it starts out as water in a ocean. it then goes to the next step called evaporation. evaporation is when the clouds "suck" up all of the water. after evaporation is condensation. condensation is where the water becomes a cloud from all of the water vapor in the air. after condensation is precipitation. as you may know, precipitation is when we get rain, snow, hail, or any other types of "water falling from the sky" after that the water may go to the ground and become groundwater and fall right back to the ocean where the water cycle will start over again.
Hadley cells
The Stratosphere
no
Phosphorus does not cycle through the Earth's atmosphere like carbon or nitrogen. Instead, phosphorus cycles mainly through terrestrial and aquatic ecosystems, where it moves slowly between soil, water, and living organisms. Due to its limited atmospheric presence, phosphorus primarily enters the environment through weathering of rocks and minerals.
Plate tectonics can change the Earth's atmosphere through volcanic activity at plate boundaries. Volcanoes release gases like carbon dioxide and sulfur dioxide into the atmosphere, affecting its composition and contributing to natural climate change. Tectonic movements can also impact weather patterns and circulation in the atmosphere.
The model that scientists use to describe air circulation in Earth's atmosphere is called the Global Circulation Model (GCM). These models simulate the interactions between the atmosphere, oceans, land surface, and ice to predict climate patterns and changes.
Hadley cells
Hadley cells
no.
yes.
The transfer of heat by the movement of air currents in Earth's atmosphere is an example of convection. As warmer air rises and cooler air sinks, heat is transferred through the circulation of air in the atmosphere.
no way obviously not
mold fossils
vaporization
Scientists estimate that more than 50 percent of the oxygen in Earth's atmosphere is produced by phytoplankton in the ocean through photosynthesis. Phytoplankton are microscopic marine organisms that play a crucial role in the global oxygen cycle.
The ozone layer.
Meteorites.