9 documents found, page 1 of 1

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Identifying imprints of externally derived dust and halogens in the sedimentary...

Moreno, J.; Ramos, A. M.; Raposeiro, P. M.; Santos, R. N.; Rodrigues, T.; Naughton, F.; Moreno, F.; Trigo, R. M.; Ibañez-Insa, J.; Ludwig, P.; Shi, X.

Iberian lacustrine sediments are a valuable archive to document environmental changes since the last glacial termination, seen as key for anticipating future climate/environmental changes and their far-reaching implica -tions for generations to come. Herein, multi-proxy-based indicators of a mountain lake record from Serra da Estrela were used to reconstruct atmospheric (in)fluxes and associated climatic/enviro...



Spatial impact and triggering conditions of the exceptional hydro-geomorphologi...

da Silva Pereira, Susana; Ramos, A. M.; Zêzere, José; Trigo, R. M.; Vaquero, J. M.

According to the DISASTER database the 20–28 December 1909 event was the hydro-geomorphologic event with the highest number of flood and landslide cases that occurred in Portugal in the period 1865–2010 (Zêzere et al., 2014). This event also caused important social impacts over the Spanish territory, especially in the Douro Basin, having triggered the highest floods in more than 100 years at the river's mouth i...


DISASTER: a GIS database on hydro-geomorphologic disasters in Portugal

Zêzere, José; Pereira, Susana; Tavares, A. O.; Bateira, C.; Trigo, R. M.; Quaresma, I.; Santos, P. P.; Santos, M.; Verde, J.

In the last century, Portugal was affected by several natural disasters of hydro-geomorphologic origin that often caused high levels of destruction. However, data on past events related to floods and landslides were scattered. The Disaster project aims to bridge the gap on the availability of a consistent and validated hydro-geomorphologic database for Portugal, by creating, disseminating and exploiting a GIS d...


The role of blocking events during the 8.2 ka event over the mid-latitudes of t...

Oliveira, Dulce; Naughton, Filipa; Trigo, R. M.; Abrantes, Fátima; Rodrigues, Teresa; Voelker, Antje H. L.

Date: 2012   |   Origin: Repositório do LNEG

The 20 February 2010 Madeira flash-floods: synoptic analysis and extreme rainfa...

Fragoso, Marcelo; Trigo, R. M.; Pinto, J. G.; Lopes, S.; Lopes, António; Ulbrich, S.; Magro, C.

This study aims to characterise the rainfall exceptionality and the meteorological context of the 20 February 2010 flash-floods in Madeira (Portugal). Daily and hourly precipitation records from the available rain-gauge station networks are evaluated in order to reconstitute the temporal evolution of the rainstorm, as its geographic incidence, contributing to understand the flash-flood dynamics and the type and...


Early Portuguese meteorological measurements (18th century)

Alcoforado, Maria Joao; Vaquero, J. M.; Trigo, R. M.; Taborda, J. P.

Natural proxies, documentary evidence and instrumental data are the only sources used to reconstruct past climates. In this paper, we present the 18th century meteorologists (either Portuguese or foreigners) who made the first observations at several sites in Continental Portugal, Madeira Island and Rio de Janeiro (Brazil), from 1749 until 1802. Information is given concerning observation site, variables observ...


Rainfall-triggered landslides in the Lisbon region over 2006 and relationships ...

Zêzere, José; Trigo, R. M.; Fragoso, Marcelo; Oliveira, Sérgio; Garcia, Ricardo A C

Landslides occurred in the Lisbon area during the last 50 years were almost always induced by rainfall and have been used to establish rainfall thresholds for regional landslide activity. In 2006, three new rainfall-triggered landslide events occurred in the study area, namely on the 20 March, the 25–27 October, and the 28 November. Landslide events occurred in March and October 2006 include shallow translation...


Shallow and deep landslides induced by rainfall in the Lisbon region (Portugal)...

Zêzere, José; Trigo, R. M.; Trigo, I. F.

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 ...


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