Seminar by Dr. Hanna Lee
Cryosphere is where water is in its solid form. The cryosphere is changing faster than global mean under current and future warming scenarios and has great consequences to the feedback […]
Cryosphere is where water is in its solid form. The cryosphere is changing faster than global mean under current and future warming scenarios and has great consequences to the feedback […]
Ocean biogeochemistry in paleoclimate history exhibits abrupt changes in calcium carbonate preservations after CO2 emissions. During the Paleocene-Eocene Thermal Maximum (PETM) period, for example, the calcium carbonate (CaCO3) content was […]
Characteristics of tropical cyclones (TCs) in global climate models (GCMs) are known to be influenced by details in model configurations, including horizontal resolution and parameterization schemes. Understanding model-to-model differences in […]