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词汇 example_english_gyre
释义

Examples of gyre


These examples are from corpora and from sources on the web. Any opinions in the examples do not represent the opinion of the Cambridge Dictionary editors or of Cambridge University Press or its licensors.
Upwelling occurs in the northern gyre and downwelling in the southern gyre.
Subtropical gyres occupy a large fraction of the world's ocean and are more productive than originally thought.
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On the relationships between primary, net community, and export production in subtropical gyres.
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As with other patches in each of the five oceanic gyres, the plastics in it break down to ever smaller particles, and to constituent polymers.
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Wind-driven surface currents interact with these gyres and the underwater topography, such as seamounts and the edge of continental shelves, to produce downwellings and upwellings.
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However, along the equatorial edge of the gyres, one finds a stagnant pool of water which has no direct connection to the ocean surface.
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As a result, large-scale horizontal flows of air or water tend to form clockwise-turning gyres.
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Using two downwelling inlets on both sides of the tank lets gravity create two gyres in the tank.
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Plastic debris tends to accumulate at the centre of ocean gyres.
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Picoplankton are responsible for the most primary productivity in oligotrophic gyres, and are distinguished from nanoplankton and microplankton.
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Information on gyres, currents, tides, and trade winds were all recorded and studied in order to determine if the information could benefit sailors.
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Like other subtropical gyres, it has a high-pressure zone in its center.
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Cyanobacteria remain critical to marine ecosystems as primary producers in oceanic gyres, as agents of biological nitrogen fixation, and, in modified form, as the plastids of marine algae.
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Pelagic plastic pieces in the center of our oceans gyres outnumber live marine plankton, and are passed up the food chain to reach all marine life.
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Flotsam can be blown by the wind, or follow the flow of ocean currents, often ending up in the middle of oceanic gyres where currents are weakest.
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Floating oceanic debris tends to accumulate at the centre of gyres and on coastlines, frequently washing aground, when it is known as "beach litter" or tidewrack.
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Wind-driven surface currents interact with these gyres and the underwater topography, such as seamounts, fishing banks, and the edge of continental shelves, to produce downwellings and upwellings.
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A secondary effect due t o the upwelling and independent of the magnitude of the eddy viscosity is the production of an extra gyre near the east coast.
Sea ice has been noted to persist in the central area of the gyre.
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Within a broad cyclonic gyre, the system moved erratically, first drifting south then east-northeast and eventually northwest.
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Despite the upgrade, the storm was not well organized, with several smaller swirls rotating around a common cyclonic gyre.
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Operculum is type c, with a gyre that bears a raised spiral row of strong, distally-tapering spines (hence the specific epithet, echinogyra).
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Their primary goal was to describe the abundance and distribution of plastic in the gyre in the most rigorous study to date.
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At the depths of the gyre lies a sea floor of fine-grained clay sediments.
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Essentially, waters that are part of the wind-driven subtropical gyre circulations are rapidly exchanged with the surface and never acquire a strong oxygen deficit.
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While waters of differing salinity and temperatures could become stratified, models predict that the seaway was well-mixed due to the circulation gyre.
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A gyre tank encourages a maximum amount of water momentum through a divider in the center of the aquarium.
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Interannual trends have established that carbon dioxide concentrations within this gyre are increasing at a similar rate to that occurring in the atmosphere.
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The gyre contains approximately six pounds of plastic for every pound of plankton.
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Stretch kreisels are a double gyre kreisel design, where the tank length is at least twice the height.
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Thereafter, deep convection gradually developed around a large cyclonic gyre which accompanied the wave.
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Wave power is distinct from the diurnal flux of tidal power and the steady gyre of ocean currents.
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The eddy effects of the gyre serve to retain pollutants in its center.
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The gyre contains both ice and water.
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Another recent method is the gyre tank.
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When water moves in this way, other water flows in to fill the gap and a circular movement of surface currents known as a gyre is formed.
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During its positive phase, the gyre warms.
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If a pollutant gets trapped in a current that is headed toward a gyre, it will stay there indefinitely or as long as the life of the pollutant.
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His dialogical theory of the gyres, in which opposites alternately increase and decrease in strength but contain and never obliterate each other, reveals his rejection of a unitary position.
Leaves are persistent and attached in an upwards parastichy of about 30@, there being 9 or 10 leaves per gyre.
As the sun heats it, the water in the gyre evaporates- but then blows away.
During the first stage the development of a secondary dipole circulation (the so-called -gyre) in the vicinity of the vortex plays a major role.
A consequence of the downwelling is that the principal interior gyre is prevented from reaching the east coast and a secondary gyre is formed in this region.
Oceanic debris tends to accumulate at the centre of gyres and coastlines, frequently washing aground where it is known as beach litter.
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Flow over the shelf below the surface layer consists of two anticyclonic gyres connected by a central cyclonic flow.
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Besides gyres, there are temporary surface currents that occur under specific conditions.
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Within this feature, two smaller cyclonic gyres operate, occupying the eastern and western sectors of the basin.
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The deep benthic habitats of the ocean gyres have been thought to typically consist of some of the most food-poor regions on the planet.
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As a direct result of this circular pattern, gyres act like giant whirlpools and become traps for anthropogenic pollutants, such as marine debris.
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The geostrophic gyres are largely independent of one another in each hemisphere, because of the patterns of driving winds and the present positions of continents.
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Because of the different factors that drive and shape them, the currents that form geostrophic gyres have different characteristics.
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Western intensification also occurs in the polar gyres, where the sign of the wind stress curl and the direction of the resulting currents are reversed.
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These examples are from corpora and from sources on the web. Any opinions in the examples do not represent the opinion of the Cambridge Dictionary editors or of Cambridge University Press or its licensors.
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