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Millennial-scale interaction between the East Asian winter monsoon and El Niño-related tropical Pacific precipitation in the Holocene

Dong, Jiang (author)
Chinese Ministry of Natural Resources,Institute of Oceanology, Chinese Academy of Sciences
Li, Anchun (author)
Qingdao National Laboratory for Marine Science and Technology,Institute of Oceanology, Chinese Academy of Sciences
Lu, Zhengyao (author)
Lund University,Lunds universitet,BECC: Biodiversity and Ecosystem services in a Changing Climate,Centrum för miljö- och klimatvetenskap (CEC),Naturvetenskapliga fakulteten,MERGE: ModElling the Regional and Global Earth system,Institutionen för naturgeografi och ekosystemvetenskap,Centre for Environmental and Climate Science (CEC),Faculty of Science,Dept of Physical Geography and Ecosystem Science
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Liu, Xiting (author)
Qingdao National Laboratory for Marine Science and Technology,Ocean University of China
Wan, Shiming (author)
Institute of Oceanology, Chinese Academy of Sciences,Qingdao National Laboratory for Marine Science and Technology
Yan, Hong (author)
State Key Laboratory of Loess and Quaternary Geology
Yu, Zhaojie (author)
Institute of Oceanology, Chinese Academy of Sciences
Feng, Xuguang (author)
Nanjing University
Shi, Xuefa (author)
Qingdao National Laboratory for Marine Science and Technology,Chinese Ministry of Natural Resources
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 (creator_code:org_t)
Elsevier BV, 2021
2021
English.
In: Palaeogeography, Palaeoclimatology, Palaeoecology. - : Elsevier BV. - 0031-0182. ; 573
  • Journal article (peer-reviewed)
Abstract Subject headings
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  • Both the East Asian winter monsoon (EAWM) and El Niño (EN) activities are vital climate modes that regulate the Pacific hydrologic cycle. However, the Holocene interactions among the EAWM, EN activities, and tropical Pacific precipitation remain unclear due to the lack of appropriate EAWM proxies. Here, we present high-resolution grain size records from the East China Sea shelf along with a transient climate model simulation to study the Holocene EAWM evolution and compare the findings with paleo-EN precipitation-related proxies records. The millennial-scale oscillations of grain size records, which are indicative of the intensity of the EAWM-driven coastal current, reveal an anti-phase coupling between the EAWM and EN-related tropical Pacific precipitation on a millennial timescale since 5.8 ka. These results, which are consistent with simulation results, indicate that the intensified EAWM could not only reduce equatorial western Pacific precipitation by reducing the sea surface temperature but also likely change boundary conditions in the tropical Pacific (i.e., the east-west Pacific temperature gradient and westerly anomaly) to favor the formation of subsequent intensive EN activities. The enhanced EN activities, inferred by the positive tropical eastern Pacific precipitation anomalies, could subsequently suppress the EAWM through anomalous low-level anticyclones and associated southerly anomalies, thereby generating intensified tropical western Pacific (mainly tropical monsoon areas) precipitation. Our study highlights these intrinsic interactions during the mid- to late Holocene and has useful implications for understanding this millennial-scale climate oscillation, which may represent periodic atmospheric exchange between high- and low-latitude climate systems by mediating the EAWM.

Subject headings

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Klimatforskning (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Climate Research (hsv//eng)

Keyword

Anticyclone
East China Sea
Grain size
Latent heat flux
TRACE simulation
Westerly anomaly

Publication and Content Type

art (subject category)
ref (subject category)

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