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Weather forecasters use base velocities to detect mesoscale boundaries, which separate contrasting air masses. Mesoscale boundaries are important, because convergence along them has the potential to initiate deep moist convection. Now, a couple of common types of mesoscale boundaries are outflow boundaries and sea and lake breeze fronts. Sea and lake breeze fronts mark the

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so um so at any rate we'll just go right forward if you've ever had the privilege of driving across south of Chicago where 80 and 90 run together you probably remember a traffic jam with toll booths but as you can see up here behind me in this beautiful digital elevation model from Tom

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