Article-Journal

Winter Patterns of the Hadley Circulation's Response to Increased CO2 are Distinct between the Upper and Lower Troposphere (in revision)

Distinguishing the Direct Radiative, Surface Warming, and Ozone Mediated Contributions to the Acceleration of the Brewer-Dobson circulation under Abrupt CO2 Forcing (in preparation)"

Replicating the Hadley Cell edge and subtropical jet latitude disconnect in idealized atmospheric models

Connections between upper tropospheric and lower stratospheric circulation responses to increased CO2

Disconnect Between Hadley Cell and Subtropical Jet Variability and Response to Increased CO2

Connecting Direct Effects of CO2 Radiative Forcing to Ocean Heat Uptake and Circulation