Polar surface currents bring low temperatures, as they originate from the polar regions where temperatures are colder. As these currents flow towards lower latitudes, they can affect the temperature of the regions they pass through.
Hot air moves towards cold air because of the principle of convection. When air is heated, it becomes less dense and rises, while cold air is denser and sinks. This movement creates a flow of air from hot areas to cold areas, balancing out the temperature difference.
Cold air masses that form at high latitudes are called polar air masses. These air masses originate over the polar regions, such as the Arctic and Antarctic, and bring cold temperatures when they move towards lower latitudes.
Generally the poles are cold places, receiving Sunlight at a low angle or no Sun at all. This means the air above the poles tends to be cooler than the rest of the planet. Cold air is dense so the pressure of the air at the poles tends to be higher than the rest of the planet. Thus air (cold air) tends to flow away from the polar regions along the Earth's surface to be replaced by light warmer air flowing into the poles at a higher level (this air then cools). There is therefore a general flow of warm air north and south towards the poles from the equator and a flow of cold air from the poles towards the equator. This flow of air spreads out the heat from the Sun, warming the poles and cooling the tropics. In detail this overall flow is restricted by the thickness of Earth's atmosphere and several flow cells form to complete the chain causing Earth's climatic zones.
Cold polar air flows toward the equator due to the difference in temperature and pressure between the polar regions and the equator. Air moves from high pressure to low pressure areas, and the temperature gradient drives the movement of cold air toward warmer regions.
The air mass indicated by cold dry air is a continental polar air mass, designated as cP. This air mass originates over cold land regions and brings cold, dry conditions when it moves into other areas.
It's Continental Polar.
The polar easterlies (also Polar Hadley cells) are the dry, cold prevailing winds that blow from the high-pressure areas of the polar highs at the north and south poles towards low-pressure areas within the Westerlies at high latitudes.
Polar easterlies. They are cold, dry winds that blow from the polar high-pressure areas towards lower latitudes.
Generally the poles are cold places, receiving Sunlight at a low angle or no Sun at all. This means the air above the poles tends to be cooler than the rest of the planet. Cold air is dense so the pressure of the air at the poles tends to be higher than the rest of the planet. Thus air (cold air) tends to flow away from the polar regions along the Earth's surface to be replaced by light warmer air flowing into the poles at a higher level (this air then cools). There is therefore a general flow of warm air north and south towards the poles from the equator and a flow of cold air from the poles towards the equator. This flow of air spreads out the heat from the Sun, warming the poles and cooling the tropics. In detail this overall flow is restricted by the thickness of Earth's atmosphere and several flow cells form to complete the chain causing Earth's climatic zones.
The cold winds that flow away from the North and South poles are called polar winds. These winds are characterized by their low temperatures and high pressure, and they play a role in shaping global climate patterns. The polar winds help distribute cold air from the poles towards lower latitudes.
Heat rises, cold falls. Hot air will rise towards the ceiling, while cold air will travel towards the floor. Thus, it's beneficial to have the air conditioning at a higher level to allow the cold air flow downwards.