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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Tropical cyclone activity over Bay of Bengal in relation to El Nino-Southern Oscillation
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Tropical cyclone activity over Bay of Bengal in relation to El Nino-Southern Oscillation

机译:在孟加拉湾的热带气旋活动与El Nino-Southern振荡相关

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摘要

The present paper investigates the impact of El Nino-Southern Oscillation (ENSO) on the Bay of Bengal tropical cyclone (TC) activity and associated alterations in environmental conditions during post-monsoon (October-December) season for a period of 44 years (1972-2015). The analysis reveals that the post-monsoon season TCs frequency, accumulated cyclone energy (ACE) and power dissipation index (PDI) values are negatively correlated with the Nino 3.4 sea surface temperature (SST) anomalies (significant at the 95% confidence level). La Nina years are characterized by more frequent and intense cyclonic events compared with El Nino years. The mean ACE and PDI values are approximately two times higher in La Nina than El Nino years. The mean number of TC days per year is also higher in La Nina (7.64 days) than El Nino (3.68 days) years (significant at 95% confidence level). In addition, a significant shift in genesis locations, tracks and landfalling locations of TCs has been observed under different ENSO phases. The mean genesis location of TCs have shifted eastward with tendency of more recurving tracks in La Nina than El Nino years. The presence of strong convective activity, reduced vertical wind shear, high SST (>= 28 degrees C), enhanced mid-tropospheric relative humidity and low-level cyclonic circulation aids the TCs formation and strengthening during La Nina and vice-versa in El Nino conditions.
机译:本文调查了El Nino-Southern振荡(ENSO)对孟加拉热带气旋(TC)活性的影响以及季风(十二月至十月至十月)季节的环境条件相关改动(1972年)(1972年) -2015)。该分析表明,季风季节TCS频率,累积的旋风能量(ACE)和功率耗散指数(PDI)值与NINO 3.4海表面温度(SST)异常(在95%置信水平上显着)负相关。与El Nino岁月相比,La Nina岁的特点是更频繁和强烈的循环事件。平均ACE和PDI值在La Nina大约比El Nino年大约两倍。 La Nina(7.64天)比El Nino(3.68天)的平均TC天数也高(3.68天)(显着的95%的置信水平)。此外,在不同的ENSO阶段观察到Genesis位置,TCS的轨道和降落位置的显着变化。 TCS的平均成因位置向东转移,随着La Nina在La Nina的倾向而不是El Nino岁。存在强烈的对流活性,垂直风剪,高SST(> = 28℃),增强的中部 - 对流层相对湿度和低水平的旋风循环助剂助剂在La Nina期间的TCS形成和强化,反之亦然状况。

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