due to high temperature north west India becomes a seat of low pressure .this condition attracts the south east trade winds from Southern Hemisphere and while crossing the equator the winds change their direction to south west
The winds that blow from the subtropical high pressure belts towards the subpolar low pressure belts are known as the westerlies. These winds move in a west-to-east direction in the middle latitudes of both hemispheres.
The trade winds in the tropics are caused by the difference in pressure between the subtropical high-pressure belts and the equatorial low-pressure trough. Air flows from the high-pressure areas towards the low-pressure areas, resulting in the trade winds blowing from east to west in both hemispheres. This pattern is influenced by the Earth's rotation and the Coriolis effect, which deflects the air towards the west, giving rise to the trade winds.
Global wind belts can cause all kinds of weather. They can pick up moisture and cause monsoons and prolonged wet seasons. They can cause calm regions of light winds, and they can also enhance warmth that causes mild weather.
The calm region produced by converging trade winds is called the doldrums. This area is known for its light winds and minimal atmospheric pressure, making it difficult for sailors to navigate through.
The trade winds diverge from the subtropical high-pressure zones located around 30 degrees latitude in both hemispheres. These high-pressure zones are areas where air descends and diverges towards the equator and the poles, creating the trade wind belts.
The equatorial breeze is called the Trade Winds. These winds blow from the subtropical high pressure to the equatorial low pressure, creating a distinct pattern of air circulation near the equator.
The winds that blow from the subtropical high pressure belts towards the subpolar low pressure belts are known as the westerlies. These winds move in a west-to-east direction in the middle latitudes of both hemispheres.
The bands of high pressure are called subtropical high-pressure belts, while the bands of low pressure are known as the intertropical convergence zone (ITCZ) or the equatorial low-pressure belt. These belts play a significant role in global atmospheric circulation.
Trade winds are steady, easterly winds that blow from the subtropical high pressure belts towards the equatorial low pressure zone. They are characterized by their consistency and direction, making them dependable for sailors' navigation. Trade winds play a crucial role in shaping global climate patterns by influencing ocean currents and affecting weather systems.
Because high pressure belts have sinking motion and dry conditions. Low pressure belts have rising motions and havey rainfall. pce
Prevailing winds Easterlies
The trade winds in the tropics are caused by the difference in pressure between the subtropical high-pressure belts and the equatorial low-pressure trough. Air flows from the high-pressure areas towards the low-pressure areas, resulting in the trade winds blowing from east to west in both hemispheres. This pattern is influenced by the Earth's rotation and the Coriolis effect, which deflects the air towards the west, giving rise to the trade winds.
The Coriolis effect explains this phenomenon clearly. Pressure belts and wind belts differ in patterns depending on certain atmospheric factors like temperature.
Global wind belts can cause all kinds of weather. They can pick up moisture and cause monsoons and prolonged wet seasons. They can cause calm regions of light winds, and they can also enhance warmth that causes mild weather.
Jet Streams are narrow belts of high speed winds.
The uneven heating of the earth produces pressure belts. these belts occur at about every 30 degrees latitude. The rotation of the Earth flings the bulk of the air creating an area of low pressure belt in this region.
belts of wind are trade winds