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Bomb cyclones (BCs) are rapidly intensifying extratropical cyclones (ETCs) that pose wintertime hazards. Current low‐resolution climate models underestimate their frequency by ∼30%, causing substantial uncertainties in future projections. Using the high‐resolution Community Earth System Model (HR‐CESM), with 0.25° atmospheric and 0.1° eddy‐permitting ocean resolution, we show that the bias is largely reduced with improved representation of wind structure, upward motion and precipitation. Under the Representative Concentration Pathway 8.5 scenario, BC frequency decreases while wind speed and precipitation intensify. Although the IPCC AR6 reports generally small changes in future ETC wind speed with medium confidence, BCs show a significant intensification. HR‐CESM projects BC precipitation enhancement reaching ∼14.8% K −1 near the cyclone center, a super‐Clausius‐Clapeyron response, whereas HighResMIP and low‐resolution CMIP6 generally show response at or below this scaling. Moisture increases remain close to thermodynamic expectations, while strengthened ascent drives the super‐Clausius‐Clapeyron response in HR‐CESM.
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Zhili et al. (2026) studied this question.
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