1. Santa Ana winds are a major weather concern in California. These winds happen when high pressure builds up over the Great Basin desert. As the air moves toward the lower pressure of the Pacific Ocean, it is squeezed through narrow canyons, which makes it move faster. Because the air is falling fromRead more

    Santa Ana winds are a major weather concern in California. These winds happen when high pressure builds up over the Great Basin desert. As the air moves toward the lower pressure of the Pacific Ocean, it is squeezed through narrow canyons, which makes it move faster. Because the air is falling from high deserts to the low coast, it gets very hot and extremely dry. These “devil winds” can suck all the moisture out of lemon and orange trees and their high speeds can even knock fruit right off the branches, causing millions of dollars in losses.

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  2. The Bora is one of the most powerful cold winds in the world. It is common in the winter when the air over the snowy mountains of Central Europe becomes very heavy and cold. This air eventually "falls" down the slopes toward the warmer Adriatic Sea. Because it is moving downhill, it gains a lot of sRead more

    The Bora is one of the most powerful cold winds in the world. It is common in the winter when the air over the snowy mountains of Central Europe becomes very heavy and cold. This air eventually “falls” down the slopes toward the warmer Adriatic Sea. Because it is moving downhill, it gains a lot of speed, sometimes reaching over 200 km/h. It is a very dry wind that brings freezing temperatures to the coast. In some coastal towns, the wind is so strong that people have to use handrails along the streets just to stay upright!

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  3. The Westerlies are a key part of the Earth's global wind system. They blow from the subtropical high-pressure belts (around 30°) toward the subpolar low-pressure belts (around 60°). Because of the Coriolis effect caused by the Earth's rotation, these winds are tilted so that they always blow from thRead more

    The Westerlies are a key part of the Earth’s global wind system. They blow from the subtropical high-pressure belts (around 30°) toward the subpolar low-pressure belts (around 60°). Because of the Coriolis effect caused by the Earth’s rotation, these winds are tilted so that they always blow from the west. This is why airplanes flying from West to East (like from New York to London) usually travel much faster than those flying the opposite way! These winds are the primary reason why weather usually moves from west to east in temperate regions of the world.

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  4. Gravity is the anchor of our atmosphere. Every gas molecule, from oxygen to nitrogen, has a tiny amount of mass. Earth’s massive size creates a strong gravitational field that pulls these molecules toward the center of the planet. This pull is strongest at the surface, which is why the air is "thickRead more

    Gravity is the anchor of our atmosphere. Every gas molecule, from oxygen to nitrogen, has a tiny amount of mass. Earth’s massive size creates a strong gravitational field that pulls these molecules toward the center of the planet. This pull is strongest at the surface, which is why the air is “thicker” or more dense at sea level than it is on top of a mountain. Without gravity, the kinetic energy of the gas molecules would cause them to fly away into space, leaving Earth as a lifeless, airless rock like the Moon.

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  5. The sea breeze is a perfect example of a local "thermal" wind. During daylight hours, the sun warms both the land and the sea. However, solid ground absorbs heat more quickly than deep water. The air touching the hot ground becomes warm and light, causing it to rise upward. Over the ocean, the air rRead more

    The sea breeze is a perfect example of a local “thermal” wind. During daylight hours, the sun warms both the land and the sea. However, solid ground absorbs heat more quickly than deep water. The air touching the hot ground becomes warm and light, causing it to rise upward. Over the ocean, the air remains much cooler and more dense. Because nature always tries to balance pressure, the cool sea air moves inland to replace the rising warm air. This is why coastal areas often feel much cooler and more pleasant during a hot sunny afternoon.

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