Hot, less-dense air rises.
That would be "convection" cycle, and one of the steps is hot (therefore lighter) air rising.
Hot, less-dense air rises.That would be "convection" cycle, and one of the steps is hot (therefore lighter) air rising.
The step of the convection cycle in Earth's atmosphere involves warm air rising due to being less dense than the surrounding cooler air. As the warm air rises, it cools and eventually sinks back down, creating a continuous cycle of air movement. This convection process helps distribute heat and moisture around the globe.
In the convection cycle in Earth's atmosphere, warm air near the surface rises due to lower density, creating a low-pressure system. As the air rises and cools, it loses moisture through condensation, forming clouds and precipitation. Eventually, the now cooler and denser air descends back to the surface, creating a high-pressure system and completing the convection cycle.
evaporation
Condensation of water vapor directly into ice without passing through the liquid phase is a step that is not part of a normal convection cycle.
The convection cycle typically includes heating the fluid, causing it to expand and become less dense, rising due to buoyancy, cooling as it moves away from the heat source, becoming denser, and sinking back down to be reheated. The step of creating new fluid particles or evaporating the fluid is not typically part of the convection cycle.
It is the first step. Water is evaporated from plants.
Step 3 in the water cycle is precipitation, where water vapor in the atmosphere cools and condenses into water droplets or ice crystals, leading to the formation of clouds. When these droplets become heavy enough, they fall back to the Earth as rain, snow, sleet, or hail.
Cooked air rises creating a high pressure system below
Cooked air rises creating a high pressure system below
Precipitation wherein products of condensation in the atmosphere, as rain or snow, fall to the ground.
percipitation!