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Mesometeorology was defined by Ligda in 1951 to include phe­ nomena which are too large to be observed by in situ sensors at a single station but too small to be defined adequately by conven­ tional station networks. The scientific, economic, and social im­ portance of weather events on the scales of 10-1000 km is not a new discovery, but only recently have the weather services, research laboratories, and academic scientists of the world begun...

Mesometeorology was defined by Ligda in 1951 to include phe­ nomena which are too large to be observed by in situ sensors at a single station but too small to be defined adequately by conven­ tional station networks. The scientific, economic, and social im­ portance of weather events on the scales of 10-1000 km is not a new discovery, but only recently have the weather services, research laboratories, and academic scientists of the world begun...