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Possible connection between summer tropical cyclone frequency and spring Arctic Oscillation over East Asia

机译:夏季热带气旋频率与东亚春季北极涛动之间的可能联系

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摘要

This study shows that the frequency of summer tropical cyclones (TCs) in the areas of Japan, Korea, and Taiwan (JKT), which are located in the middle latitudes of East Asia, has a positive correlation with the Arctic Oscillation (AO) occurring during the preceding spring, while summer TC frequency in the Philippines (PH), located in the low latitudes, has a negative correlation with the AO of the preceding spring. During a positive AO phase, when the anomalous anticyclone forms over the mid-latitudes of East Asia, other anomalous cyclones develop not only in the high latitudes but also in the low latitudes from the preceding spring to the summer months. With this change, while southeasterlies in the JKT area derived from the mid-latitude anticyclone plays a role in steering TCs toward this area, northwesterlies strengthened in the PH area by the low-latitude cyclone plays a role in preventing TC movement toward this area. In addition, because of this pressure systems developed during this AO phase, TCs occur, move, and recurve in further northeastern part of the western North Pacific than they do during a negative AO phase.
机译:这项研究表明,位于东亚中纬度的日本,韩国和台湾地区(JKT)的夏季热带气旋(TCs)的频率与北极涛动(AO)的发生呈正相关。在前一个春季,菲律宾(PH)的夏季TC频率位于低纬度,与前一个春季的AO呈负相关。在正AO阶段,当东亚中纬度地区形成反气旋异常时,从前一个春季到夏季,不仅在高纬度地区而且在低纬度地区也出现了其他异常气旋。伴随这一变化,虽然来自中纬度反旋风的JKT地区的东南方在将TC导向该地区方面发挥了作用,但低纬度旋风在PH区加强的西北方在阻止TC向该地区移动方面发挥了作用。此外,由于在此AO阶段形成了这种压力系统,因此与负AO阶段相比,TC在北太平洋西部的东北部发生,移动和弯曲。

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