We study the dynamics of atmospheric motions
from mesoscale to global scale, with a focus on the upper troposphere and lower stratosphere.
We employ nonhydrostatic numerical models, global meteorological fields,
satellite constituent distributions, and aircraft flight
data to better understand the general circulation and
dynamical transport mechanisms. A primary theme is to explore
the role of inertial instability in midlatitude and tropical cyclones.
The University of Wisconsin Nonhydrostatic Modeling System (UWNMS), theory, and observations are used to investigate
the role of inertial instability and PV dipoles created by convective updrafts and downdrafts in Upper Midwest severe weather events.
UTLS PV dipoles and tropical cyclones
Dynamical and climatological studies of inertial instability and UTLS PV dipoles in tropical cyclones with nonhydrostatic numerical models and high resolution global data sets.
Tropopause Folds, Midlatitude Cyclones, and Jets
Numerical simulations and aircraft flight data are used to investigate the cause of tropopause folds, constituent transport, and the role of inertial instability in midlatitude cyclones and westerly jets.
Influence of the QBO on the UTLS
Climatological investigations into the influence of the stratospheric quasi-biennial oscillation (QBO) on the tropical and subtropical tropopause environment.