Anjana U, Kumar Karanam Kishore
Space Physics Laboratory, VSSC/ISRO, Trivandrum, India.
Kerala University, Trivandrum, India.
Sci Rep. 2023 Sep 11;13(1):15009. doi: 10.1038/s41598-023-42323-7.
Recent investigations have shown a robust signature of poleward migration of the tropical cyclone latitudes using observations and climate model simulations. Most of these studies invoked the role of the Hadley circulation (HC) expansion in the poleward shifting of tropical cyclones. However, none of these studies focused on the dissection of the zonally asymmetric HC into ascending and descending regions at regional scales, which holds the key in establishing the association between these two phenomena. Here, we are reporting the poleward migration of tropical cyclones and their association with ascending region boundaries of the HC at regional scales for the first time. The results emphatically show that the tropical cyclone latitudes as well as latitudes of maximum lifetime intensity vary in tandem with boundaries of the ascending region of the HC as compared to its descending region thus providing a vital clue on processes governing poleward migration of tropical cyclones.
最近的调查显示,利用观测和气候模型模拟,热带气旋纬度存在明显的向极迁移特征。这些研究大多认为哈德利环流(HC)扩张在热带气旋向极移动中发挥了作用。然而,这些研究都没有聚焦于在区域尺度上把纬向非对称的哈德利环流分解为上升和下降区域,而这是建立这两种现象之间联系的关键。在此,我们首次报告了热带气旋在区域尺度上的向极迁移及其与哈德利环流上升区域边界的关联。结果有力地表明,与哈德利环流下降区域相比,热带气旋纬度以及最大生命期强度纬度与哈德利环流上升区域边界同步变化,从而为控制热带气旋向极迁移的过程提供了重要线索。