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Coastal Meteorology - Institute of Coastal Research

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<strong>Coastal</strong> Fronts<br />

A longer-lived cousin <strong>of</strong> the<br />

land and sea breeze front<br />

<strong>Coastal</strong> fronts are shallow mesoscale boundaries that separate<br />

moist marine air from cold, dry continental air.<br />

Along the Carolinas, coastal fronts are typically 1000 km long,<br />

with temperature contrasts as large as 20°C, and may persist for<br />

several days.<br />

These fronts can form in response to the temperature gradient<br />

produced by differential heating across the margin <strong>of</strong> the Gulf<br />

Stream. But many triggering mechanisms for differential heating.<br />

... also been observed at the Black Sea, and the coasts <strong>of</strong> Norway,<br />

the Netherlands, and Japan.<br />

These fronts are particularly important because they are <strong>of</strong>ten<br />

associated with cyclogenesis and heavy precipitation.<br />

M.Quante 2002

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