definition of land breeze
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Land breeze Land breeze, a local wind system characterized by a flow from land to water late at night. Land breezes alternate with sea breezes along coastlines adjacent to large bodies of water. Both are induced by differences that occur between the heating or cooling of the water surface and the adjacent land surface. The land breeze is typically shallower than the sea breeze since the cooling of the atmosphere over land is confined to a shallower layer at night than the heating of the air during the day. Since the surface flow of the land breeze terminates over water, a region of low-level air convergence is produced.
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- Sundowners-When the land is heated hotter than the ocean, the wind blows from cold to hot, onshore. When the land cools and becomes cooler than the water, the wind blows from cooler to warmer surface temperatures, offshore. Put a fire on the land and that can change the usual timing of the event.
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Is the Best Time to Fish Low or High Tide? When planning a saltwater fishing trip, familiarize yourself with the tides in your area to choose the best time to go fishing. The movement of ocean water is controlled vertically by tides and horizontally by currents. Each day has two high tides and two low tides, and neither of them are good times to fish.
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Local Winds Sea breezes can move 70km inland in temperate climates by 9pm in the evening. Sea breezes can be noticed several kilometres out to sea. In the tropics they can be felt 20km from the land. Wind speeds from sea breezes can be about 4-8m/s but can be even stronger.
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Sea and Land Breezes Over the water, high surface pressure will form because of the colder air. To compensate, the air will sink over the ocean. The wind will blow from the higher pressure over the water to lower pressure over the land causing the sea breeze. The sea breeze strength will vary depending on the temperature difference between the land and the ocean. At night, the roles reverse. The air over the ocean is now warmer than the air over the land.
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Wind Wind is the flow of gases on a large scale. On the surface of the Earth, wind consists of the bulk movement of air. In outer space, solar wind is the movement of gases or charged particles from the Sun through space, while planetary wind is the outgassing of light chemical elements from a planet's atmosphere into space. Winds are commonly classified by their spatial scale, their speed, the types of forces that cause them, the regions in which they occur, and their effect. The strongest observed winds on a planet in the Solar System occur on Neptune and Saturn.
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In defense of Confederate flag, frequent Fox News guest claims Civil War wasn't about slavery A common explanation is that the Civil War was fought over the moral issue of slavery. In fact, it was the economics of slavery and political control of that system that was central to the conflict.. No. 3 on the Google hit parade was Americanhistoryabout.com.
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Sea and Land Breezes The sea breeze strength will vary depending on the temperature difference between the land and the ocean. At night, the roles reverse. The air over the ocean is now warmer than the air over the land. The land loses heat quickly after the sun goes down and the air above it cools too.
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Sea and Land Breezes At certain locations, converging sea breezes can cause thunderstorms during the afternoon. On the peninsula of Florida, winds are blowing easterly (from the east) off the Atlantic Ocean and westerly (from the west) off the Gulf of Mexico. This causes sea breezes to converge towards the central part of the peninsula.
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Sea Breezes on the NSW Coast On the other hand a well established sea breeze may contribute to cloud formation, of two kinds in particular: 1  large cumulus and cumulonimbus (thunderstorm clouds) which require an inflow of moist air in the lower levels. In fact, the sea breeze can provide the moisture to help form thunderstorm clouds. Once these form on the ranges to the west of Sydney, these clouds are generally steered toward the coast. Once these clouds get close to the coast, the sea breeze decreases in strength, whilst its direction will veer towards the east. Very soon after this, the sea breeze falters, we enter a short calm period before being hit by wind squalls out of the storm clouds. So the moral of the story is that the sea breeze can lead to its own demise. low stratus (scud), in the late afternoon as the moist sea breeze air becomes cooled and is also lifted slightly over the land.
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- On a warm summer day along the coast, this differential heating of land and sea leads to the development of local winds called sea breezes. As air above the land surface is heated by radiation from the Sun, it expands and begins to rise, being lighter than the surrounding air.
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- seabreezes occur during the afternoon i.e. during the day time  because the land remains warmer than the sea during the day. Low  pressure is created over the land causing … the winds to blow from  the sea to land .thus, sea breezes occur during the afternoon.
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Sea and Land Breezes The ancient Greeks were the first to write extensively of the sea-land breeze rhythm. Homer, in the Odyssey, related that both Odysseus and Telemachus set sail after dark to take advantage of the land breeze blowing out to sea.
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- Barber A strong wind carrying damp snow or sleet and spray that freezes upon contact with objects, especially the beard and hair. Bayamo A violent wind blowing from the land on the south coast of Cuba, especially near the Bight of Bayamo. Bentu de Soli An east wind on the coast of Sardinia. Bora A cold, northerly wind blowing from the Hungarian basin into the Adriatic Sea. See also FALL WIND.
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- The warm air rises up through convection, and cooler air from the ocean flows in to take its place. At night the reverse occurs, and the result (at least in late spring and summer, and close to the coast) is what's called a land breeze.. The ocean cools off slower than the land.
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Wind Wind refers to any flow of air relative to the earth's surface in a roughly horizontal direction. Breezes that blow back and forth from a body of water to adjacent land areas—on-shore and off-shore breezes, or land and sea breezes—are examples of local wind.
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Prevailing winds In areas where winds tend to be light, the sea breeze /land breeze cycle is the most important to the prevailing wind; in areas which have variable terrain, mountain and valley breezes dominate the wind pattern. Highly elevated surfaces can induce a thermal low, which then augments the environmental wind flow.inds are part of Earth's atmospheric circulation. Play media. Global surface wind vector flow lines colored by wind speed from June 1, 2011 to October 31, 2011. Prevailing winds are winds that blow predominantly from a single general direction over a particular point on the Earth 's surface.
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breeze 1 a wind or current of air, especially a light or moderate one. 2. a wind of 4–31 miles per hour (2–14 m/sec). 3. Informal. an easy task; something done or carried on without difficulty: Finding people to join in the adventure was a breeze. 4. Chiefly British Informal. a disturbance or quarrel.
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- Heat, Land and Sea. If you ever spend a vacation day at the beach, or on the shore of a large lake, you may notice a phenomenon that can help you remember how high and low pressure, and warm and cold air, translate into wind direction.
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Sea and Land Breezes A sea breeze describes a wind that blows from the ocean inland towards land. This breeze occurs most often in the spring and summer months because of the greater temperature differences between the ocean and nearby land, particularly in the afternoon when the land is at maximum heating from the sun.
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Why do sea breezes occur during the day but not the not at night? During the day, land is warmed at a faster rate than water (since water has a higher specific heat and therefore requires more time to be heated). The air over land is heated as well, and rises in the atmosphere. At the same time, cooler air from the sea moves to replace the rising warm air.
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Mid- Latitude Cyclones Westerlies. Prevailing winds that blow from west to east between 30 degrees and 60 degrees latitude in both hemispheres. For example, if person east has warm conditions and person west has cold conditions, in a matter of days person east will get the cold conditions, as the winds move easterly.
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What causes mountain breezes to form? Answer by Weatherbyrd. Confidence votes 227. After sunset the sun is no longer warming the mountain side and there is cooling of the air along the slope. The air becomes more dense and sinks into to valley. Thus the wind blows from the mountain side down into the valley and is thus called a mountain breeze.
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Sea Breezes and Land Breezes Low level wind shears are often enhanced by sea breeze circulation. Land breezes because the of reverse situation. Overnight the land cools to be colder than the sea so cold overland air moves to replace warmer the warmer air over the sea.
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Sea and Land Breezes The result is that a higher pressure is maintained. With a high pressure above the water and a lower pressure above the land, conditions are perfect for a small breeze to develop. Wind blows from the sea towards the land along the pressure gradient in an attempt to equalize pressure. This is known as a sea breeze. In the night, land cools down much quicker than does the waters of the ocean. As the land becomes cooler, so does the air above it. This results in air becoming more dense, forming a high pressure, causing winds to blow outward towards the sea. This is known as a land breeze.
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- Shortly after sunset a land breeze will flow from the warmer air over the land out towards the rapidly cooling air over the sea. sea breeze-from the sea towards shore land breeze-from the land towards the water. Source(s): http://www.islandnet.com/~see/weather/el... Mr.J · 6 years ago. Thumbs up.