End of Green Sahara amplified mid- to late Holocene megadroughts in mainland Southeast Asia

• Published in: Nature communications Vol. 11; no. 1; p. 4204
• Main Authors: Griffiths, Michael L., Johnson, Kathleen R., Pausata, Francesco S. R., White, Joyce C., Henderson, Gideon M., Wood, Christopher T., Yang, Hongying, Ersek, Vasile, Conrad, Cyler, Sekhon, Natasha
• Format: Journal Article
• Language: English
• Published: London Nature Publishing Group UK 21.08.2020; Nature Publishing Group; Nature Portfolio
• Subjects: 140/58; 704/106/35/823; 704/106/413; Archaeology; Atmospheric dynamics; Atmospheric models; Catalysts; Climate; Drying; Dust; ENVIRONMENTAL SCIENCES; Holocene; Humanities and Social Sciences; Monsoons; multidisciplinary; palaeoclimate; Rain; Rainfall; Science; Science (multidisciplinary); Vegetation; Wind; Southeast Asia
• ISSN: 2041-1723; 2041-1723
• DOI: 10.1038/s41467-020-17927-6

Between 5 and 4 thousand years ago, crippling megadroughts led to the disruption of ancient civilizations across parts of Africa and Asia, yet the extent of these climate extremes in mainland Southeast Asia (MSEA) has never been defined. This is despite archeological evidence showing a shift in human settlement patterns across the region during this period. We report evidence from stalagmite climate records indicating a major decrease of monsoon rainfall in MSEA during the mid- to late Holocene, coincident with African monsoon failure during the end of the Green Sahara. Through a set of modeling experiments, we show that reduced vegetation and increased dust loads during the Green Sahara termination shifted the Walker circulation eastward and cooled the Indian Ocean, causing a reduction in monsoon rainfall in MSEA. Our results indicate that vegetation-dust climate feedbacks from Sahara drying may have been the catalyst for societal shifts in MSEA via ocean-atmospheric teleconnections. The mid-Holocene has seen a number of climate shifts, which have been associated with societal changes. Here, the authors investigate in a centuries long megadrought in Southeast Asia during the mid-Holocene, possibly caused by the end of the Green Sahara period.