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首页> 外文期刊>Meteorology and Atmospheric Physics >A rare East Indian Ocean autumn season tropical cut-off low: impacts and a high-resolution modelling study
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A rare East Indian Ocean autumn season tropical cut-off low: impacts and a high-resolution modelling study

机译:东印度洋罕见的金秋时节热带低气压:影响和高分辨率模拟研究

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摘要

There are two aims of this study. The first is to provide a synoptic description of the lifecycle and impacts of a seasonally rare but intense cut-off low of tropical origin that developed off the northwest coast of Australia, during the Southern Hemisphere autumn months of late April/early May, 2005. The second, and more important, part of this study is an assessment of the capacity of a state-of-the-science numerical model, assimilating all available satellite-derived observational data, to predictthe track, intensity, duration, and severe weather that occurred during the life cycle of the cut-off low. The system was unusual in that its initial development occurred over tropical waters and was associated with a strong and highly involuted subtropical Jetstream, generating a cloud band that produced record 24 h rainfall totals in northwest Western Australia for this time of the year. The cut-off low then underwent further deepening which produced more unseasonable heavy rainfall. Confirmed tornado reports occurred over the populous southwest corner of Western Australia. The synoptic discussion focuses initially on the intensification phase of the system, next on the period of heavy rainfall and gale to storm force winds that were generated by the cutoff during its most intense phase, and finally on the severe thunderstorm outbreak over southwest Western Australia. The study reveals a possible additional reason for the intensification of the tropical low, namely, the presence of positive SST anomalies of up to 3 °C over which the storm track passed early in its life. The modelling study used a high-resolution version (10km horizontal grid spacing) ofa coupled atmosphere-ocean model developed at the University of Oklahoma. The 96 hour forecast covered the period 00 UTC April 28 to 00 UTC May 2, 2005. The initial and boundary conditions were obtained from the archived analyses and forecasts from the Australian Bureau of Meteorology. The numerical forecasts focussed on the salient features of the tropical cut-off low, including the development, track and the rainfall patterns and totals.
机译:这项研究有两个目的。首先是对气候变化的简要描述,以及在2005年4月下旬/ 2005年5月上旬的南半球秋季,澳大利亚西北沿海地区出现的季节性稀有但强烈的热带低产临界值,概述了其生命周期。该研究的第二个也是更重要的部分是评估一个科学数值模型的能力,该模型吸收所有可用的卫星衍生的观测数据,以预测可能发生的轨道,强度,持续时间和恶劣天气发生在生命周期中的低门槛。该系统之所以与众不同,是因为其最初的发展发生在热带水域,并伴有强烈而高度侵入的亚热带急流,产生了一个云带,该云带在一年中的这个时候在澳大利亚西部的西北部产生了创纪录的24小时降雨总量。截止低点随后进一步加深,产生了更多不合季节的强降雨。在西澳大利亚人口稠密的西南角发生了确凿的龙卷风报告。概要的讨论最初集中在系统的集约化阶段,其次集中在暴雨和强风在最强烈的阶段由中断产生的暴风期,最后是西澳大利亚州西南部的雷暴暴发。这项研究揭示了热带低气压加剧的另一个可能原因,即存在高达3°C的SST正异常,风暴路径在其生命早期就通过了。建模研究使用了俄克拉荷马大学开发的大气-海洋耦合模型的高分辨率版本(水平网格间距为10 km)。 96小时的预报涵盖了2005年4月28日世界标准时间到2005年5月2日世界标准时间。初始和边界条件是从澳大利亚气象局的存档分析和预报中获得的。数值预报的重点是热带临界低点的显着特征,包括发育,径迹和降雨模式及总量。

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