Ice Age Terminations

@article{Cheng2009IceAT,
  title={Ice Age Terminations},
  author={Hai Cheng and Richard Lawrence Edwards and Wallace S. Broecker and George H. Denton and Xinggong Kong and Yongjin Wang and Rong-Hua Zhang and Xianfeng Wang},
  journal={Science},
  year={2009},
  volume={326},
  pages={248 - 252}
}
Monsoon Cave Recordings Rocky deposits in caves in central China record the changes over time in the Asian Monsoon through the oxygen isotopic composition of the minerals from which they are formed. These deposits can be precisely dated and provide an absolute time line for climate system changes. Cheng et al. (p. 248; see the Perspective by Severinghaus) present oxygen isotope data from speleothems collected from Sanbao Cave, China, for the three glacial terminations that occurred between 120… 
The Asian monsoon over the past 640,000 years and ice age terminations
TLDR
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TLDR
It is found that the records close to the monsoon moisture source show large glacial-interglacial variability, which then decreases landward, the moisture transport pathway effect, which counteracts the forcing of glacial boundary conditions.
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Carbonate cave deposits in India and China are assumed to record the intensity of monsoon precipitation, because the 18 O of the carbonate tracks the isotopic signature of precipitation. These
Direct measurements of deglacial monsoon strength in a Chinese stalagmite
Chinese speleothems (cave deposits) preserve a remarkable paleoclimate record in their oxygen isotope ratios (δ 18 O); the precise interpretation of this record has been the subject of stimulating
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Paleoclimate data from the Okhotsk Sea (OS) over Terminations II and I (TII, TI), and the Last and Present Interglacial (LIG, PIG) periods were compiled in order to examine Northern Hemisphere
The Preboreal-like Asian monsoon climate in the early last interglacial period recorded from the Dark Cave, Southwest China
Abstract Transitions of glacial-interglacial cycles are critical periods for Quaternary climate shifts. Here, we present new, decadal resolution Asian summer monsoon (ASM) record from three
Interglacial Hydroclimate in the Tropical West Pacific Through the Late Pleistocene
TLDR
A stalagmite-based reconstruction of tropical West Pacific hydroclimate from 570 to 210 ka suggests that tropical hydroclimate was insensitive to interglacial differences in Pco2 and high-latitude temperature, implying that the tropical convective heat engine can either stabilize or amplify global climate change, depending on the nature of the climate forcing.
Deglaciation in the tropical Indian Ocean driven by interplay between the regional monsoon and global teleconnections
Abstract High resolution climate records of the ice age terminations from monsoon-dominated regions reveal the interplay of regional and global driving forces. Speleothem records from Chinese caves
Precession and glacial-cycle controls of monsoon precipitation isotope changes over East Asia during the Pleistocene
Abstract Precipitation isotope reconstructions derived from speleothems and plant waxes are important archives for understanding hydroclimate dynamics. Their climatic significance in East Asia,
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