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cotidal - vertaling naar russisch

RISE AND FALL OF SEA LEVELS CAUSED BY THE COMBINED EFFECTS OF THE GRAVITATIONAL FORCES EXERTED BY THE MOON AND THE SUN AND THE ROTATION OF THE EARTH
Tides; Low tide; High tide; Neap tide; Neap Tide; Lunar tide; Tidal flow; Spring Tide; Spring tide; High water; Low water; Land tide; Ebb tide; Ebbing tide; Flooding tide; Tidal cycle; Flow tide; Tide lands; Tidal currents; Tidal movement; Astronomical tide; Ocean tide; Semidiurnal tides; Semidiurnal tide; Tidal current; Shift his tides; Shift tides; Spring high tide; Neap-tide; Lake tide; Lake tides; Tides in the Mediterranean; Tidal constituent; Tidal constituents; Neap Tides; Compound Tide; Compound Tides; Overtide; Overtides; Neaps; Springs (tide); Equilibrium tide theory; Spring tides; High tides; Ebbing; Flood tide; Low Tides; High tide line; Tides (ocean); Springtide; High astronomical tide; Cotidal map; Tidal phase; Principal lunar semi-diurnal constituent; Ocean tides; Equilibrium tide; M2 tide; M2 lunar tide; M2 tidal constituent; Full tide; Tidal biology; High-tide; Tidal stream (marine science)
  • Bar Harbor]], [[Maine]], U.S. (2014)
  • Low tide at Bangchuidao scenic area, [[Dalian]], [[Liaoning Province]], [[China]]
  • Brouscon's Almanach]] of 1546: Compass bearings of high waters in the [[Bay of Biscay]] (left) and the coast from [[Brittany]] to [[Dover]] (right).
  • Brouscon's Almanach of 1546: Tidal diagrams "according to the age of the moon".
  • mi}}.
  • alt=Diagram showing a circle with closely spaced arrows pointing away from the reader on the left and right sides, while pointing towards the user on the top and bottom.
  • date=30 December 2016}}</ref>
  • The harbour of [[Gorey, Jersey]] falls dry at low tide.
  • alt=Photo of partially submerged rock showing horizontal bands of different color and texture, where each band represents a different fraction of time spent submerged.
  • alt=Map showing relative tidal magnitudes of different ocean areas
  • Ocean Beach]] in [[San Francisco]], [[California]], U.S.
  • 4}} feet above mean low water and is still falling, as indicated by pointing of the arrow. Indicator is powered by system of pulleys, cables and a float. (Report Of The Superintendent Of The Coast & Geodetic Survey Showing The Progress Of The Work During The Fiscal Year Ending With June 1897 (p. 483))
  • Earth's rotation drags the position of the tidal bulge ahead of the position directly under the Moon showing the lag angle.
  • alt=Graph showing one line each for M&nbsp;<sub>2</sub>, S&nbsp;<sub>2</sub>, N&nbsp;<sub>2</sub>, K&nbsp;<sub>1</sub>, O&nbsp;<sub>1</sub>, P&nbsp;<sub>1</sub>, and one for their summation, with the X axis spanning slightly more than a single day
  • alt=Graph with a single line showing tidal peaks and valleys gradually cycling between higher highs and lower highs over a 14-day period
  • alt=Graph showing with a single line showing only a minimal annual tidal fluctuation
  • alt=Graph with a single line rising and falling between 4 peaks around 3 and four valleys around −3
  • alt=Graph showing 6 lines with two lines for each of three cities. Nelson has two monthly spring tides, while Napier and Wellington each have one.
  • 2}} hours before high tide
  • In [[Maine]] (U.S.), low tide occurs roughly at moonrise and high tide with a high Moon, corresponding to the simple gravity model of two tidal bulges; at most places however, the Moon and tides have a [[phase shift]].
  • alt=Chart illustrating that tidal heights enter in calculations of legally significant data such as ''boundary lines'' between the high seas and territorial waters. Chart shows an exemplar coastline, identifying bottom features such as longshore bar and berms, tidal heights such as mean higher high water, and distances from shore such as the 12 mile limit.
  • The types of tides
  • Illustration by the course of half a month
  • alt=Three graphs. The first shows the twice-daily rising and falling tide pattern with nearly regular high and low elevations. The second shows the much more variable high and low tides that form a "mixed tide". The third shows the day-long period of a diurnal tide.
  • A regular water level chart

cotidal      

общая лексика

равноприливный

cotidal      
1) равноприливный
2) котидальный
3) котидальный
high water         

[hai'wɔ:tə]

общая лексика

высокая [полная] вода

паводок

полая вода

география

вода полная

метеорология

водополье

синоним

high tide

существительное

общая лексика

паводок

синоним

high tide

Definitie

Cotidal
·adj Marking an equality in the tides; having high tide at the same time.

Wikipedia

Tide

Tides are the rise and fall of sea levels caused by the combined effects of the gravitational forces exerted by the Moon (and to a much lesser extent, the Sun) and are also caused by the Earth and Moon orbiting one another.

Tide tables can be used for any given locale to find the predicted times and amplitude (or "tidal range"). The predictions are influenced by many factors including the alignment of the Sun and Moon, the phase and amplitude of the tide (pattern of tides in the deep ocean), the amphidromic systems of the oceans, and the shape of the coastline and near-shore bathymetry (see Timing). They are however only predictions, the actual time and height of the tide is affected by wind and atmospheric pressure. Many shorelines experience semi-diurnal tides—two nearly equal high and low tides each day. Other locations have a diurnal tide—one high and low tide each day. A "mixed tide"—two uneven magnitude tides a day—is a third regular category.

Tides vary on timescales ranging from hours to years due to a number of factors, which determine the lunitidal interval. To make accurate records, tide gauges at fixed stations measure water level over time. Gauges ignore variations caused by waves with periods shorter than minutes. These data are compared to the reference (or datum) level usually called mean sea level.

While tides are usually the largest source of short-term sea-level fluctuations, sea levels are also subject to change from thermal expansion, wind, and barometric pressure changes, resulting in storm surges, especially in shallow seas and near coasts.

Tidal phenomena are not limited to the oceans, but can occur in other systems whenever a gravitational field that varies in time and space is present. For example, the shape of the solid part of the Earth is affected slightly by Earth tide, though this is not as easily seen as the water tidal movements.

Vertaling van &#39cotidal&#39 naar Russisch