This article provides a comprehensive review of the global monsoon that encompasses
findings from studies of both modern monsoons and paleomonsoons. We introduce a …
findings from studies of both modern monsoons and paleomonsoons. We introduce a …
Millennial-and orbital-scale changes in the East Asian monsoon over the past 224,000 years
High-resolution speleothem records from China have provided insights into the factors that
control the strength of the East Asian monsoon,,,. Our understanding of these factors …
control the strength of the East Asian monsoon,,,. Our understanding of these factors …
Chinese stalagmite δ18O controlled by changes in the Indian monsoon during a simulated Heinrich event
Carbonate cave deposits in India and China are assumed to record the intensity of monsoon
precipitation, because the δ18O of the carbonate tracks the isotopic signature of …
precipitation, because the δ18O of the carbonate tracks the isotopic signature of …
Variability of stalagmite-inferred Indian monsoon precipitation over the past 252,000 y
A speleothem δ18O record from **aobailong cave in southwest China characterizes
changes in summer monsoon precipitation in Northeastern India, the Himalayan foothills …
changes in summer monsoon precipitation in Northeastern India, the Himalayan foothills …
[HTML][HTML] Indian monsoon variability on millennial-orbital timescales
The Indian summer monsoon (ISM) monsoon is critical to billions of people living in the
region. Yet, significant debates remain on primary ISM drivers on millennial-orbital …
region. Yet, significant debates remain on primary ISM drivers on millennial-orbital …
Glacial-interglacial Indian summer monsoon dynamics
A Zhisheng, SC Clemens, J Shen, X Qiang, Z **… - science, 2011 - science.org
The modern Indian summer monsoon (ISM) is characterized by exceptionally strong
interhemispheric transport, indicating the importance of both Northern and Southern …
interhemispheric transport, indicating the importance of both Northern and Southern …
Chinese stalagmite paleoclimate researches: A review and perspective
Stalagmite is one kind of secondary carbonates formed in limestone caves (speleothem).
After cave water droplets containing Ca 2+ and HCO _3^-HCO 3− drip onto floor, carbonate …
After cave water droplets containing Ca 2+ and HCO _3^-HCO 3− drip onto floor, carbonate …