During the day, the sea breeze blows from the sea to land as the air over the land warms up faster than the air over the water. At night, the land breeze blows from land to sea as the land cools down faster than the water due to the water's higher specific heat capacity, causing the air over the water to become warmer and less dense than the air over the land. The document defines and describes the sea breeze and land breeze patterns that occur daily as a result of the differing ways land and water absorb and release heat.

1. LAND AND SEA BREEZE MADE BY CHAMPA

2. DEFINITIONS THE WIND THAT BLOWS FROM SEA TO LAND IS CALLED THE SEA BREEZE OR ON SHORE WIND .THIS WIND BLOWS DURING THE DAY TIME. HOT AIR ON THE LAND RISES UP AND COOL AIR FROM THE SEA TAKES ITS PLACE.

3. SEA BREEZE During the day, the land warms up faster than the water . The warm air over the land rises, while the cooler air over the water sinks down and moves in to replace the warm air.

4. LAND BREEZE THE WIND THAT BLOWS FROM LAND TO SEA IS CALLED THE LAND BREEZE OR THE OFF SHORE WINDS .THIS WINDS BLOW DURING THE NIGHT. HOT AIR OVER THE SEA RISES UP AND COOL AIR FROM THE LAND TAKES ITS PLACE.

5. LAND BREEZE At night, dry land cools faster than water, due to the water’s large specific heat capacity . Since the land cools faster than the water, the air above the water is now warmer and less dense than the air above the dry land.

6. SEA BREEZE

7. DAY TIME MOVEMENT OF WINDS

8. LAND BREEZE

9. NIGHT TIME MOVEMENT OF WINDS

10. CLIMATIC REGIONS

11. CLIMATIC ZONES

12. VOLCANOES AROUND THE WORLD