The theory of tides is the application of continuum mechanics to interpret and predict the tidal deformations of planetary and satellite bodies and their atmospheres and oceans (especially Earth's oceans) under the gravitational loading of another astronomical body or bodies (especially the Moon and Sun).
The Yolngu people of northeastern Arnhem Land in the Northern Territory of Australia identified a link between the Moon and the tides, which they mythically attributed to the Moon filling with water and emptying out again.
The tides received relatively little attention in the civilizations around the Mediterranean Sea, as the tides there are relatively small, and the areas that experience tides do so unreliably. A number of theories were advanced, however, from comparing the movements to breathing or blood flow to theories involving whirlpools or river cycles. A similar "breathing earth" idea was considered by some Asian thinkers. Plato reportedly believed that the tides were caused by water flowing in and out of undersea caverns. An ancient Indian Purana text dated to 400-300 BC refers to the ocean rising and falling because of heat expansion from the light of the Moon.
Ultimately the link between the Moon (and Sun) and the tides became known to the Greeks, although the exact date of discovery is unclear; references to it are made in sources such as Pytheas of Massilia in 325 BC and Pliny the Elder's Natural History in 77 AD. Although the schedule of the tides and the link to lunar and solar movements was known, the exact mechanism that connected them was unclear. Seneca mentions in De Providentia the periodic motion of the tides controlled by the lunar sphere. Eratosthenes (3rd century BC) and Posidonius (1st century BC) both produced detailed descriptions of the tides and their relationship to the phases of the Moon, Posidonius in particular making lengthy observations of the sea on the Spanish coast, although little of their work survived. The influence of the Moon on tides was mentioned in Ptolemy's Tetrabiblos as evidence of the reality of astrology.
Cette page est générée automatiquement et peut contenir des informations qui ne sont pas correctes, complètes, à jour ou pertinentes par rapport à votre recherche. Il en va de même pour toutes les autres pages de ce site. Veillez à vérifier les informations auprès des sources officielles de l'EPFL.
vignette|Système amphidromique du terme M2 (composante principale lunaire semi-diurne de la marée) en mer du Nord. Les lignes bleu clair illustrent des endroits de même phase de marée (hauteur de surface identique) ; les points amphidromiques sont indiqués par 1, 2 et 3. Un point amphidromique est un point d'un système physique soumis à une force de marée où le marnage est voisin de zéro. Le terme « amphidromique » dérive du grec ancien ἀμφίς (amphís, « des deux côtés », « autour ») et δρόμος (drómos, course), en référence aux marées qui tournent autour de tels points.
La marée est la variation de la hauteur du niveau des mers et des océans, causée par la combinaison des forces gravitationnelles dues à la Lune et au Soleil et des forces d'inertie dues à la révolution de la Terre autour du centre de masse du couple Terre-Lune et de celui du couple Terre-Soleil, le tout conjugué à la rotation de la Terre sur son axe. Lors de la pleine lune et de la nouvelle lune, c'est-à-dire lorsque la Terre, la Lune et le Soleil sont sensiblement dans le même axe (on parle de syzygie), l'influence des corps célestes s'additionne et les marées sont de plus grande amplitude (vives-eaux).
Unsaturated flow influences both the seawater extent under steady-state conditions and the propagation of tides in coastal aquifers. However, its effects on salt distributions in tidally influenced coastal aquifers are little investigated. The present stud ...
Understanding tidal hydrodynamics response to sea level rise (SLR) in estuaries is essential to predict future potential issues such as shoreline erosion, more frequent and intense flooding, coastal wetland threatening, and their economic and ecological as ...
Ancient off-shore lighthouses have a phenomenal cultural significance. They were built as physical aid for navigation to guide mariners and to warn them from dangerous shallow rocky reefs. Understanding their structural response under waves loading is a ch ...