Abstract

A meso-g-scale observational analysis of the fine surface structure of the sea-breeze fronts (SBF) over the coast of southern Israel is presented. Objective criteria for the SBF passage are derived based on wind speed and direction, temperature, and humidity. A realization of an automized detection system for SBF is described. Preliminary results indicate that, in addition to the primary SBF, there are significant and consistent pre- and post-SBF lines. The surface structures of these lines are shown, and related to earlier theoretical studies of the SBF forerunners and Kelvin‐Helmholz waves. Although the pre- and post-SBF lines seem to be important for pollutant transport, human comfort, and better theoretical understanding of the SBF, they have previously attracted little attention in the SBF literature.

Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call