Skip to main content Skip to secondary navigation
Satellite image of storms

Hurricane Florence, TS Isaac, Hurricane Helene 2018

Main content start

Severe Weather and Climate Group @ Stanford

The Severe Weather and Climate Group at Stanford is led by Dr. Morgan O'Neill in the Department of Earth System Science. We study the dynamics and thermodynamics of multiscale severe events, including supercell thunderstorms and hurricanes. The two-way feedbacks between these storms and the climate in which they occur is of importance to meteorologists, climate scientists and planetary scientists. In a changing climate, it is critical to accurately predict how the extremes to which we are accustomed will change in the future. The past and present climates of Earth, as well as those of other planets in our solar system, serve as physical laboratories in which we can observe a range of extreme phenomena.

The tools that our group uses to address these questions are varied, from simple theory and observations to complex numerical models that simulate realistic atmospheric phenomena. Because of the impossibility of recreating all the complexities of the atmosphere in a laboratory, our laboratory is a hierarchy of numerical models that approximate the equations of motion. Ultimately, numerical results and theoretical understanding must be tested against observations. We collaborate with other scientists and institutions to take the observations we need to validate our work. Our focus is on the genesis, evolution and environmental interaction of convective storms in a range of climates.

New paper out in Science

10 September 2021

science-mag-cover

Hydraulic jump dynamics above supercell thunderstormsby Morgan O'Neill, Leigh Orf @ U. Wisconsin Madison, Gerald Heymsfield @ NASA Goddard, and Kelton Halbert @ U. Wisconsin Madison

We find that the above-anvil cirrus plume (AACP), found above some thunderstorms and before some of the most severe weather on Earth, is the visible manifestation of a new type of hydraulic jump: one that is forced by the overshooting top of the thunderstorm itself. The lower boundary of the jump is a moving fluid of nearly the same composition as the air above it.

See Science's video explainer here:

 

Image is of Hurricane Irma (2017) on Sept. 6th in the infrared, courtesy NOAA.

Image is of Hurricane Irma (2017) on Sept. 6th in the infrared, courtesy NOAA.

Two hurricane hunting aircraft flying side by side

Tropical Cyclone Diurnal Cycle Experiment

Our group is participating in the 2021 NOAA AOML/Hurricane Research Division field campaign: the Advancing the Prediction of Hurricanes EXperiment (APHEX). We deployed dropsondes from the NOAA Hurricane Hunter planes into Hurricane Larry this year and Hurricane Teddy last year to better understand the diurnal cycle, with scientists at NOAA, Florida State University and Purdue University. Due to the pandemic, we participate remotely. All observations from our and other HRD experiments are available to the public shortly after they are processed, and can be accessed here. Image courtesy the National Oceanographic and Atmospheric Administration (NOAA).

Gulfstream IV flight path through Hurricane Teddy, 6 September 2021

Observing Hurricane Larry (2021)

We had a successful diurnal cycle experiment flight through Hurricane Larry on 6 September, 2021, after a nearly identical flight pattern through Larry the previous day. The plane was the NOAA Gulfstream-IV, "Gonzo", with a flight crew of scientists and engineers. Each blue dot on the flight path indicates where a dropsonde was released to measure wind, temperature, humidity and pressure as it falls toward the ocean surface. These data, taken at different times for each flight day, will help us better understand the diurnal pulse of convection seen to propagate outward at the hurricane's cloud top.