Publications

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

Competing Influences from Direct Radiative, Surface Warming, and Ozone Responses to Increased CO2 on the Brewer-Dobson Circulation (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