Continuous gusts typically refer to a phenomenon in meteorology where there are persistent bursts of wind that last for an extended period of time, rather than short, sporadic gusts. Wind gusts are defined as brief increases in wind speed, often caused by turbulence, changes in atmospheric pressure, or other meteorological conditions. When gusts are described as "continuous," it implies that the wind is consistently gusty rather than being characterized by intermittent bursts that occur sporadically.

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