William R. Boos

Jan 5, 2024 | wcd.copernicus.org | Michael Byrne |William R. Boos |Shineng Hu

Bliss, A., Hock, R., and Radić, V.: Global response of glacier runoff to twenty-first century climate change, J. Geophys. Res.-Earth, 119, 717–730, https://doi.org/10.1002/2013JF002931, 2014. a Byrne, M. P. and O'Gorman, P. A.: Land–ocean warming contrast over a wide range of climates: Convective quasi-equilibrium theory and idealized simulations, J. Climate, 26, 4000–4016, 2013.

Oct 19, 2023 | nature.com | Yongyun Hu |Xiang Li |William R. Boos |Jiaqi Guo |Jiawenjing Lan |Jing Han | +7 more

AbstractGeologic evidence and palaeoclimate simulations have indicated the existence of an extensive, interconnected megamonsoon system over the Pangaea supercontinent. However, the ways in which subsequent continental break-up about 180 million years ago and reassembly in the Cenozoic, as well as large global climatic fluctuations, influenced the transition to the modern global monsoon system are uncertain.