Articles | Volume 21, issue 5
Nat. Hazards Earth Syst. Sci., 21, 1531–1550, 2021
https://doi.org/10.5194/nhess-21-1531-2021
Nat. Hazards Earth Syst. Sci., 21, 1531–1550, 2021
https://doi.org/10.5194/nhess-21-1531-2021

Research article 19 May 2021

Research article | 19 May 2021

The role of geomorphology, rainfall and soil moisture in the occurrence of landslides triggered by 2018 Typhoon Mangkhut in the Philippines

Clàudia Abancó et al.

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Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (further review by editor and referees) (03 Jan 2021) by Paolo Tarolli
AR by Clàudia Abancó on behalf of the Authors (10 Feb 2021)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (11 Feb 2021) by Paolo Tarolli
RR by Anonymous Referee #1 (24 Feb 2021)
RR by Anonymous Referee #2 (03 Mar 2021)
ED: Publish subject to minor revisions (review by editor) (06 Mar 2021) by Paolo Tarolli
AR by Clàudia Abancó on behalf of the Authors (15 Mar 2021)  Author's response    Manuscript
ED: Publish as is (22 Mar 2021) by Paolo Tarolli
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Short summary
In 2018 Typhoon Mangkhut triggered thousands of landslides in the Itogon region (Philippines). An inventory of 1101 landslides revealed that landslides mostly occurred in slopes covered by wooded grassland in clayey materials, predominantly facing E-SE. Satellite rainfall and soil moisture data associated with Typhoon Mangkhut and the previous months in 2018 were analyzed. Results showed that landslides occurred during high-intensity rainfall that coincided with the highest soil moisture values.
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