Abstract
Optimizing the use of surface sensors for wind shear detection involves addressing a broad range of physical processes and time and spatial scales, in addition to the operational considerations of providing timely warnings with systems that are practical to install and maintain Concentrating on thunderstorm gust fronts and down bursts important properties for detection and warning are reviewed from the perspectives of both analytical calculations and experimental measurements Calculations of such properties as the forms of the low level divergence fields and dynamic pressure changes indicate important measurement scales for the use of combined sensing systems of anemometers and pressure sensors
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