Brill, Dominik ORCID: 0000-0001-8637-4641, May, Simon Matthias ORCID: 0000-0001-6762-7500, Engel, Max ORCID: 0000-0002-2271-4229, Reyes, Michelle, Pint, Anna, Opitz, Stephan, Dierick, Manuel, Gonzalo, Lia Anne, Esser, Sascha and Brueckner, Helmut (2016). Typhoon Haiyan's sedimentary record in coastal environments of the Philippines and its palaeotempestological implications. Nat. Hazards Earth Syst. Sci., 16 (12). S. 2799 - 2823. GOTTINGEN: COPERNICUS GESELLSCHAFT MBH. ISSN 1561-8633

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Abstract

On 8 November 2013, category 5 Supertyphoon Haiyan made landfall on the Philippines. During a post-typhoon survey in February 2014, Haiyan-related sand deposition and morphological changes were documented at four severely affected sites with different exposure to the typhoon track and different geological and geomorphological settings. Onshore sand sheets reaching 100-250m inland are restricted to coastal areas with significant inundation due to amplification of surge levels in embayments or due to accompanying long-wave phenomena at the most exposed coastlines of Leyte and Samar. However, localized washover fans with a storm-typical laminated stratigraphy occurred even along coasts with limited inundation due to waves overtopping or breaching coastal barriers. On a recent reef platform off Negros in the Visayan Sea, storm waves entrained coral rubble from the reef slope and formed an intertidal coral ridge several hundreds of metres long when breaking at the reef edge. As these sediments and landforms were generated by one of the strongest storms ever recorded, they not only provide a recent reference for typhoon signatures that can be used for palaeotempestological and palaeotsunami studies in the region but might also increase the general spectrum of possible cyclone deposits. Although a rather atypical example for storm deposition due to the influence of infragravity waves, it nevertheless provides a valuable reference for an extreme case that should be considered when discriminating between storm and tsunami deposits in general. Even for sites with low topography and high inundation levels dur-ing Supertyphoon Haiyan, the landward extent of the documented sand sheets seems significantly smaller than typical sand sheets of large tsunamis. This criterion may potentially be used to distinguish both types of events.

Item Type: Journal Article
Creators:
CreatorsEmailORCIDORCID Put Code
Brill, DominikUNSPECIFIEDorcid.org/0000-0001-8637-4641UNSPECIFIED
May, Simon MatthiasUNSPECIFIEDorcid.org/0000-0001-6762-7500UNSPECIFIED
Engel, MaxUNSPECIFIEDorcid.org/0000-0002-2271-4229UNSPECIFIED
Reyes, MichelleUNSPECIFIEDUNSPECIFIEDUNSPECIFIED
Pint, AnnaUNSPECIFIEDUNSPECIFIEDUNSPECIFIED
Opitz, StephanUNSPECIFIEDUNSPECIFIEDUNSPECIFIED
Dierick, ManuelUNSPECIFIEDUNSPECIFIEDUNSPECIFIED
Gonzalo, Lia AnneUNSPECIFIEDUNSPECIFIEDUNSPECIFIED
Esser, SaschaUNSPECIFIEDUNSPECIFIEDUNSPECIFIED
Brueckner, HelmutUNSPECIFIEDUNSPECIFIEDUNSPECIFIED
URN: urn:nbn:de:hbz:38-252278
DOI: 10.5194/nhess-16-2799-2016
Journal or Publication Title: Nat. Hazards Earth Syst. Sci.
Volume: 16
Number: 12
Page Range: S. 2799 - 2823
Date: 2016
Publisher: COPERNICUS GESELLSCHAFT MBH
Place of Publication: GOTTINGEN
ISSN: 1561-8633
Language: English
Faculty: Unspecified
Divisions: Unspecified
Subjects: no entry
Uncontrolled Keywords:
KeywordsLanguage
TOHOKU-OKI TSUNAMI; STORM-SURGE; TROPICAL CYCLONES; OVERWASH DEPOSITS; WASHOVER DEPOSITS; FIELD SURVEY; ISLAND; BEACH; STRATIGRAPHY; TRANSPORTMultiple languages
Geosciences, Multidisciplinary; Meteorology & Atmospheric Sciences; Water ResourcesMultiple languages
Refereed: Yes
URI: http://kups.ub.uni-koeln.de/id/eprint/25227

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