The lower temperature is called wind chill
Sea breeze typically occurs during the day when the land heats up faster than the water, causing the air above the land to rise. This creates lower pressure over the land, drawing in cooler air from the sea to replace it. Sea breeze is most common in the afternoon when the temperature difference between land and water is greatest.
A land breeze originates at night when the land cools more quickly than the water. This temperature difference causes the air over the land to become cooler and denser, creating a high pressure area which pushes air towards the lower pressure area over the warmer water, resulting in a land breeze.
A sea breeze is created when the temperature of the land rises faster than that of the sea during the day. As the air over the land heats up, it rises, creating a low pressure area. This lower pressure draws in cooler air from the sea, resulting in a wind that blows from the sea towards the land.
The lower layer temperature typically refers to the temperature of the lower atmosphere, which can vary depending on location, time of day, and weather conditions. It is important for understanding weather patterns and climate dynamics.
Bulb temperature is typically lower than dry temperature because the bulb thermometer measures the temperature of the air without factoring in the effects of evaporation. The dry bulb temperature, on the other hand, accounts for the cooling effect of evaporation, giving a lower reading than the bulb temperature.
The seemingly lower temperature caused by excessive breeze is known as the "wind chill" effect. This phenomenon occurs when wind increases the rate of heat loss from the body, making it feel colder than the actual air temperature. Wind chill is particularly important to consider in cold weather, as it can lead to a higher risk of frostbite and hypothermia.
The wind chill effect causes the temperature to feel colder than it actually is because it removes heat from the body more quickly. When there is excessive breeze, it can enhance this effect, making it feel even colder than the actual temperature. Essentially, the wind carries away the heat your body generates, resulting in a lower perceived temperature.
During a sea breeze, cold air comes from the ocean, which has a lower temperature than the land. As the land heats up during the day, it warms the air above it, causing that air to rise. In contrast, the cooler air over the ocean moves in to replace the rising warm air, creating a breeze that flows from the sea towards the land. This temperature difference drives the sea breeze phenomenon.
Convection plays a crucial role in the formation of a breeze by facilitating the movement of air due to temperature differences. When the sun heats the Earth's surface, warm air rises, creating an area of lower pressure. Cooler air then moves in to replace the rising warm air, resulting in a breeze. This process is a part of the larger convection cycle that helps regulate temperature and distribute heat in the atmosphere.
It is because Chennai is a coastal region and the temperature is influenced by the presence of sea breeze i.e. it has moderate climate, whereas Lucknow don't have any such influence and so the annual range of temperature is high.
A mountain breeze is a local wind pattern that occurs in mountainous areas. During the day, air at higher elevations becomes warmer and rises, creating a breeze that flows downhill towards lower elevations. At night, the process reverses as the air at lower elevations cools and sinks, creating a breeze that flows uphill.
um.... sometimes, but i guess it depends on if the wind is a cold breeze or a warm wind but in winter ya it would be cold but no it does not lower temperature it might give you chills though?!?! justinbieber4eva!!!
Sea breeze typically occurs during the day when the land heats up faster than the water, causing the air above the land to rise. This creates lower pressure over the land, drawing in cooler air from the sea to replace it. Sea breeze is most common in the afternoon when the temperature difference between land and water is greatest.
A land breeze originates at night when the land cools more quickly than the water. This temperature difference causes the air over the land to become cooler and denser, creating a high pressure area which pushes air towards the lower pressure area over the warmer water, resulting in a land breeze.
It refers to wind chill factor. This is the decrease in air temperature that someone would feel because of a cold breeze of air flow. The wind chill factor will be lower than the air temperature. The opposite would be used with the heat index.
A land breeze occurs due to the difference in temperature between the land and the sea at night. As the land cools more quickly than the water, the air above the land becomes cooler and denser, causing it to sink and create high pressure. This high-pressure air then moves towards the lower pressure area over the warmer water, resulting in a breeze that blows from the land to the sea.
A sea breeze apex is primarily caused by the differential heating of land and water. During the day, land heats up more rapidly than the ocean, leading to lower air pressure over the land and higher pressure over the cooler water. This pressure difference causes cooler, denser air from the ocean to move inland, creating a breeze. The apex refers to the point where this breeze is strongest, typically occurring in the late afternoon when the temperature contrast is most pronounced.