Interdecadal variability of the pre-monsoon cyclone characteristics over the Bay of Bengal

Biswajit Jena, S. Pattnaik
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Abstract

The low-pressure systems intensified to cyclones prior to the onset of the Indian summer monsoon season over the North Indian Ocean (NIO) are referred to as pre-monsoon season (PMS) cyclones. Climate change is amplifying the pre-monsoon cyclone landscape, fostering more frequent and intense storms with altered tracks, resulting in heightened risks for coastal communities and economies. This study investigates the interdecadal variations in tropical cyclone (TC) and key large-scale atmospheric parameters that influence the characteristics of cyclones, including track, frequency over the Bay of Bengal (BoB) during the pre-monsoon season from 60 years of data. The large-scale atmospheric parameters are analysed by calculating climatological anomalies. It is noted that the frequency of cyclones making landfall over the eastern Indian coastal landmass has increased in the recent decade compared to the past five decades. Compared to the past fifty years, the percentage frequency has increased in the recent ten years by 50%. At the low level, stronger easterlies are dominant and upper-level jet streams shift to lower latitudes, indicating that the path of cyclones has shifted from the north (N)-northeast (NE) to the northwest (NW), i.e., towards the east Indian coastal landmass, over the recent decade. In contrast to the previous five decades, an unusual low-pressure region has emerged over the NW India and Pakistan regions, creating a favourable path for cyclones moving towards the Indian region in recent decade. Cyclones have been more intense in the recent decade than they were in the previous five decades, according to the rise in low- and mid-level specific humidity (SPH) and temperature over the BoB.
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孟加拉湾季风前气旋特征的年代际变化
在印度夏季季风季节来临之前,北印度洋(NIO)上的低压系统会增强为气旋,被称为季风季节前气旋(PMS)。气候变化正在扩大季风前气旋的范围,使风暴更加频繁和强烈,并改变了路径,从而导致沿海社区和经济面临的风险增加。本研究通过 60 年的数据,调查了热带气旋和影响气旋特征的主要大尺度大气参数的年代际变化,包括孟加拉湾季前季节的路径和频率。大尺度大气参数是通过计算气候学异常来分析的。结果表明,与过去五十年相比,最近十年在印度东部沿海陆地登陆的气旋频率有所增加。与过去五十年相比,最近十年的频率百分比增加了 50%。在低层,较强的东风占主导地位,高层喷流向低纬度移动,这表明气旋的路径在近十年来已从北(N)-东北(NE)转向西北(NW),即转向印度东部沿海陆地。与前五十年不同的是,近十年来,印度西北部和巴基斯坦地区出现了一个不寻常的低压区域,为气旋向印度地区移动创造了有利条件。根据波罗的海上空中低层特定湿度(SPH)和温度的上升,最近十年气旋的强度比前五十年更大。
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