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AlexCastleberry (トーク | 投稿記録) (ページの作成:「<br>Hurricanes are powerful storms, and captivate human imagination. Hurricane Harvey hit Texas in August 2017, flooding one among the biggest metro areas in the United States. Lower than two weeks later, ideas turned to hurricane Irma, among the strongest Atlantic hurricanes ever measured. And as hurricane Sandy made its approach to the Eastern coast of the United States in October 2012, meteorologists referred to as the storm unprecedented by way of its potential…」) |
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2025年8月31日 (日) 18:58時点における最新版
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The gases that make up Earth's environment are subject to the planet's gravity. The truth is, the atmosphere weighs in at a combined 5.5 quadrillion tons (4.99 quadrillion metric tons). The gas molecules at the underside, or those closest to the Earth's floor the place all of us stay, are compressed by the burden of the air above them. The air closest to us is also the warmest, because the atmosphere is usually heated by the land and the sea, not by the sun. To grasp this precept, think of a person frying an egg on the sidewalk on a hot, sunny day. The heat absorbed by the pavement truly fries the egg, not the heat coming down from the sun. When air heats up, its molecules move farther apart, making it much less dense. This air then rises to higher altitudes the place air molecules are much less compressed by gravity. When heat, low-pressure air rises, cool, high-stress air seizes the chance to move in underneath it.
This motion is known as a stress gradient drive. What else is occurring? Well, as we know, warm, moist air from the ocean's floor begins to rise quickly. As it rises, its water vapor condenses to form storm clouds and droplets of rain. The condensation releases heat called latent heat of condensation. This latent heat warms the cool air, inflicting it to rise. This rising air is replaced by extra heat, humid air from the ocean beneath. And the cycle continues, Wood Ranger Power Shears sale drawing more heat, moist air into the creating storm and shifting heat from the surface to the ambiance. This change of heat creates a pattern of wind that circulates around a center, like water going down a drain. But what about these signature ferocious winds? Converging winds at the surface are colliding and pushing heat, moist air upward. This rising air reinforces the air that is already ascending from the floor, so the circulation and wind speeds of the storm increase.