Dr. Cedrick Ansorge-September 8 BUL Seminar
Scale dependence of Monin–Obukhov similarity theory — Sampling convergence and surface-layer closure
Jinxin Wang-April 28
Urban Heat Island in the Dallas-Fort Worth during Dry and Wet Summers: An Evaluation of Single-layer and Multi-layer Urban Canopy Models
Elizabeth Smith-April 21
The Great Plains low-level jet during PECAN: observations, simulations, and ongoing analyses
Ryan Lagerquist-March 31
Machine Learning for Real-time Prediction of Damaging Straight-line Convective Wind
Larissa Reames-March 24th
Influence of a Great Plains urban environment on a simulated supercell
Observations of Moisture Increases During the Southern Great Plains Afternoon to Evening Transition
In-Situ measurements and remotely sensed estimations of surface fluxes over the Southern Great Plains of the United States.
Evapotranspiration (ET) is an important variable in the hydrologic cycle. As such, improved understanding of the spatial and temporal variability of ET is critical to weather and climate analysis and prediction, water management resources, agriculture, land-use and land-change projects, and ecological research.
