Zhonghui Liu, Ph.D.
Affiliations: | 2004 | Brown University, Providence, RI |
Area:
Geology, GeophysicsGoogle:
"Zhonghui Liu"Mean distance: (not calculated yet)
Parents
Sign in to add mentor| Timothy D. Herbert | grad student | 2004 | Brown | |
| (Pleistocene climate evolution in the eastern Pacific and implications for the orbital theory of climate change.) | ||||
BETA: Related publications
See more...
Publications
|
You can help our author matching system! If you notice any publications incorrectly attributed to this author, please sign in and mark matches as correct or incorrect. |
| Zhang R, Liu Z, Jiang D, et al. (2024) Cenozoic Indo-Pacific warm pool controlled by both atmospheric CO and paleogeography. Science Bulletin |
| Jiang J, Meng B, Wang H, et al. (2024) Spatial patterns of Holocene temperature changes over mid-latitude Eurasia. Nature Communications. 15: 1507 |
| Herbert TD, Dalton CA, Liu Z, et al. (2022) Tectonic degassing drove global temperature trends since 20 Ma. Science (New York, N.Y.). 377: 116-119 |
| Jiang Q, Meng B, Wang Z, et al. (2021) Exceptional terrestrial warmth around 4200-2800 years ago in Northwest China. Science Bulletin. 67: 427-436 |
| Ao H, Rohling EJ, Zhang R, et al. (2021) Global warming-induced Asian hydrological climate transition across the Miocene-Pliocene boundary. Nature Communications. 12: 6935 |
| Zhang Y, Zheng X, Kong D, et al. (2021) Enhanced North Pacific subtropical gyre circulation during the late Holocene. Nature Communications. 12: 5957 |
| Zhao C, Rohling EJ, Liu Z, et al. (2020) Possible obliquity-forced warmth in southern Asia during the last glacial stage. Science Bulletin. 66: 1136-1145 |
| Ao H, Dupont-Nivet G, Rohling EJ, et al. (2020) Orbital climate variability on the northeastern Tibetan Plateau across the Eocene-Oligocene transition. Nature Communications. 11: 5249 |
| Liu W, Liu Z, Sun J, et al. (2020) Onset of permanent Taklimakan Desert linked to the mid-Pleistocene transition Geology. 48: 782-786 |
| Zhong Y, Chen Z, Hein JR, et al. (2020) Evolution of a deep-water ferromanganese nodule in the South China Sea in response to Pacific deep-water circulation and continental weathering during the Plio-Pleistocene Quaternary Science Reviews. 229: 106106 |