The abnormal track of super typhoon Hinnamnor (2022) and its interaction with the upper ocean

The upper ocean response and feedback to super typhoon Hinnamnor (2022) were systematically investigated considering multi-satellite, Array for Real-time Geostrophic Oceanography (Argo) float and reanalysis data. Hinnamnor experienced three main stages: a rapid intensification (RI) stage with a high...

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Veröffentlicht in:Deep-sea research. Part I, Oceanographic research papers Oceanographic research papers, 2023-11, Vol.201, p.104160, Article 104160
Hauptverfasser: Wang, Huipeng, Li, Jiagen, Song, Junqiang, Leng, Hongze, Wang, Huizan, Zhang, Ze, Zhang, Han, Zheng, Minglin, Yang, Xiangrong, Wang, Chunming
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Sprache:eng
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Zusammenfassung:The upper ocean response and feedback to super typhoon Hinnamnor (2022) were systematically investigated considering multi-satellite, Array for Real-time Geostrophic Oceanography (Argo) float and reanalysis data. Hinnamnor experienced three main stages: a rapid intensification (RI) stage with a high moving speed along a westward track, a rapid weakening (RW) stage with a low moving speed along a northward sudden-turning track and a re-intensification (Re-I) stage with a moderate speed along a northward track. At the westward straight-line stage, despite the thin warm water layer (D26 
ISSN:0967-0637
1879-0119
DOI:10.1016/j.dsr.2023.104160