Modeling tides and tsunami propagation in the former Gulf of Tartessos, as a tool for Archaeological Science

被引:12
作者
Abril, Jose-Maria [1 ]
Perianez, Raul [1 ]
Escacena, Jose-Luis [2 ]
机构
[1] Univ Seville, Dept Fis Aplicada 1, ETSIA, Seville 41013, Spain
[2] Univ Seville, Fac Geog & Hist, Dept Prehist & Arqueol, Seville 41004, Spain
关键词
Former Gulf of Tartessos; Tsunami propagation; Tidal dynamics; The city of Tartessos; Recreation of palaeo-marine environments; SEA-LEVEL RISE; GUADIANA ESTUARY; OCEAN TIDES; SW; SIMULATION; EVOLUTION; SPAIN;
D O I
10.1016/j.jas.2013.06.030
中图分类号
Q98 [人类学];
学科分类号
030303 ;
摘要
After the last Holocene sea level rise (about 6900 BP), the Gulf of Tartessos extended over the southwestern area of the nowadays Guadalquivir Valley (Spain). With the development of some depositional littoral landforms and the progressive infill, the system evolved towards an inland lagoon. The first political system in the area emerged and collapsed from the fourth to the second millennium BC. Around the first millennium BC the culture of Tartessos flourished in this area under the Phoenician influence, but it vanished by the sixth century BC. The quest of its lost capital, the city of Tartessos, has been one of the most exciting archaeological enterprises in the past century. The former coastline and the bathymetry of the gulf can be reasonably reconstructed from geo-archaeological studies, and it can be used for the numerical modeling of tide and tsunami propagation in this water body. Models, with a spatial resolution of 30 s of arc, are based on the 2D non-linear hydrodynamic equations and have been previously validated under nowadays conditions. Computed tidal elevations and currents can provide some insight on the ancient trades for ship traffic and fisheries. The simulation of tsunami propagation, like the catastrophic one of 1755, allows estimating their potential hazardous effects on ancient coastal cities. (C) 2013 Elsevier Ltd. All rights reserved.
引用
收藏
页码:4499 / 4508
页数:10
相关论文
共 58 条
[21]   Simulation of the trans-oceanic tsunami propagation due to the 1883 Krakatau volcanic eruption [J].
Choi, B. H. ;
Pelinovsky, E. ;
Kim, K. O. ;
Lee, J. S. .
NATURAL HAZARDS AND EARTH SYSTEM SCIENCES, 2003, 3 (05) :321-332
[22]   Three-dimensional simulation of the 1983 central East (Japan) Sea earthquake tsunami at the Imwon Port (Korea) [J].
Choi, Byung Ho ;
Pelinovsky, Efim ;
Kim, Dong Chul ;
Kim, Kyeong Ok ;
Kim, Kyung Hwan .
OCEAN ENGINEERING, 2008, 35 (14-15) :1543-1557
[23]   Sea-level rise and anthropogenic activities recorded in the late Pleistocene/Holocene sedimentary infill of the Guadiana Estuary (SW Iberia) [J].
Delgado, J. ;
Boski, T. ;
Nieto, J. M. ;
Pereira, L. ;
Moura, D. ;
Gomes, A. ;
Sousa, C. ;
Garcia-Tenorio, R. .
QUATERNARY SCIENCE REVIEWS, 2012, 33 :121-141
[24]  
Escacena J.L., 2012, BELTRAN RODRIGUEZ GU, V2012, P763
[25]  
Esteve Guerrero M., 1969, Tartessos: V Symposium Internacional de Prehistoria Peninsular (Jerez 1968), P111
[26]  
GAVALA JLA, 1959, GEOLOGIA COSTA BAHIA
[27]   Numerical simulation of the 1969 Portuguese tsunami by a finite element method [J].
Guesmia, M ;
Heinrich, P ;
Mariotti, C .
NATURAL HAZARDS, 1998, 17 (01) :31-46
[28]   Realistic test cases for limited area ocean modelling [J].
Herzfeld, M. ;
Schmidt, M. ;
Griffies, S. M. ;
Liang, Z. .
OCEAN MODELLING, 2011, 37 (1-2) :1-34
[29]   Numerical Modelling of the 26th December 2004 Indian Ocean Tsunami for the Southeastern Coast of India [J].
Ioualalen, M. ;
Arreaga-Vargas, P. ;
Pophet, N. ;
Chlieh, M. ;
Ilayaraja, K. ;
Ordonez, J. ;
Renteria, W. ;
Pazmino, N. .
PURE AND APPLIED GEOPHYSICS, 2010, 167 (10) :1205-1214
[30]  
Jimenez-Vialas H., 2009, ALMORAIMA, V38, P11