Abstract
The effects of storm-induced sea surface temperature (SST) cooling on hurricane intensity are investigated using a 5-day cloud-resolving simulation of Hurricane Bonnie (1998). Two sensitivity simulations are performed in which the storm-induced cooling is either ignored or shifted close to the modeled storm track. Results show marked sensitivity of the model-simulated storm intensity to the magnitude and relative position with respect to the hurricane track. It is shown that incorporation of the storm-induced cooling, with an average value of 1.3°C, causes a 25-hPa weakening of the hurricane, which is about 20 hPa per 1°C change in SST. Shifting the SST cooling close to the storm track generates the weakest storm, accounting for about 47% reduction in the storm intensity. It is found that the storm intensity changes are well correlated with the air-sea temperature difference. The results have important implications for the use of coupled hurricane-ocean models for numerical prediction of tropical cyclones.
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Zhu, T., Zhang, DL. The impact of the storm-induced SST cooling on hurricane intensity. Adv. Atmos. Sci. 23, 14–22 (2006). https://doi.org/10.1007/s00376-006-0002-9
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DOI: https://doi.org/10.1007/s00376-006-0002-9