Articles | Volume 23, issue 7
https://doi.org/10.5194/nhess-23-2449-2023
https://doi.org/10.5194/nhess-23-2449-2023
Research article
 | 
12 Jul 2023
Research article |  | 12 Jul 2023

Assessing Typhoon Soulik-induced morphodynamics over the Mokpo coastal region in South Korea based on a geospatial approach

Sang-Guk Yum, Moon-Soo Song, and Manik Das Adhikari

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Cited articles

Abbas, S., Nichol, J. E., Fischer, G. A., Wong, M. S., and Irteza, S. M.: Impact assessment of a super-typhoon on Hong Kong's secondary vegetation and recommendations for restoration of resilience in the forest succession, Agr. Forest Meteorol., 280, 107784, https://doi.org/10.1016/j.agrformet.2019.107784, 2020. 
Adhikari, M. D., Maiti, S., Bera, A., and Chaudhury, N. R.: Post-tsunami adjustment of coral reef platform and other morphometric changes in Landfall Island, North Andaman – An integrated field and remote sensing-based approach, Regional Studies in Marine Science, 48, 101975, https://doi.org/10.1016/j.rsma.2021.101975, 2021. 
Altman, J., Doležal, J., Černý, T., and Song, J. S.: Forest response to increasing typhoon activity on the Korean peninsula: evidence from oak tree-rings, Glob. Change Biol., 19, 498–504, https://doi.org/10.1111/gcb.12067, 2013. 
Amiri, R., Weng, Q., Alimohammadi, A., and Alavipanah, S. K.: Spatial–temporal dynamics of land surface temperature in relation to fractional vegetation cover and land use/cover in the Tabriz urban area, Iran, Remote Sens. Environ., 113, 2606–2617, https://doi.org/10.1016/j.rse.2009.07.021, 2009. 
Arisanty, D. and Saputra, A. N.: Remote sensing studies of suspended sediment concentration variation in Barito Delta, in: IOP Conference Series: Earth and Environmental Science, 27–28 September 2017, Yogyakarta, Indonesia, 98, 012058, https://doi.org/10.1088/1755-1315/98/1/012058, 2017. 
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This study performed analysis on typhoon-induced coastal morphodynamics for the Mokpo coast. Wetland vegetation was severely impacted by Typhoon Soulik, with 87.35 % of shoreline transects experiencing seaward migration. This result highlights the fact that sediment resuspension controls the land alteration process over the typhoon period. The land accretion process dominated during the pre- to post-typhoon periods.
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