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  4. Precipitation response to Heinrich Event-3 in the northern Indochina as revealed in a high-resolution speleothem record
 
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Precipitation response to Heinrich Event-3 in the northern Indochina as revealed in a high-resolution speleothem record

Journal
Journal of Asian Earth Sciences: X
Journal Volume
7
Date Issued
2022-06-01
Author(s)
Nguyen, Dung Chi
Lee, Shih Yu
YUE-GAU CHEN  
Chiang, Hong Wei
CHUAN-CHOU SHEN  
Wang, Xianfeng
Doan, Lam Dinh
Lin, Yin
DOI
10.1016/j.jaesx.2022.100090
URI
https://scholars.lib.ntu.edu.tw/handle/123456789/626977
URL
https://api.elsevier.com/content/abstract/scopus_id/85126953076
Abstract
Heinrich Event-3 (HE-3) differs from other Heinrich Events (HEs) in terms of the strength of its expression in climatic records from different global localities. Here, we present new high resolution δ18O records from a composite speleothem record spanning from 31.5 to 28.4 ka within the HE-3 time interval. The record is obtained from two stalagmites collected from the Thuong Thien cave (TT), northern Vietnam, which exhibit growth rates of 0.12 to 0.68 mm/yr. The TT record shows a pronounced positive excursion of δ18O values of stalagmite in the time interval from 30.8 ka and lasted about one thousand years. Specifically, the δ18O reached maximum between ∼30.3–30.2 ka and returned to low values at 29.5 ka. Both the onset and termination phases of the excursion show gradual changes in δ18O values that form a relatively symmetric ‘V’ shape. The excursion suggests that the Indian Summer Monsoon (ISM), which modulates the climate and hydrology in the region, has endured dramatic weakening in response to HE-3. The timing and duration of the monsoonal decline are consistent with a significant slowdown of the Atlantic Meridional Ocean Circulation (AMOC), which probably drove the southward migration of the intertropical convergence zone (ITCZ) and consequently a decrease in precipitation over the Asian monsoonal region including northern Vietnam. To test the proposed mechanism, we further performed modeling simulations via an atmosphere general circulation model with a coupled slab ocean. Simulated results confirm both the scale and mechanistic connections between cooling in the North Atlantic and changes in precipitation at the Thuong Thien cave locality.
Subjects
Climate change | Heinrich event | Speleothem | Tropical Asia
SDGs

[SDGs]SDG13

[SDGs]SDG14

Type
journal article

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