FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2266431013> ?p ?o ?g. }

• W2266431013 endingPage "89" @default.
• W2266431013 startingPage "63" @default.
• W2266431013 abstract "This paper analyses the meteorological conditions and the specific peak flows of 24 catastrophic floods that affected NE Iberian Peninsula in the period 1842–2000. We classify these floods according to the affected area, peak flow magnitude, and damages. Additionally, the NOAA 6 Hourly 20th Century V2 Reanalysis Data Composites have been used to analyze the synoptic conditions during each flood and to evaluate several stability indices, such as the convective available potential energy (CAPE), or the lift index. We found a good correlation between stability indices and the season when the flood occurred. For instance, if maximum CAPE is considered, larger values are found for summer floods, moderate for autumn, and low values during winter floods. We select 5 representative episodes occurred in different seasons and areas to describe in detail the synoptic conditions and to show the temporal evolution of the stability indices. In one the summer floods analyzed in detail, the largest instability, according to all the convective indices, is found. On the contrary, the winter case shows very low values of the convective indices, and autumn cases lay in between. During the other analyzed summer flood instability was low but snow thaw played an important role in producing the flood. Regarding hydrological variables, clear differences between floods occurred at the coast or at the Pyrenees are found. Coastal specific peak flows are larger than Pyrenean ones, especially for small catchment areas. We also combine meteorological (rainfall duration, CAPE), hydrological (specific peak flow) and geomorphological (catchment area) variables to show that for many of the analyzed floods these variables are related: the specific peak flow generally shows larger values when CAPE is also large. However some differences appear depending on the season and area. In those summer floods, where snow thaw played doesn’t played any role, either Pyrenean or coastal, specific peak flow seems to be correlated with CAPE. For autumn floods, depending on the area different correlations were found: Pyrenean floods seem to be a correlation between CAPE and specific peak flows, but not for coastal ones. For winter coastal floods we couldn’t find any correlation between CAPE and specific peak flows." @default.
• W2266431013 created "2016-06-24" @default.
• W2266431013 creator A5006364902 @default.
• W2266431013 creator A5009298724 @default.
• W2266431013 creator A5034799001 @default.
• W2266431013 creator A5063163388 @default.
• W2266431013 creator A5065346497 @default.
• W2266431013 creator A5078124200 @default.
• W2266431013 creator A5081088240 @default.
• W2266431013 creator A5082865402 @default.
• W2266431013 date "2016-10-01" @default.
• W2266431013 modified "2023-10-18" @default.
• W2266431013 title "Meteorological and hydrological analysis of major floods in NE Iberian Peninsula" @default.
• W2266431013 cites W1974176098 @default.
• W2266431013 cites W1975213442 @default.
• W2266431013 cites W1976341027 @default.
• W2266431013 cites W1976351629 @default.
• W2266431013 cites W1979253857 @default.
• W2266431013 cites W1983965066 @default.
• W2266431013 cites W1985282458 @default.
• W2266431013 cites W2000385312 @default.
• W2266431013 cites W2000895246 @default.
• W2266431013 cites W2001602455 @default.
• W2266431013 cites W2005552249 @default.
• W2266431013 cites W2007348708 @default.
• W2266431013 cites W2010530015 @default.
• W2266431013 cites W2011403416 @default.
• W2266431013 cites W2019373637 @default.
• W2266431013 cites W2019675777 @default.
• W2266431013 cites W2020267045 @default.
• W2266431013 cites W2027336705 @default.
• W2266431013 cites W2028275635 @default.
• W2266431013 cites W2032065867 @default.
• W2266431013 cites W2032644449 @default.
• W2266431013 cites W2041814102 @default.
• W2266431013 cites W2042552061 @default.
• W2266431013 cites W2042862265 @default.
• W2266431013 cites W2047780513 @default.
• W2266431013 cites W2052298702 @default.
• W2266431013 cites W2062926622 @default.
• W2266431013 cites W2063823485 @default.
• W2266431013 cites W2064235603 @default.
• W2266431013 cites W2067710282 @default.
• W2266431013 cites W2068252888 @default.
• W2266431013 cites W2070787619 @default.
• W2266431013 cites W2076215905 @default.
• W2266431013 cites W2079258802 @default.
• W2266431013 cites W2080426002 @default.
• W2266431013 cites W2085000704 @default.
• W2266431013 cites W2085957869 @default.
• W2266431013 cites W2088362906 @default.
• W2266431013 cites W2094305586 @default.
• W2266431013 cites W2097360484 @default.
• W2266431013 cites W2099712561 @default.
• W2266431013 cites W2101007820 @default.
• W2266431013 cites W2103162719 @default.
• W2266431013 cites W2103761486 @default.
• W2266431013 cites W2111410742 @default.
• W2266431013 cites W2113265013 @default.
• W2266431013 cites W2116463242 @default.
• W2266431013 cites W2119171342 @default.
• W2266431013 cites W2119633169 @default.
• W2266431013 cites W2121935081 @default.
• W2266431013 cites W2122588877 @default.
• W2266431013 cites W2141393873 @default.
• W2266431013 cites W2157473329 @default.
• W2266431013 cites W2165242200 @default.
• W2266431013 cites W2168266670 @default.
• W2266431013 cites W2168286152 @default.
• W2266431013 cites W2174499327 @default.
• W2266431013 cites W2174870528 @default.
• W2266431013 cites W2178104914 @default.
• W2266431013 cites W2888367769 @default.
• W2266431013 cites W76038776 @default.
• W2266431013 doi "https://doi.org/10.1016/j.jhydrol.2016.02.008" @default.
• W2266431013 hasPublicationYear "2016" @default.
• W2266431013 type Work @default.
• W2266431013 sameAs 2266431013 @default.
• W2266431013 citedByCount "24" @default.
• W2266431013 countsByYear W22664310132016 @default.
• W2266431013 countsByYear W22664310132017 @default.
• W2266431013 countsByYear W22664310132018 @default.
• W2266431013 countsByYear W22664310132019 @default.
• W2266431013 countsByYear W22664310132020 @default.
• W2266431013 countsByYear W22664310132022 @default.
• W2266431013 countsByYear W22664310132023 @default.
• W2266431013 crossrefType "journal-article" @default.
• W2266431013 hasAuthorship W2266431013A5006364902 @default.
• W2266431013 hasAuthorship W2266431013A5009298724 @default.
• W2266431013 hasAuthorship W2266431013A5034799001 @default.
• W2266431013 hasAuthorship W2266431013A5063163388 @default.
• W2266431013 hasAuthorship W2266431013A5065346497 @default.
• W2266431013 hasAuthorship W2266431013A5078124200 @default.
• W2266431013 hasAuthorship W2266431013A5081088240 @default.
• W2266431013 hasAuthorship W2266431013A5082865402 @default.
• W2266431013 hasBestOaLocation W22664310131 @default.
• W2266431013 hasConcept C100970517 @default.
• W2266431013 hasConcept C107054158 @default.

• next