frazil वाक्य
उदाहरण वाक्य
मोबाइल
- Frazil ice formation may also be started by snowfall, rather than supercooling.
- The frazil ice accumulates as more gets deposited.
- The water distribution system can be subject to freezing and clogging from frazil ice.
- The first ice that forms in a polynya are loose ice crystals called frazil ice.
- The accumulation of frazil ice often causes flooding or damage to objects such as trash racks.
- Since frazil ice is found below the surface of water, it is difficult to detect its formation.
- Usually what happens is the frazil ice accumulates on the upstream side of objects and sticks to them.
- Grease ice is the second stage in the formation of solid sea ice after ice floes and then frazil ice.
- In the 1920s, he became a world-class expert on anchor ice, frazil ice, and ice engineering.
- Close spacing keeps out more small floating debris or fish, but may plug up easily with frazil ice in cold climates.
- The growth will extend upstream and increase in width until the point where the frazil ice accumulations bridge together and block the water.
- The ice cover is composed of juxtaposed frazil ice pans and break-away border ice pieces that consolidate in the river flow direction.
- The uppermost layer of the ocean is supercooled to slightly below the freezing point, at which time tiny ice platelets ( frazil ice ) form.
- When the irregular frazil crystals collect, they form something like an icy city filled with streets, elevators and bridges that link countless small pocketlike abodes.
- If the level of turbulence is sufficient, the frazil ice will be mixed down into the upper layer and form a surface layer of grease ice.
- "' Grease ice "'is a very thin, soupy layer of frazil crystals clumped together, which makes the ocean surface resemble an oil slick.
- On the swells far below, long ribbons of grease ice _ a thin, transparent film made from jumbled ice crystals known as frazil _ extended from the pack edge.
- Frazil ice has also been demonstrated to form beneath temperate ( or " warm-based " ) glaciers as water flows quickly downhill and supercools due to a rapid loss of pressure.
- As the crystals grow in number and size, the frazil ice will begin to adhere to objects in the water, especially if the objects themselves are at a temperature below water s freezing point.
- With any kind of turbulence in the water, these fragments break up further into random-shaped small crystals which form a suspension of increasing density in the surface water, an ice type called frazil or grease ice.
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