Between the evening of October 23^rd and the evening of October 24^th 2017, a sea storm hit the city of Bari, along the Adriatic coast, in the south of Italy, causing widespread damages. Due to the absence of direct observations of wave characteristics, the present paper is aimed to (i) compare the development of the occurred sea storm as hindcasted by ’84 method with the predictions by atmosphere-ocean numerical models and satellite observations and (ii) estimate the most reliable value of the significant wave height, H_s, at the peak of the sea storm, with its associated return period. As a result, the ’84 showed the better agreement with the satellite observations in determining the value of H_s at the peak of the sea storm, compared with the predictions by more sophisticated atmosphere-ocean numerical models. In particular, the obtained value of H_s, equal to 6.58 m, makes the investigated sea storm an exceptional event.

10月23日晚与^RD和10月24日晚上^日2017年，海上风暴袭击的城市巴里，亚得里亚海沿岸，在意大利南部，造成大面积破坏。由于缺乏对波特征的直接观测，因此本文旨在（i）将'84方法造成的海暴发生的发展与大气海洋数值模型和卫星观测的预测进行比较，以及（ii）估计海浪峰值时重要波高H _s的最可靠值及其相关的返回期。结果，'84卫星在确定H _s值时显示出与卫星观测结果更好的一致性_。与更复杂的海洋-海洋数值模型的预测相比，在海啸的高峰期。特别是，获得的H _s值等于6.58 m，使得被调查的海暴成为例外事件。