http://ruby.fgcu.edu/courses/twimberley/envirophilo/wanner.pdf

Mid- to Late Holocene climate change: an overview

https://boris.unibe.ch/62575/1/1-s2.0-S0277379114003485-main.pdf

A stratigraphic framework for abrupt climatic changes during the Last Glacial period based on three synchronized Greenland ice-core records: refining and extending the INTIMATE event stratigraphy

Surface temperature reconstructions of the past 1500 years suggest that recent warming is unprecedented in that time. Here we provide a broader perspective by reconstructing regional and global temperature anomalies for the past 11,300 years from 73 globally distributed records. Early Holocene (10,000 to 5000 years ago) warmth is followed by ~0.7°C cooling through the middle to late Holocene (<5000 years ago), culminating in the coolest temperatures of the Holocene during the Little Ice Age, about 200 years ago. This cooling is largely associated with ~2°C change in the North Atlantic. Current global temperatures of the past decade have not yet exceeded peak interglacial values but are warmer than during ~75% of the Holocene temperature history. Intergovernmental Panel on Climate Change model projections for 2100 exceed the full distribution of Holocene temperature under all plausible greenhouse gas emission scenarios.

/pdf/a-reconstruction-of-regional-and-global-temperature-for-the-v46ufkdlme.pdf

A Reconstruction of Regional and Global Temperature for the Past 11,300 Years

https://www.lehigh.edu/~ziy2/pubs/Chen2008QSR.pdf

Holocene moisture evolution in arid central Asia and its out-of-phase relationship with Asian monsoon history

Rainfall on Earth is most intense in the intertropical convergence zone (ITCZ), a narrow belt of clouds centred on average around six degrees north of the Equator. The mean position of the ITCZ north of the Equator arises primarily because the Atlantic Ocean transports energy northward across the Equator, rendering the Northern Hemisphere warmer than the Southern Hemisphere. On seasonal and longer timescales, the ITCZ migrates, typically towards a warming hemisphere but with exceptions, such as during El Nino events. An emerging framework links the ITCZ to the atmospheric energy balance and may account for ITCZ variations on timescales from years to geological epochs.

Migrations and dynamics of the intertropical convergence zone

A 5-year-resolution absolute-dated oxygen isotope record from Dongge Cave, southern China, provides a continuous history of the Asian monsoon over the past 9000 years. Although the record broadly follows summer insolation, it is punctuated by eight weak monsoon events lasting approximately 1 to 5 centuries. One correlates with the "8200-year" event, another with the collapse of the Chinese Neolithic culture, and most with North Atlantic ice-rafting events. Cross-correlation of the decadal- to centennial-scale monsoon record with the atmospheric carbon-14 record shows that some, but not all, of the monsoon variability at these frequencies results from changes in solar output.

https://science.sciencemag.org/content/sci/308/5723/854.full.pdf

Yaoqi He

Papers

The holocene Asian monsoon : links to solar changes and North Atlantic climate

Sub-millennial variability of Asian monsoon intensity during the early MIS 3 and its analogue to the ice age terminations

Strong link between Asian summer monsoon and westerlies for the past 4750 years

Yaoqi He

Papers

The holocene Asian monsoon : links to solar changes and North Atlantic climate

Sub-millennial variability of Asian monsoon intensity during the early MIS 3 and its analogue to the ice age terminations

Strong link between Asian summer monsoon and westerlies for the past 4750 years

Strong link between Asian summer monsoon and westerlies for the past 4750 years