Water Exchange on a Geological Timescale - Examples from Two Coastal Sites in the Baltic Sea
Datos Bibliográficos
| ID | 10888573 |
|---|---|
| Autores | Christin Eriksson (WSP Sverige (Sweden), autor de correspondencia), Anders Engqvist (Vattenfall (Sweden)) |
| Año | 2013 |
| Volumen | 42 |
| Número | 4 |
| Páginas | 447-454 |
| Fecha de publicación | 2013-05-01 |
| Open Access | Sí |
| Tipo | ARTICLE |
| Revista | AMBIO (JOURNAL) |
| Identificadores de la revista | ISSN: 0044-7447 • E-ISSN: 1654-7209 |
| Editorial | Springer Science and Business Media LLC (PUBLISHER) |
| DOI | 10.1007/s13280-013-0396-4 |
| PMID | 23619802 |
| PMCID | PMC3636375 |
| OpenAlex | W2053569757 |
| Idioma | EN |
| Citas recibidas | 4 |
| Referencias citadas | 18 |
The water turnover of two coastal areas, Forsmark and Laxemar-Simpevarp, has been modeled for 13 selected years between 6500 BC and 9000 AD by utilizing information about past, present, and future bathymetry. The Forsmark area can be described as an open-ended funnel, and is analyzed with a 3D-model (MIKE 3-FM); the Laxemar area is partitioned into clusters of sub-basins treated with a discrete coupled basin model (CouBa). In all simulations, the main variation factor is the land uplift. The 3D-model domain is successively modified. For the CouBa approach the successive basin configurations are objectively deduced based on the 3D domain modifications. The average age (AvA) of the resident water relative to the open coast is generally lower for the Forsmark area. A typical progression is that the AvA values increase until a sub-basin ceases to be connected to the coastal zone. This disconnection is often preceded by a lowered AvA
Bathymetry · Cartography · Geography · Geomorphology · Geotechnical engineering · Hydrology (agriculture · Open water · Sink (geography · Structural basin · Geological formations and processes · Geology · Geology and Paleoclimatology Research · Oceanography · Scientific Research and Discoveries
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| Citas por año | 0,31 |
|---|---|
| Intervalo de citas | 2013 - 2013 (1) |
| Altamente citado | No |