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Loess Plateau
Anti-phase variation of long eccentricity and precipitation in inland Asia during the Middle Miocene Climatic Optimum
East Asian summer monsoon variations across the Miocene–Pliocene boundary recorded by sediments from the Guide Basin, northeastern Tibetan Plateau
Impact liquefaction mechanism of sandy silt with a change in impact energy
100 k.y. pacing of the East Asian summer monsoon over the past five glacial cycles inferred from land snails
Dominant precessional forcing of the East Asian summer monsoon since 260 ka
Paleoclimates inform on a weakening and amplitude-reduced East Asian winter monsoon in the warming future
New constraints on the source of loess from U/Th-Pb geochronology of detrital multi-minerals
An absolutely dated record of climate change over the last three glacial–interglacial cycles from Chinese loess deposits
Separation of seismic multiple reflection-refraction based on morphological component analysis with high-resolution linear Radon transform
Lithium isotopic composition of soil pore water: Responses to evapotranspiration
Spatially variable provenance of the Chinese Loess Plateau
Review: Progress with Functional Materials Based on Loess Particles
Asian paleomonsoon variation linked to “tripolar” environmental changes
ABSTRACT Global warming and ice melting in the “tripolar” regions, namely, Antarctica, the Arctic, and the Tibetan Plateau, might lead to a reorganization of the global climate system. Understanding the dynamic links between the “tripolar” environments and the Earth climate system is crucial to improving our capability to project future climate variability. “Tripolar” changes have influenced the onset and evolution of the Asian paleomonsoon system through various atmospheric and/or oceanic mechanisms. Here, we summarize previously reported Asian paleomonsoon variations that can be linked to “tripolar” environmental changes, from tectonic to millennial time scales, and explore linkages between the “tripolar” regions and global climate changes.