Articles | Volume 23, issue 8
https://doi.org/10.5194/nhess-23-2807-2023
https://doi.org/10.5194/nhess-23-2807-2023
Research article
 | 
16 Aug 2023
Research article |  | 16 Aug 2023

A phytoplankton bloom caused by the super cyclonic storm Amphan in the central Bay of Bengal

Haojie Huang, Linfei Bai, Hao Shen, Xiaoqi Ding, Rui Wang, and Haibin Lü

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Cited articles

Akter, N. and Tsuboki, K.: Role of synoptic-scale forcing in cyclogenesis over the Bay of Bengal, Clim. Dynam., 43, 2651–2662, https://doi.org/10.1007/s00382-014-2077-9, 2014. 
Bai, L., Lü, H., Huang, H., Muhammad Imran, S., Ding, X., and Zhang, Y.: Effects of Anticyclonic Eddies on the Unique Tropical Storm Deliwe (2014) in the Mozambique Channel, J. Mar. Sci. Eng., 11, 129, https://doi.org/10.3390/jmse11010129, 2023. 
Balaguru, K., Chang, P., Saravanan, R., Leung, L. R., Xu, Z., Li, M., and Hsieh, J. S.: Ocean barrier layers' effect on tropical cyclone intensification, P. Natl. Acad. Sci. USA, 109, 14343–14347, https://doi.org/10.1073/pnas.1201364109, 2012. 
Cai, J., Zhang, Y., Li, Y., Liang, X., and Jiang, T.: Analyzing the Characteristics of Soil Moisture Using GLDAS Data: A Case Study in Eastern China, Appl. Sci., 7, 566, https://doi.org/10.3390/app7060566, 2017. 
Cheung, H.-F., Pan, J., Gu, Y., and Wang, Z.: Remote-sensing observation of ocean responses to Typhoon Lupit in the northwest Pacific, Int. J. Remote Sens., 34, 1478–1491, https://doi.org/10.1080/01431161.2012.721940, 2012. 
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Short summary
The super cyclonic storm Amphan occurred in the central Bay of Bengal in May 2020, and a phytoplankton bloom occurred. Its dynamic mechanism was first researched. An inertial oscillation with a 2 d period appeared and lasted for approximately 2 weeks. With the weakened thermocline and thinner barrier layer thickness, nitrate and Chl a were uplifted to the upper ocean by upwelling. With the high photosynthetically available radiation, a phytoplankton bloom occurred.
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