Sedimentary Signatures of Super Typhoon Haiyan: Insight from Core Record in South China Sea

Sedimentary records of event deposits are crucial for regional natural disaster risk assessments and hazard history reconstructions. After Super Typhoon Haiyan passed through the South China Sea in 2013, five gravity cores were collected along the typhoon path in the southern South China Sea basin (...

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Main Authors: Yu-Huang Chen, Chih-Chieh Su, Pai-Sen Yu, Ta-Wei Hsu, Sheng-Ting Hsu, Hsing-Chien Juan, Yuan-Pin Chang, Yu-Fang Ma, Shye-Donq Chiu
Format: Article
Language:English
Published: MDPI AG 2024-12-01
Series:Journal of Marine Science and Engineering
Subjects:
Online Access:https://www.mdpi.com/2077-1312/13/1/10
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author Yu-Huang Chen
Chih-Chieh Su
Pai-Sen Yu
Ta-Wei Hsu
Sheng-Ting Hsu
Hsing-Chien Juan
Yuan-Pin Chang
Yu-Fang Ma
Shye-Donq Chiu
author_facet Yu-Huang Chen
Chih-Chieh Su
Pai-Sen Yu
Ta-Wei Hsu
Sheng-Ting Hsu
Hsing-Chien Juan
Yuan-Pin Chang
Yu-Fang Ma
Shye-Donq Chiu
author_sort Yu-Huang Chen
collection DOAJ
description Sedimentary records of event deposits are crucial for regional natural disaster risk assessments and hazard history reconstructions. After Super Typhoon Haiyan passed through the South China Sea in 2013, five gravity cores were collected along the typhoon path in the southern South China Sea basin (>3800 mbsl). The results showed that Super Typhoon Haiyan deposits with clear graded bedding are preserved at the top of all cores. The thickness of the typhoon layers ranges from 20 to 240 cm and is related to changes in typhoon intensity. The lack of river-connected submarine canyon systems limited the transportation of terrestrial sediments from land to sea. Super Typhoon Haiyan-induced large surface waves played an important role in carrying suspended sediment from the Philippines. The Mn-rich layers at the bottom of the typhoon layers may be related to the soil and rock composition of the Palawan region, which experienced tsunami-like storm surges caused by Super Typhoon Haiyan. These Mn-rich layers may serve as a proxy for sediment export from large-scale extreme terrigenous events. This study provides the first sedimentary record of extreme typhoon events in the deep ocean, which may shed light on reconstructing regional hazard history.
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spelling doaj-art-f4ce8b6b301e4c199dc0edfec8772d282025-01-24T13:36:32ZengMDPI AGJournal of Marine Science and Engineering2077-13122024-12-011311010.3390/jmse13010010Sedimentary Signatures of Super Typhoon Haiyan: Insight from Core Record in South China SeaYu-Huang Chen0Chih-Chieh Su1Pai-Sen Yu2Ta-Wei Hsu3Sheng-Ting Hsu4Hsing-Chien Juan5Yuan-Pin Chang6Yu-Fang Ma7Shye-Donq Chiu8Institute of Oceanography, National Taiwan University, Taipei 10617, TaiwanInstitute of Oceanography, National Taiwan University, Taipei 10617, TaiwanNational Applied Research Laboratories, Taiwan Ocean Research Institute, Kaohsiung 85243, TaiwanInstitute of Oceanography, National Taiwan University, Taipei 10617, TaiwanInstitute of Oceanography, National Taiwan University, Taipei 10617, TaiwanInstitute of Oceanography, National Taiwan University, Taipei 10617, TaiwanDepartment of Oceanography, National Sun Yat-Sen University, Kaohsiung 80424, TaiwanInstitute of Oceanography, National Taiwan University, Taipei 10617, TaiwanInstitute of Oceanography, National Taiwan University, Taipei 10617, TaiwanSedimentary records of event deposits are crucial for regional natural disaster risk assessments and hazard history reconstructions. After Super Typhoon Haiyan passed through the South China Sea in 2013, five gravity cores were collected along the typhoon path in the southern South China Sea basin (>3800 mbsl). The results showed that Super Typhoon Haiyan deposits with clear graded bedding are preserved at the top of all cores. The thickness of the typhoon layers ranges from 20 to 240 cm and is related to changes in typhoon intensity. The lack of river-connected submarine canyon systems limited the transportation of terrestrial sediments from land to sea. Super Typhoon Haiyan-induced large surface waves played an important role in carrying suspended sediment from the Philippines. The Mn-rich layers at the bottom of the typhoon layers may be related to the soil and rock composition of the Palawan region, which experienced tsunami-like storm surges caused by Super Typhoon Haiyan. These Mn-rich layers may serve as a proxy for sediment export from large-scale extreme terrigenous events. This study provides the first sedimentary record of extreme typhoon events in the deep ocean, which may shed light on reconstructing regional hazard history.https://www.mdpi.com/2077-1312/13/1/10Super Typhoon Haiyansedimentary sequenceMn-rich layer
spellingShingle Yu-Huang Chen
Chih-Chieh Su
Pai-Sen Yu
Ta-Wei Hsu
Sheng-Ting Hsu
Hsing-Chien Juan
Yuan-Pin Chang
Yu-Fang Ma
Shye-Donq Chiu
Sedimentary Signatures of Super Typhoon Haiyan: Insight from Core Record in South China Sea
Journal of Marine Science and Engineering
Super Typhoon Haiyan
sedimentary sequence
Mn-rich layer
title Sedimentary Signatures of Super Typhoon Haiyan: Insight from Core Record in South China Sea
title_full Sedimentary Signatures of Super Typhoon Haiyan: Insight from Core Record in South China Sea
title_fullStr Sedimentary Signatures of Super Typhoon Haiyan: Insight from Core Record in South China Sea
title_full_unstemmed Sedimentary Signatures of Super Typhoon Haiyan: Insight from Core Record in South China Sea
title_short Sedimentary Signatures of Super Typhoon Haiyan: Insight from Core Record in South China Sea
title_sort sedimentary signatures of super typhoon haiyan insight from core record in south china sea
topic Super Typhoon Haiyan
sedimentary sequence
Mn-rich layer
url https://www.mdpi.com/2077-1312/13/1/10
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