School of Meteorology (Defense)

All Faculty Meeting Student Org Events Career Development School of Meteorology Colloquium Social Event/Celebration Academic Calendar National Weather Center Colloquia Boundary Layer, Urban Meteorology and Land-Surface Processes School of Meteorology (Defense) Weather and Climate Systems Convective Meteorology (Mesoscale Dynamics)

Veronica Fall-April 24

Characteristics of the 2011-2016 California Drought

By Debbie Barnhill |
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Apr
21

Larissa Reames-April 21

Simulated effects of urban environments on the dynamics of a supercell thunderstorm

By Debbie Barnhill |
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Chris Kerr-April 17

Analysis of environmental modifications by deep convection during the Mesoscale Predictability Experiment

By Debbie Barnhill |
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Joshua Gebauer-April 12

Convection Initiation Caused by Heterogeneous Great Plains Low-Level Jets

By Debbie Barnhill |
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Amanda Kis-April 3

A phenomenological investigation of voluntary exits from the atmospheric science occupation

By Debbie Barnhill |
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Jan
17

Manda Chasteen-Defense

Most continental regions experience an afternoon or evening maximum of convective activity, which is dominated by convection driven by surface heating. However, the Great Plains of North America experiences a nocturnal maximum in convective precipitation during the warm season, which is associated with the frequent occurrence of elevated mesoscale convective systems (MCSs). These elevated convective […]

By Debbie Barnhill |
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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.

By admin |
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Near Surface Atmospheric Impacts Resulting from a Developing Metropolitan Area

Over the past century, the population of the world has become increasingly urbanized. As a result, cities have become larger and more densely populated than any time in history. This unprecedented growth and rapid modification of the surface has impacted the overlying boundary-layer of the atmosphere.

By admin |
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