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We make use of three different hazard thresholds to determine a hot day fixed thresholds (time-invariant climatological thresholds), seasonally moving thresholds according to alterations in the summer indicates, and totally going thresholds (hot days defined relative to the long run climatology). We find an amazing increase of spatiotemporally contiguous reasonable heatwaves with worldwide heating using fixed thresholds, whereas modifications when it comes to other two danger

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