Articles | Volume 31
https://doi.org/10.5194/sd-31-1-2022
https://doi.org/10.5194/sd-31-1-2022
Science report
 | 
28 Oct 2022
Science report |  | 28 Oct 2022

A synthesis of monsoon exploration in the Asian marginal seas

Peter D. Clift, Christian Betzler, Steven C. Clemens, Beth Christensen, Gregor P. Eberli, Christian France-Lanord, Stephen Gallagher, Ann Holbourn, Wolfgang Kuhnt, Richard W. Murray, Yair Rosenthal, Ryuji Tada, and Shiming Wan

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Cited articles

Abram, N. J., Hargreaves, J. A., Wright, N. M., Thirumalai, K., Ummenhofer, C. C., and England, M. H.: Palaeoclimate perspectives on the Indian Ocean Dipole, Quaternary Sci. Rev., 237, 106302, https://doi.org/10.1016/j.quascirev.2020.106302, 2020. 
Acosta, R. P. and Huber, M.: Competing Topographic Mechanisms for the Summer Indo-Asian Monsoon, Geophys. Res. Lett., 47, e2019GL085112, https://doi.org/10.1029/2019GL085112, 2020. 
Adhikari, S. K., Sakai, T., and Yoshida, K.: Data report: grain size analysis of Bengal Fan sediments at Sites U1450 and U1451, IODP Expedition 354, Proceedings of the International Ocean Discovery Program, College Station, TX, 354, https://doi.org/10.14379/iodp.proc.354.202.2018, 2018. 
Ali, S., Hathorne, E. C., and Frank, M.: Persistent Provenance of South Asian Monsoon-Induced Silicate Weathering Over the Past 27 Million Years, Paleoceanography and Paleoclimatology, 36, e2020PA003909, https://doi.org/10.1029/2020PA003909, 2021. 
Allen, M. B. and Armstrong, H. A.: Reconciling the Intertropical Convergence Zone, Himalayan/Tibetan tectonics, and the onset of the Asian monsoon system, J. Asian Earth Sci., 44, 36–47, https://doi.org/10.1016/j.jseaes.2011.04.018, 2012. 
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Short summary
An integrated campaign of drilling around Asia and Australia was conducted from 2013 to 2016 to reconstruct the monsoon climate. The results provide relatively continuous records spanning the last 24 myr. Asia has shown a steady drying since the late Miocene, while Australia has become wetter. The monsoons are affected by the tectonics of Asia and surrounding seas, as well as orbital forcing, resulting in diachronous evolution of continental climate, ocean currents, and the marine biosphere.