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Heat Transfer in Nature - Land and Sea Breeze

Grade 7CBSE

Review the key concepts, formulae, and examples before starting your quiz.

🔑Concepts

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Heat transfer in fluids (liquids and gases) primarily occurs through the process of Convection.

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The land heats up and cools down much faster than the sea. This differential heating is the primary cause of coastal winds.

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Sea Breeze: During the day, land temperature (TlandT_{land}) is higher than sea temperature (TseaT_{sea}). Warm air over the land rises, creating low pressure. Cool air from the sea blows towards the land to take its place.

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Land Breeze: At night, the land cools down faster, making Tland<TseaT_{land} < T_{sea}. The air above the sea is warmer and rises, causing cool air from the land to blow towards the sea.

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Air always moves from a region of High Pressure (cooler air) to a region of Low Pressure (warmer air).

📐Formulae

Density (ρ)∝1Temperature (T)\text{Density } (\rho) \propto \frac{1}{\text{Temperature } (T)}

Wind Direction: High Pressure →Low Pressure\text{Wind Direction: High Pressure } \rightarrow \text{Low Pressure}

ΔT=∣Tland−Tsea∣\Delta T = |T_{land} - T_{sea}|

💡Examples

Problem 1:

During the day in a coastal area, the temperature of the land is 35∘C35^\circ C and the temperature of the sea is 28∘C28^\circ C. In which direction will the wind blow?

Solution:

The wind will blow from the sea to the land (Sea Breeze).

Explanation:

Since Tland=35∘CT_{land} = 35^\circ C and Tsea=28∘CT_{sea} = 28^\circ C, then Tland>TseaT_{land} > T_{sea}. The air over the land becomes lighter and rises, creating a low-pressure zone. The cooler, denser air from the sea (28∘C28^\circ C) moves towards the land to fill the gap.

Problem 2:

A person living in a coastal house notices that the wind blows towards the sea at 11:00 PM. Explain this phenomenon using the concept of heat transfer.

Solution:

At night, the land cools faster than the sea, causing air to move from land to sea.

Explanation:

This is a Land Breeze. At night, the land loses heat faster than the water. This means Tland<TseaT_{land} < T_{sea}. The air above the sea is warmer and rises, while the cool air from the land moves towards the sea.