It's called evaporation.
Carbon leaves the hydrosphere through processes such as outgassing from the ocean, where carbon dioxide is released into the atmosphere. Additionally, carbon can be taken up by marine organisms and then stored in their bodies or shells, eventually sinking to the ocean floor as sediment. Finally, carbon can re-enter the atmosphere through chemical reactions that release carbon dioxide back into the air.
Nitrogen enters the atmosphere from the lithosphere through processes like volcanic eruptions and denitrification by bacteria. It enters the hydrosphere mainly through rainwater and runoff. In the biosphere, nitrogen is absorbed by plants from the soil, and in the atmosphere, it leaves through denitrification and nitrogen-fixing bacteria returning it to the soil. In the geosphere, nitrogen is locked in rocks and minerals for long periods until released through weathering processes.
Gases can enter the atmosphere through natural processes like volcanic eruptions and biological decay, as well as human activities such as burning fossil fuels and industrial processes. Gases leave the atmosphere through processes like photosynthesis, where plants absorb carbon dioxide, and through chemical reactions that remove gases from the air. Wind and precipitation can also play a role in removing gases from the atmosphere.
Water leaves the atmosphere through a process called precipitation, where water vapor in the air condenses into liquid droplets or ice crystals and falls to the ground as rain, snow, sleet, or hail. Additionally, water vapor can also leave the atmosphere through evaporation and transpiration from plants.
Water leaves Earth's surface and enters the atmosphere through processes such as evaporation from oceans, lakes, and rivers, as well as transpiration from plants. Additionally, water is released into the atmosphere through sublimation from snow and ice.
the process that causes the water to enter and leave the cell is diffusion
By air
Filtration
Evaporation.
Carbon leaves the hydrosphere through processes such as outgassing from the ocean, where carbon dioxide is released into the atmosphere. Additionally, carbon can be taken up by marine organisms and then stored in their bodies or shells, eventually sinking to the ocean floor as sediment. Finally, carbon can re-enter the atmosphere through chemical reactions that release carbon dioxide back into the air.
The condition that does not heat to enter or leave the system.
Small uncharged substances enter and leave the cell membrane through passive diffusion. This process relies on the concentration gradient and does not require energy input from the cell.
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diffusion
Asteroids are the rocky planet remnants orbiting the solar system in the asteroid belt. Collisions between these objects may leave debris that can enter the Earth's atmosphere and become meteorites.
Nitrogen enters the atmosphere from the lithosphere through processes like volcanic eruptions and denitrification by bacteria. It enters the hydrosphere mainly through rainwater and runoff. In the biosphere, nitrogen is absorbed by plants from the soil, and in the atmosphere, it leaves through denitrification and nitrogen-fixing bacteria returning it to the soil. In the geosphere, nitrogen is locked in rocks and minerals for long periods until released through weathering processes.
They enter and leave on the or at the superior border.