V. L. ; Bertassoli Jr, Dailson J. ; Venancio, Igor M. ; Santos, Thiago P. ; Baker, Paul A. ; Silva, Cleverson G. ; Chiessi, Cristiano M.
Total Authors: 12
Document type: Journal article
Source: PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY; v. 661, p. 10-pg., 2025-01-16.
Abstract

Northern northeastern Brazil (NEB) is a climate change hotspot due to its high biological and social vulnerability to ongoing and future hydroclimate changes. Precipitation in this region is influenced by the Intertropical Convergence Zone (ITCZ), which is largely controlled by the strength of the Atlantic Meridional Overturning Circulation (AMOC). Accordingly, the projected weakening of the AMOC due to anthropogenic global warming may substantially change NEB hydroclimate. Heinrich Stadials (HS), past millennial-scale events during which the AMOC was significantly weaker, provide important insights into the AMOC-ITCZ dynamics. This is especially true for those HS that occurred under similar to modern boundary conditions. HS10 (ca. 110 thousand years ago) was the first HS of Marine Isotope Stage 5, providing an ideal target for investigating AMOC-ITCZ dynamics under relatively warm climate conditions. Here we investigate the response of the surface and deep western equatorial Atlantic (WEA) circulation, as well as NEB precipitation to HS10. Therefore, we use foraminiferal carbon and oxygen stable isotopes and bulk sediment major elemental data from a marine sediment core retrieved from the WEA. Our results record a weakening of the AMOC during HS10 and show a concurrent increased WEA upper stratification and precipitation over NEB. We suggest that the mechanism controlling the WEA upper ocean stratification during HS depends on the background climate. Furthermore, we infer that the southward shift of the ITCZ during HS10 was more limited if compared to the shifts that occurred under colder climate background. Our findings provide useful insights into how a weakening of the AMOC under a relatively warm climate can impact the ITCZ and tropical South American precipitation. (AU)

FAPESP's process: 19/25179-0 - Penultimate glacial-to-interglacial transition in Northeastern South America and the adjacent ocean
Grantee:Marília de Carvalho Campos Garcia
Support Opportunities: Scholarships in Brazil - Post-Doctoral
FAPESP's process: 22/06440-1 - Wetland expansion in Amazonia during the late Holocene and its implications to the global methane budget
Grantee:Dailson José Bertassoli Junior
Support Opportunities: Generation Project Research Grant
FAPESP's process: 22/06452-0 - The South Atlantic on a 2°C warmer planet
Grantee:Marília de Carvalho Campos Garcia
Support Opportunities: Generation Project Research Grant
FAPESP's process: 22/09822-2 - Improvement of analytical routines and software development for analysis of carbon and oxygen stable isotopes by gas isotope ratio mass spectrometry in single specimens
Grantee:Stefano Crivellari
Support Opportunities: Scholarships in Brazil - Technical Training Program - Technical Training
FAPESP's process: 18/15123-4 - Past perspectives on tipping elements of the climate system: the Amazon Rainforest and the Atlantic Meridional Overturning Circulation (PPTEAM)
Grantee:Cristiano Mazur Chiessi
Support Opportunities: Research Grants - Research Program on Global Climate Change - Young Investigators - Phase 2
FAPESP's process: 20/11452-3 - Carbon storage changes in the mid-depth South Atlantic during the penultimate glacial termination and the Anthropocene
Grantee:Bruna Borba Dias
Support Opportunities: Scholarships in Brazil - Post-Doctoral
FAPESP's process: 19/24349-9 - Assessing the effects of past and future climate change on Amazonian biodiversity (CLAMBIO)
Grantee:Cristiano Mazur Chiessi
Support Opportunities: BIOTA-FAPESP Program - Regular Research Grants
FAPESP's process: 22/01056-9 - The application of neodymium isotopes to reconstruct AMOC variability and its role in the global carbon cycle during the last two glacial terminations
Grantee:Bruna Borba Dias
Support Opportunities: Scholarships abroad - Research Internship - Post-doctor
FAPESP's process: 21/02877-3 - Paleoceanographic evolution of the South Atlantic subtropical gyre over the past 800,000 years based on a multi-proxy approach
Grantee:Marcus Vinicius Lermen Kochhann
Support Opportunities: Scholarships in Brazil - Doctorate
FAPESP's process: 19/24977-0 - Environmental signals recorded in modern sediments of tropical South American rivers
Grantee:Dailson José Bertassoli Junior
Support Opportunities: Scholarships in Brazil - Post-Doctoral
FAPESP's process: 23/14028-6 - Orbital-scale variability of heat content in the South Atlantic Subtropical Gyre: assessing seawater temperature via Mg/Ca analysis
Grantee:Marcus Vinicius Lermen Kochhann
Support Opportunities: Scholarships abroad - Research Internship - Doctorate
FAPESP's process: 22/09479-6 - Changes in ITCZ-related precipitation over NE South America during the penultimate glacial-to-interglacial transition: assessing fluvial discharge via planktonic foraminiferal Ba/Ca
Grantee:Marília de Carvalho Campos Garcia
Support Opportunities: Scholarships abroad - Research Internship - Post-doctor