The Younger Dryas cold event was caused by meltwater pulses disrupting ocean circulation
The claim that the Younger Dryas cold event was triggered by meltwater pulses disrupting ocean circulation is well-supported by paleoclimate modeling and ocean circulation proxies.
Papers [1] and [4] provide direct support for the widely accepted hypothesis that North Atlantic meltwater input disrupted ocean circulation (specifically weakening the AMOC) and caused the Younger Dryas cold event. Papers [0], [2], and [3] discuss meltwater pulse 1A/1B or sea-level records but do not refute the overarching consensus on the Younger Dryas trigger mechanism.
Jean Lynch‐Stieglitz, Matthew W. Schmidt, William B. Curry. Evidence from the Florida Straits for Younger Dryas ocean circulation changes. 2011. https://doi.org/10.1029/2010pa002032
Paper [1] supports the premise by showing that ocean circulation (Atlantic meridional overturning circulation) was abruptly reduced during the Younger Dryas.
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Jie Wu, Zhengguo Shi, Yongheng Yang. Response of East Asian summer monsoon climate to North Atlantic meltwater during the Younger Dryas. 2023. https://doi.org/10.5194/egusphere-egu23-6376
Paper [4] supports the claim by stating that the Younger Dryas event is widely accepted to result from meltwater fluxes injected into the North Atlantic.
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