Storm surges and coastal impacts at Mar del Plata, Argentina
Positive storm surges (PSS) lasting for several days can raise the water level producing significant differences between the observed level and the astronomical tide. These storm events can be more severe if they coincide with a high tide or if they bracket several tidal cycles, particularly in the...
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2009
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| LEADER | 11245caa a22009257a 4500 | ||
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| 001 | PAPER-8624 | ||
| 003 | AR-BaUEN | ||
| 005 | 20250306092105.0 | ||
| 008 | 190411s2009 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-67651001582 | |
| 030 | |a CSHRD | ||
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Fiore, M.M.E. | |
| 245 | 1 | 0 | |a Storm surges and coastal impacts at Mar del Plata, Argentina |
| 260 | |c 2009 | ||
| 270 | 1 | 0 | |m Pousa, J.L.; Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET), Av. Rivadavia 1917, C1033AAJ Buenos Aires, Argentina; email: jlp@fcnym.unlp.edu.ar |
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| 506 | |2 openaire |e Política editorial | ||
| 520 | 3 | |a Positive storm surges (PSS) lasting for several days can raise the water level producing significant differences between the observed level and the astronomical tide. These storm events can be more severe if they coincide with a high tide or if they bracket several tidal cycles, particularly in the case of the highest astronomical tide. Besides, the abnormal sea-level elevation near the coast can cause the highest waves generated to attack the upper beach. This combination of factors can produce severe erosion, threatening sectors located along the coastline. These effects would be more serious if the storm surge height and duration increase as a result of a climatic change. The Mar del Plata (Argentina) coastline and adjacent areas are exposed to such effects. A statistical characterization of PSS based on their intensity, duration and frequency, including a surge event classification, was performed utilizing tide-gauge records over the period 1956-2005. A storm erosion potential index (SEPI) was calculated from observed levels based on hourly water level measurements. The index was related to beach profile responses to storm events. Also, a return period for extreme SEPI values was calculated. Results show an increase in the average number of positive storm surge events per decade. Considering all the events, the last decade (1996-2005) exhibits an average 7% increase compared to each one of the previous decades. A similar behavior was found for the decadal average of the heights of maximum annual positive storm surges. In this case the average height of the last two decades exceeds that of the previous decades by approximately 8 cm. The decadal average of maximum annual duration of these meteorological events shows an increase of 2 h in the last three decades. A possible explanation of the changes in frequency, height and duration of positive storm surges at Mar del Plata would seem to lie in the relative mean sea-level rise. © 2009 Elsevier Ltd. All rights reserved. |l eng | |
| 536 | |a Detalles de la financiación: Comisión de Investigaciones Científicas | ||
| 536 | |a Detalles de la financiación: Centro de Investigación en Computación | ||
| 536 | |a Detalles de la financiación: This research was funded by the Comisión de Investigaciones Científicas de la Provincia de Buenos Aires (CIC), to which the authors are gratefully acknowledged. It is also part of the “Study of the ocean tides on the Argentine coast” Project (Hydrographic Plan 206-PHID, Naval Hydrographic Service, Argentina), and of the I014 Project (Science and Technological Division, University of Buenos Aires (UBACYT) 2008–2010). | ||
| 593 | |a Departamento de Oceanografía, Servicio de Hidrografía Naval, Escuela de Ciencias del Mar, Av. Montes de Oca 2124, C1270ABV Buenos Aires, Argentina | ||
| 593 | |a Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET), Av. Rivadavia 1917, C1033AAJ Buenos Aires, Argentina | ||
| 593 | |a Laboratorio de Oceanografía Costera, Facultad de Ciencias Naturales y Museo, Universidad Nacional de La Plata, Calle 64, No. 3, Casilla Correo 45, 1900 La Plata, Argentina | ||
| 593 | |a Instituto de Geodesia, Facultad de Ingeniería, Universidad de Buenos Aires, Av. Las Heras 2214, C1127AAR Buenos Aires, Argentina | ||
| 593 | |a Departamento de Ciencias de la Atmósfera y los Océanos, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Ciudad Universitaria, Pabellon II, C1428EGA Buenos Aires, Argentina | ||
| 593 | |a Comisión de Investigaciones Científicas de la Provincia de Buenos Aires (CIC), Calle 526 e/10 y 11, 1900 La Plata, Argentina | ||
| 593 | |a Centro de Geología de Costas y del Cuaternario, Facultad de Ciencias Exactas y Naturales, Universidad Nacional de Mar del Plata, Funes 3350, 7600 Mar del Plata, Argentina | ||
| 651 | 4 | |a ARGENTINA | |
| 651 | 4 | |a ARGENTINA | |
| 651 | 4 | |a BUENOS AIRES [ARGENTINA] | |
| 651 | 4 | |a SOUTH AMERICA | |
| 690 | 1 | 0 | |a BEACH PROFILES |
| 690 | 1 | 0 | |a EROSION |
| 690 | 1 | 0 | |a MAR DEL PLATA |
| 690 | 1 | 0 | |a SEA LEVEL |
| 690 | 1 | 0 | |a STORM INDEX |
| 690 | 1 | 0 | |a STORM SURGES |
| 690 | 1 | 0 | |a BEACH PROFILE |
| 690 | 1 | 0 | |a EROSION RATE |
| 690 | 1 | 0 | |a SEA LEVEL CHANGE |
| 690 | 1 | 0 | |a STATISTICAL ANALYSIS |
| 690 | 1 | 0 | |a STORM SURGE |
| 690 | 1 | 0 | |a TIDAL CYCLE |
| 690 | 1 | 0 | |a TIDE GAUGE |
| 690 | 1 | 0 | |a WATER LEVEL |
| 690 | 1 | 0 | |a MAR DEL PLATA |
| 700 | 1 | |a D'Onofrio, Enrique Eduardo | |
| 700 | 1 | |a Pousa, J.L. | |
| 700 | 1 | |a Schnack, E.J. | |
| 700 | 1 | |a Bértola, G.R. | |
| 773 | 0 | |d 2009 |g v. 29 |h pp. 1643-1649 |k n. 14 |p Cont. Shelf Res. |x 02784343 |w (AR-BaUEN)CENRE-4324 |t Continental Shelf Research | |
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