Member Since 2016
Jiang Zhu
Project Scientist II, National Center for Atmospheric Research
AGU Research
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The runaway problem in CESM2 and climate sensitivity over a wide temperature range
AGU 2024
atmospheric sciences | 12 december 2024
Jiang Zhu, Bette L. Otto-Bliesner, Guo Zhun, Adam ...
The Community Earth System Model version 2 (CESM2) exhibits runaway behavior under realistic Eocene boundary conditions with 4× preindustrial CO2 (113...
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Quantifying Earth’s thermostat — a case study of the Middle Miocene
AGU 2024
paleoceanography and paleoclimatology | 12 december 2024
Weimin Si, Taehee Lee, Feng Zhu, Jiang Zhu, Kaustu...
The Middle Miocene was a climate optimum (MCO) characterized by warmer than present-day temperatures. The geological cause(s) for the warming, however...
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High-Resolution Simulations of Tropical Cyclones: From the Geological Past to Future Projections
AGU 2024
atmospheric sciences | 12 december 2024
Bette L. Otto-Bliesner, Esther C. Brady, Jiang Zhu...
Tropical cyclones (TCs) cause extreme precipitation, floods, storm surges, and destructive winds with devastating loss of lives and property.In this s...
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Revisiting Miocene Climatic Optimum with Equilibrated iCESM Simulations
AGU 2024
paleoceanography and paleoclimatology | 12 december 2024
Feng Zhu, Jiang Zhu, Weimin Si, Timothy Herbert
Miocene Climatic Optimum (MCO) is a geological period (~15 Ma) of great scientific interest. Its high CO2 level offers valuable insights into warm cli...
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Investigating Controls on the Isotopic Composition of Precipitation in the Continental United States using Numerical Tracers in the Community Earth System Model
AGU 2024
paleoceanography and paleoclimatology | 12 december 2024
Sophia Macarewich, Jeffrey M. Welker, Jiang Zhu, J...
Stable water isotope ratios are a powerful tool to understand past and present changes in water cycling because they incorporate the temperature and t...
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Modeling the Eocene Ocean and Marine εNd Distribution using iCESM1.2
AGU 2024
paleoceanography and paleoclimatology | 11 december 2024
Adam Aleksinski, Matthew Huber, Jiang Zhu, Alexand...
The Eocene-Oligocene Transition (EOT) ended with the first permanent Antarctic ice sheet of the Cenozoic and was thus a pivotal time slice in establis...
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Atmospheric River Responses to Past and Future Climate Change in the High-Resolution Community Earth System Model
AGU 2024
paleoceanography and paleoclimatology | 11 december 2024
Sophia Macarewich, Bette L. Otto-Bliesner, Jiang Z...
Atmospheric rivers (ARs) cause extreme precipitation, floods, and drought events, and are expected to intensify with global warming. Past climate stat...
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DeepMIP-Miocene: experimental design for model simulations of the Miocene Climatic Optimum (MioMIP2)
AGU 2024
paleoceanography and paleoclimatology | 11 december 2024
Natalie Burls, Catherine Bradshaw, Nicky Wright, R...
The Miocene Epoch, between the hot house climate of the Eocene and the more moderate warm climate of the Pliocene, has emerged as an important paleocl...
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