1876-2019年维多利亚大雨大洪事件气候学及1976年气候变化的影响

J. Callaghan
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引用次数: 1

摘要

我们对1876年开始有南方涛动(SOI)数据以来维多利亚州的所有大洪水和特大降雨事件进行了广泛的搜索。对天气模式进行了分析,在319个事件中,发现121个事件为东海岸低压,82个为其他类型的低压系统。热带影响也发挥了很大的作用,其中105起事件与热带空气向维多利亚的天气系统流动有关。文中列举了已确定的所有主要天气模式的例子。在144年的研究中,SOI是一个重要的气候驱动因子,其正SOI与许多事件相关。研究了1976年气候变化及其对维多利亚降水事件的影响,发现气候变化后SOI月值主要为负。然而,144年来维多利亚大雨最活跃的时期之一发生在转变之后,2007年至2014年持续出现SOI正事件。因此,预测未来维多利亚大雨的关键是要了解这些正SOI事件的序列是否像转变之前那样持续。还探讨了这种转变与全球气温上升之间可能存在的关系。从一些最强降雨事件中获得的高空数据显示,在850至500hPa水平之间存在反气旋转向风,这已被发现与全球极端降雨有关。
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A Climatology of Heavy Rain and Major Flood Events in Victoria 1876-2019 and the Effect of the 1976 Climate Shift
An extensive search has been carried out to find all major flood and very heavy rainfall events in Victoria since 1876 when Southern Oscillation (SOI) data became available. The synoptic weather patterns were analysed and of the 319 events studied,121 events were found to be East Coast Lows (ECLs) and 82 were other types of low-pressure systems. Tropical influences also played a large role with 105 events being associated with tropical air advecting down to Victoria into weather systems. Examples are presented of all the major synoptic patterns identified. The SOI was found to be an important climate driver with positive SOIs being associated with many events over the 144 years studied. The 1976 Climate Shift and its influence on significant Victorian rainfall events is studied and negative SOI monthly values were shown to dominate following the Shift.However,one of the most active periods in 144 years of Victorian heavy rain occurred after the shift with a sustained period of positive SOI events from 2007 to 2014. Therefore, it is critical for forecasting future Victorian heavy rainfall is to understand if sequences of these positive SOI events continue like those preceding the Shift. Possible relationships between the Shift and Global Temperature rises are also explored. Upper wind data available from some of the heaviest rainfall events showed the presence of anticyclonic turning of the winds between 850hPa and 500hPa levels which has been found to be linked with extreme rainfall around the Globe. 
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