Shallow and deep landslides induced by rainfall in the Lisbon region (Portugal): assessment of relationships with the North Atlantic Oscillation

The aim of this study is to assess the impact of the North Atlantic Oscillation (NAO) on both the winter precipitation and the temporal occurrence of different landslide types in Portugal. The analysis is applied to five sample areas located just north of Lisbon, the capital of Portugal. These sites...

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Published in:Natural Hazards and Earth System Sciences
Main Authors: Zêzere, J. L., Trigo, R. M., Trigo, I. F.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/nhess-5-331-2005
https://nhess.copernicus.org/articles/5/331/2005/
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spelling ftcopernicus:oai:publications.copernicus.org:nhess37192 2023-05-15T17:29:41+02:00 Shallow and deep landslides induced by rainfall in the Lisbon region (Portugal): assessment of relationships with the North Atlantic Oscillation Zêzere, J. L. Trigo, R. M. Trigo, I. F. 2018-09-27 application/pdf https://doi.org/10.5194/nhess-5-331-2005 https://nhess.copernicus.org/articles/5/331/2005/ eng eng doi:10.5194/nhess-5-331-2005 https://nhess.copernicus.org/articles/5/331/2005/ eISSN: 1684-9981 Text 2018 ftcopernicus https://doi.org/10.5194/nhess-5-331-2005 2020-07-20T16:27:28Z The aim of this study is to assess the impact of the North Atlantic Oscillation (NAO) on both the winter precipitation and the temporal occurrence of different landslide types in Portugal. The analysis is applied to five sample areas located just north of Lisbon, the capital of Portugal. These sites are particularly relevant because actual dates of most of the recent landslide events are known but also because the landslides occurred in a suburban area with growing urbanization pressure. Results show that the large inter-annual variability of winter precipitation observed in western Iberia, i.e. Portugal and parts of Spain, is largely modulated by the NAO mode. In particular, precipitation falling in Portugal between November and March presents a correlation coefficient of R =–0.66 with the NAO index. Precipitation distribution for the reference rain gauge in the study area reveals that the probability of a wet month to occur is much higher for low NAO index composites than for the corresponding high NAO index composite. It is shown that this control, exerted by NAO on the precipitation regime, is related to corresponding changes in the associated activity of North-Atlantic storm tracks that affect the western Iberia. Landslide activity in the study area is related to both intense, short duration precipitation events (1–15 days) and long-lasting rainfall episodes (1–3 months). The former events trigger shallow translational slides while the later episodes are usually associated with deeper and larger slope movements. This second group of landslides is shown to be statistically associated with the 3-month average of the NAO index. Text North Atlantic North Atlantic oscillation Copernicus Publications: E-Journals Natural Hazards and Earth System Sciences 5 3 331 344
institution Open Polar
collection Copernicus Publications: E-Journals
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language English
description The aim of this study is to assess the impact of the North Atlantic Oscillation (NAO) on both the winter precipitation and the temporal occurrence of different landslide types in Portugal. The analysis is applied to five sample areas located just north of Lisbon, the capital of Portugal. These sites are particularly relevant because actual dates of most of the recent landslide events are known but also because the landslides occurred in a suburban area with growing urbanization pressure. Results show that the large inter-annual variability of winter precipitation observed in western Iberia, i.e. Portugal and parts of Spain, is largely modulated by the NAO mode. In particular, precipitation falling in Portugal between November and March presents a correlation coefficient of R =–0.66 with the NAO index. Precipitation distribution for the reference rain gauge in the study area reveals that the probability of a wet month to occur is much higher for low NAO index composites than for the corresponding high NAO index composite. It is shown that this control, exerted by NAO on the precipitation regime, is related to corresponding changes in the associated activity of North-Atlantic storm tracks that affect the western Iberia. Landslide activity in the study area is related to both intense, short duration precipitation events (1–15 days) and long-lasting rainfall episodes (1–3 months). The former events trigger shallow translational slides while the later episodes are usually associated with deeper and larger slope movements. This second group of landslides is shown to be statistically associated with the 3-month average of the NAO index.
format Text
author Zêzere, J. L.
Trigo, R. M.
Trigo, I. F.
spellingShingle Zêzere, J. L.
Trigo, R. M.
Trigo, I. F.
Shallow and deep landslides induced by rainfall in the Lisbon region (Portugal): assessment of relationships with the North Atlantic Oscillation
author_facet Zêzere, J. L.
Trigo, R. M.
Trigo, I. F.
author_sort Zêzere, J. L.
title Shallow and deep landslides induced by rainfall in the Lisbon region (Portugal): assessment of relationships with the North Atlantic Oscillation
title_short Shallow and deep landslides induced by rainfall in the Lisbon region (Portugal): assessment of relationships with the North Atlantic Oscillation
title_full Shallow and deep landslides induced by rainfall in the Lisbon region (Portugal): assessment of relationships with the North Atlantic Oscillation
title_fullStr Shallow and deep landslides induced by rainfall in the Lisbon region (Portugal): assessment of relationships with the North Atlantic Oscillation
title_full_unstemmed Shallow and deep landslides induced by rainfall in the Lisbon region (Portugal): assessment of relationships with the North Atlantic Oscillation
title_sort shallow and deep landslides induced by rainfall in the lisbon region (portugal): assessment of relationships with the north atlantic oscillation
publishDate 2018
url https://doi.org/10.5194/nhess-5-331-2005
https://nhess.copernicus.org/articles/5/331/2005/
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source eISSN: 1684-9981
op_relation doi:10.5194/nhess-5-331-2005
https://nhess.copernicus.org/articles/5/331/2005/
op_doi https://doi.org/10.5194/nhess-5-331-2005
container_title Natural Hazards and Earth System Sciences
container_volume 5
container_issue 3
container_start_page 331
op_container_end_page 344
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