Breeze is the name given to the light and chilly breeze. It is one of the most wonderful sensations to feel a cold and moderate wind on a hot summer day at the beach.
Both land breeze and sea breeze occur around big bodies of water.
The primary distinction between the two forms of Breeze is that water maintains heat for a longer period of time. The temperature differential between land and water produces a change in the density of the air over their respective surfaces. The Breeze is generated by the alternating airflow induced by the consequent low pressure. People who live near the shore get cold sea breezes during the day and warm land breezes at night. These breezes also have an impact on the temperature, humidity, and precipitation rates. The land wind and sea breeze diagrams are shown below, along with an explanation of how they occur.
The passage of wind from land to water is referred to as the land breeze; it is also referred to as offshore wind at times. During the night and early morning, the temperature of the land is lower than that of the surrounding water body. The land wind lasts longer in the last weeks of summer because the warmth of the water increases the daily temperature fluctuation on the land.
The following diagram depicts how the land wind is formed:
The flow of winds from vast bodies of water such as the sea and ocean is referred to as the sea breeze; these winds are also referred to as onshore winds. These Breezes occur more frequently during the spring and summer seasons when there is a greater temperature differential between the land and the nearby water bodies. This is particularly noticeable in the afternoon when the land achieves its peak temperature. When compared to land breezes, sea breezes are more dependable throughout the winter season, which may also be attributable to the large temperature differential between the sea and land, which can also create thunderstorms and bring in the rain. The sea breezes are not as noticeable during the fall and winter months due to the lower temperature differentials.
The following process explains the development of a sea breeze:
|Sea breeze||Land breeze|
|The sea breeze is usually strong.||When opposed to sea wind, a land breeze is shallower.|
|The sea breeze lowers the temperature.||In general, the land breeze has little influence on temperature.|
|During the summer and spring seasons, a sea breeze is more common. This is due to the fact that temperatures remain higher during the day during these seasons.||During the winter and fall, a land wind is more prevalent. At such periods, the nights tend to be colder.|
|Sea breezes are often faster, reaching velocities of up to 20 knots.||The land breeze is significantly slower, with peak speeds of up to 8 knots.|
|Sea breeze contains more moisture, which it collects when it blows over a body of water.||Land breeze is drier because it cannot absorb water from any source.|
|Finally, the sea wind passes from the sea to a land mass.||Land wind blows from land to a body of water, usually a sea or ocean.|