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Parameterization of synoptic weather systems in the South Atlantic Bight for modeling applications

机译:南大西洋湾天气天气系统的参数化,用于建模应用

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摘要

An event based, long-term, climatological analysis is presented that allows the creation of coastal ocean atmospheric forcing on the coastal ocean that preserves both frequency of occurrence and event time history. An algorithm is developed that identifies individual storm event (cold fronts, warm fronts, and tropical storms) from meteorological records. The algorithm has been applied to a location along the South Atlantic Bight, off South Carolina, an area prone to cyclogenesis occurrence and passages of atmospheric fronts. Comparison against daily weather maps confirms that the algorithm is efficient in identifying cold fronts and warm fronts, while the identification of tropical storms is less successful. The average state of the storm events and their variability are represented by the temporal evolution of atmospheric pressure, air temperature, wind velocity, and wave directional spectral energy. The use of uncorrected algorithm-detected events provides climatologies that show a little deviation from those derived using corrected events. The effectiveness of this analysis method is further verified by numerically simulating the wave conditions driven by the characteristic wind forcing and comparing the results with the wave climatology that corresponds to each storm type. A high level of consistency found in the comparison indicates that this analysis method can be used for accurately characterizing event-based oceanic processes and long-term storm-induced morphodynamic processes on wind-dominated coasts.
机译:提出了基于事件的长期气候学分析,该分析允许在沿海海洋上创建沿海海洋大气强迫,同时保留发生频率和事件时间历史。开发了一种从气象记录中识别单个风暴事件(冷锋,暖锋和热带风暴)的算法。该算法已应用于南卡罗来纳州南部大西洋沿岸的一个位置,该区域易于发生旋回发生和大气锋面通过。与每日天气图的比较证实,该算法在识别冷锋和暖锋方面是有效的,而对热带风暴的识别则不太成功。风暴事件的平均状态及其变异性由大气压力,气温,风速和波向频谱能量的时间演变表示。使用未经校正的算法检测到的事件所提供的气候与使用经过校正的事件所得出的气候略有不同。通过数值模拟由特征风强迫驱动的波浪条件,并将结果与​​对应于每种风暴类型的波浪气候进行比较,可以进一步验证这种分析方法的有效性。在比较中发现的高度一致性表明,该分析方法可用于准确表征风为主海岸上基于事件的海洋过程和长期风暴诱发的形态动力学过程。

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