In meteorology, the process by which weather fronts weaken, disappear, or are dissipated.
From 'front' (meteorological) + Greek 'lysis' (loosening, dissolution). The term parallels 'frontogenesis,' representing the opposite weather process.
Weather fronts are like atmospheric battles between cold and warm air masses, and frontolysis is when the tension breaks down—understanding this process helps meteorologists predict when storms will die out versus intensify.
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