circle the planet from pole to pole.
Jupiter's stripes are caused by various storms and the different gases in its atmosphere. Jupiter's atmosphere contains mostly hydrogen and helium, with trace amounts of methane, sulfur, ammonia, and water.
In the open atmosphere, cloudy conditions are often associated with sinking air that cools as it descends. This cooling can result in the saturation of the air, leading to the formation of clouds and potentially precipitation. The sinking air in cloudy conditions is generally stable and can inhibit vertical cloud development.
Because all the warm air is rising and traveling to the colder spots in the northern hemisphere.
Convection in the atmosphere occurs when warm air rises and cooler air sinks due to differences in temperature and density. As the sun heats the Earth's surface, the air above it warms up, becomes less dense, and rises. This rising air creates a low-pressure area, which allows cooler, denser air from surrounding areas to move in and replace it. This continuous cycle of rising and sinking air leads to the formation of wind patterns and contributes to weather phenomena.
No, convection in the Sun involves hot gas rising towards the surface due to its lower density, then cooling and sinking back into the interior. This process is driven by the heat produced in the Sun's core through nuclear fusion.
The belts and zones of Jupiter refer to alternating bands of clouds that encircle the planet. The belts are dark-colored, low-pressure zones with sinking air, while the zones are light-colored, high-pressure regions with rising air. These structures are caused by Jupiter's fast rotation and dynamic atmosphere.
Jupiter's stripes are caused by various storms and the different gases in its atmosphere. Jupiter's atmosphere contains mostly hydrogen and helium, with trace amounts of methane, sulfur, ammonia, and water.
Warm air rising and cold air sinking in combination with the rotation of the Earth cause the various currents in the atmosphere.
In the open atmosphere, cloudy conditions are often associated with sinking air that cools as it descends. This cooling can result in the saturation of the air, leading to the formation of clouds and potentially precipitation. The sinking air in cloudy conditions is generally stable and can inhibit vertical cloud development.
The rising and sinking motion is called convection current.
Hot particles rising and cold particles sinking create convection currents. This phenomenon is responsible for heat transfer in fluids, such as the movement of air in the atmosphere or water in the ocean. It plays a key role in driving weather patterns and ocean currents.
rising
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No, the sea level is rising
Rising and sinking air is called up draft and down draft, respectively.
The Himalayas are still rising at a rate of 5 millimeters per year.
The name given to the upward and downward movement of air in the atmosphere is convection. This movement is driven by temperature and pressure differences, with warm air rising and cool air sinking.