Journal
GEOPHYSICAL RESEARCH LETTERS
Volume 47, Issue 21, Pages -Publisher
AMER GEOPHYSICAL UNION
DOI: 10.1029/2020GL090273
Keywords
Asian summer monsoon; abrupt events; speleothem; Loess Plateau; northern China; Holocene
Categories
Funding
- Strategic Priority Research Program of CAS [XDB40000000]
- NSFC [41372192, 41888101]
- CAS PIFI Program [2020VCA0019]
- USA NSF [0908792, 1211299, 1702816]
- 111 program of China [D19002]
- Belt & Road Center for Climate and Environment Studies of IEECAS
- Directorate For Geosciences
- Division Of Earth Sciences [0908792, 1211299] Funding Source: National Science Foundation
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Here we present, to date, the highest-resolved (similar to 5 years) and most precisely dated Holocene monsoon climate reconstruction for the western Chinese Loess Plateau based on five replicated stalagmite delta O-18 records from Wuya Cave, eastern Gansu, China. Our record suggests the wettest period occurred between 10,500 and 6,600 a BP in this region. After this period, the amplitude of Asian summer monsoon decadal-scale variability progressively increased likely in response to increasing ENSO frequency since the middle Holocene. Our study reveals similar asymmetric centennial-scale double-plunging structures of the 8.2, 5.5, and 2.8 ka events in the western Chinese Loess Plateau, suggesting a possible role of solar activity whose impact was amplified around 8.2 ka BP by the meltwater flood. In contrast, the 4.2 ka event exhibit gradually declining monsoon rainfall with centennial- to decadal-scale fluctuations.
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