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Shape of the Ocean Basins Because of Coriolis effect, the water goes right in the Northern Hemisphere and left in the Southern Hemisphere.

The Coriolis effect influences wind direction around the world in this way: in the Northern Hemisphere it curves winds to the right; in the Southern Hemisphere it curves them left. The exception is with low pressure systems.

Because the Earth rotates on its axis, circulating air is deflected toward the right in the Northern Hemisphere and toward the left in the Southern Hemisphere. This deflection is called the Coriolis effect. This deflection is called the Coriolis effect.

The Coriolis Effect deflects the path of the winds to the right in the Northern Hemisphere and to the left in the Southern Hemisphere. Adding this deflection leads to the pattern of prevailing winds illustrated in Figure 8.2.

When the air mass above the land becomes cooler than the air mass over water, the wind direction and convective cell currents reverse and the land breeze blows from land out to sea.

It is safer to surf at night because water has higher capacity than land/sand. During the day, land temperature increases more than the water and by convection, there is warmer air in the land and this air direction will go from land to the sea so the wind will move the waves away from the coast and towards the sea.

In coastal area, wind current moves from the sea towards the land during day; but during night it moves from land to the sea.

As this hot air rises up, a region of low pressure is created at the surface and air over the sea moves in to this area of low pressure. Hence, the direction of the wind is from the sea to the land during the day.

At nigh the land is cooler than water due to the fact that the land gets cooler and heater faster than the water. So at night the air over the water has higher temperature than that of land.So the air over water rises upwards. Due to which a low pressure area is created over the water .

Answer Expert Verified during the day, the land gets heated up fast and rise up. which creates a low pressure in land so the cool air above the sea, goes and occupies a space in land. so during the day the wind blows from sea to land in coastal areas. and the wind blows from land to sea at night time.

The direction of coastal winds changes from day to night. This is due to the differential heating of land and ocean.

A coastal region, for instance, undergoes changes in wind direction daily. The sun heats the land more quickly than the water. Warm air above the land rises, and cooler air above the water moves in over the land, creating an inland breeze.

Air in the atmosphere moves around the world in a pattern called global atmospheric circulation. When the air cools, it drops back to the ground, flows back towards the Equator, and warm again. The, now, warmed air rises again, and the pattern repeats. This pattern, known as convection, happens on a global scale.

As the temperature of the surface of the land rises, the land heats the air above it by convection. The air above the sea has a relatively higher pressure, causing air near the coast to flow towards the lower pressure over land.

Answer. Answer: sea breeze or onshore breeze is any wind that blows from a large body of water toward or onto a landmass; it develops due to differences in air pressure created by the differing heat capacities of water and dry land. As such, sea breezes are more localised than prevailing winds.

Between about 30 degrees north and 30 degrees south of the equator, in a region called the horse latitudes, the Earth’s rotation causes air to slant toward the equator in a southwesterly direction in the northern hemisphere and in a northwesterly direction in the southern hemisphere. This is called the Coriolis Effect.