2005
DOI: 10.1016/j.jhydrol.2005.02.004
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Floods in Catalonia (NE Spain) since the 14th century. Climatological and meteorological aspects from historical documentary sources and old instrumental records

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Cited by 183 publications
(173 citation statements)
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“…Relevant publications include Lall (2005), Pittock (2002), Trenberth (1999), Benestad (2003), Beniston et al (1997), Hanson et al (2004), Svensson et al (2005), Hisdal et al (2001), and Llasat et al (2005). Similarly, there have been numerous publications on land cover change effects on floods, low flows and, more generally water yield, including Robinson et al (2003), Brown et al (2005), Andréassian (2004), Cosandey et al (2005), Bonell and Bruijnzeel (2005), Bonell (1999), Mahé et al (2005b), Archer (2003), Jones (2000), Bronstert et al (2002) and Pfister et al (2004).…”
Section: Introductionmentioning
confidence: 99%
“…Relevant publications include Lall (2005), Pittock (2002), Trenberth (1999), Benestad (2003), Beniston et al (1997), Hanson et al (2004), Svensson et al (2005), Hisdal et al (2001), and Llasat et al (2005). Similarly, there have been numerous publications on land cover change effects on floods, low flows and, more generally water yield, including Robinson et al (2003), Brown et al (2005), Andréassian (2004), Cosandey et al (2005), Bonell and Bruijnzeel (2005), Bonell (1999), Mahé et al (2005b), Archer (2003), Jones (2000), Bronstert et al (2002) and Pfister et al (2004).…”
Section: Introductionmentioning
confidence: 99%
“…Floods are frequently referred to among extreme hydrometeorological phenomena in various historical sources. Up to the present, continuous Spanish flood chronologies covering the last few centuries are only available for some regions, such as Catalonia in the northeast of the country (Barriendos & Martín-Vide, 1998;Llasat et al, 2005), central Spain (Benito et al, 2003), and Andalusia in the south of the country . The main purpose of this work is to present an ensemble of flood chronologies covering most of the river basins in the Iberian Peninsula.…”
Section: Introductionmentioning
confidence: 99%
“…The intensity and the duration of the rainfall, the level and distribution of damage of man-made structures, the number of victims, and the induced geological effects have been considered to distinguish major flash floods from minor flash floods (Table 4; Casas Planes et al, 2003;Llasat et al, 2005;Barnolas and Llasat, 2007). In particular, shoreline progradation has been considered as a key element for major flash floods as it results from significant bed load transport and hyperconcentrated streamflows.…”
Section: Historical Documentation Of Past Floodsmentioning
confidence: 99%