amphidromic system

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• Amphidromic point — An amphidromic point is a point within a tidal system where the tidal range is almost zero. [ 2 tidal constituent the amplitude indicated by color. The white lines are cotidal differing by 1 hr. [ Picture credit: R. Ray,… …   Wikipedia

• amphidromic — | ̷ ̷ ̷ ̷|drämik adjective Etymology: Greek amphidromos running both ways (from amphi + dromos course, racecourse) + English ic more at dromedary : relating to a system of tidal action in which the tide wave progresses around a point or center of …   Useful english dictionary

• North Sea — For other uses, see North Sea (disambiguation). North Sea Location Atlantic Ocean Coordinates …   Wikipedia

• Tide — This article is about tides in the Earth s oceans. For other uses, see Tide (disambiguation). Tidal redirects here. For other uses, see Tidal (disambiguation). High Tide redirects here. For other uses, see High Tide (disambiguation) …   Wikipedia

• Coriolis effect — For the psychophysical perception effect, see Coriolis effect (perception). Classical mechanics Newton s Second Law …   Wikipedia

• Ocean thermal energy conversion — Temperature differences between the surface and 1000m depth in the oceans Ocean Thermal Energy Conversion (OTEC) uses the difference between cooler deep and warmer shallow or surface ocean waters to run a heat engine and produce useful work,… …   Wikipedia

• Tsunami — For other uses, see Tsunami (disambiguation) …   Wikipedia

• Global climate model — AGCM redirects here. For Italian competition regulator, see Autorità Garante della Concorrenza e del Mercato. Climate models are systems of differential equations based on the basic laws of physics, fluid motion, and chemistry. To “run” a model,… …   Wikipedia

• Ocean observations — The following are considered essential ocean climate variables by the OOPC[1][clarification needed] that are currently feasible with current observational systems. Contents 1 Ocean climate variables 1 …   Wikipedia

• Tidal acceleration — is an effect of the tidal forces between an orbiting natural satellite ( i.e. a moon), and the planet (called the primary) that it orbits. It causes a gradual recession of a satellite in a prograde orbit away from the primary, and a corresponding …   Wikipedia

• Deep-ocean Assessment and Reporting of Tsunamis — A diagram of the Dart II System A tsunami b …   Wikipedia