cool and dry
The ocean acts as a giant thermostat by transferring heat from the equator to the poles through a process called thermohaline circulation. Warm water moves towards the poles, releases heat, becomes denser and sinks, then circulates back towards the equator to complete the cycle. This regulates the climate by distributing heat more evenly across the globe.
The circulation of tropical air is driven by the Hadley cell, a large-scale atmospheric circulation pattern that transports warm air from the tropics towards the poles and cold air from the poles towards the tropics. This circulation plays a key role in shaping global weather patterns and climate.
The decrease in temperature towards the north and south poles is primarily due to the angle at which sunlight hits the Earth's surface. Near the equator, sunlight is more direct and concentrated, leading to warmer temperatures. As one moves towards the poles, the sunlight strikes at a lower angle, spreading the energy over a larger area and reducing its intensity. Additionally, the poles experience longer periods of darkness during winter, further contributing to lower temperatures.
Yes, ocean currents can help redistribute heat from the equator towards the poles by moving warm water from the tropics towards higher latitudes. This heat transfer can influence local and global climates by influencing air temperature and humidity in different regions.
Air circulates in global wind systems due to differential heating of the Earth's surface by the sun. Warm air rises at the equator and moves towards the poles, while cool air from the poles moves towards the equator to replace the rising warm air. This creates the prevailing wind patterns on Earth.
cool and dry
Heat moves from the tropics to the poles through a process called atmospheric circulation. Warm air rises at the equator, moves towards the poles at high altitudes, and then descends back towards the surface at around 30 degrees latitude. This creates wind patterns that help to distribute heat from the tropics to the poles.
colder and denser. This results in high pressure systems forming in polar regions.
The ocean acts as a giant thermostat by transferring heat from the equator to the poles through a process called thermohaline circulation. Warm water moves towards the poles, releases heat, becomes denser and sinks, then circulates back towards the equator to complete the cycle. This regulates the climate by distributing heat more evenly across the globe.
The circulation of tropical air is driven by the Hadley cell, a large-scale atmospheric circulation pattern that transports warm air from the tropics towards the poles and cold air from the poles towards the tropics. This circulation plays a key role in shaping global weather patterns and climate.
5. Tropics, subtropics and poles. subtropics are between the tropics and poles on each side.
Warm water flows towards the poles due to a combination of factors, including wind patterns, currents, and Earth's rotation. As warm water moves towards the poles, it cools and becomes denser, eventually sinking and circulating back towards the equator in a global pattern known as thermohaline circulation. This process helps distribute heat around the world's oceans.
Because the poles are at no point directed straght towards the sun, its due to the Earth being upright (with a small tilt) as it circles the sun. The sun will never be directly overhead outside the tropics.
Tropics- area near equator polar- area closer to the poles
At the poles, the Coriolis force is minimal, causing the wind to be less affected by its deflective influence. The Coriolis force is based on the rotation of the Earth and is strongest at the equator, gradually weakening towards the poles. As a result, wind deflection decreases towards the poles and becomes nearly zero.
The decrease in temperature towards the north and south poles is primarily due to the angle at which sunlight hits the Earth's surface. Near the equator, sunlight is more direct and concentrated, leading to warmer temperatures. As one moves towards the poles, the sunlight strikes at a lower angle, spreading the energy over a larger area and reducing its intensity. Additionally, the poles experience longer periods of darkness during winter, further contributing to lower temperatures.
The amount of heat from the equator becomes less as one moves towards the poles due to the increasing angle of sunlight. Near the equator, sunlight hits the Earth's surface more directly, providing more heat. However, as you move towards the poles, the sunlight is spread over a larger area, leading to less heat per unit area.