The ocean water absorbed much of the carbon dioxide from the atmosphere.
carbon dioxide
The Earth atmosphere is formed from gases.
When Earth formed, it was initially composed of gases such as hydrogen, helium, methane, and ammonia. Over time, these gases gradually dissipated into space or were absorbed into the planet's interior. The gases released from the Earth's interior during volcanic activity contributed to the formation of the early atmosphere.
evaporation.
Helium is most commonly found in the Earth's crust, often in natural gas deposits. It can also be found in the atmosphere in small amounts. Helium is not typically found in significant quantities in the oceans.
when the water turns into gas form as water vapour
The process by which water in rivers, lakes, and oceans is converted to a gas and moves into the atmosphere is called evaporation. Evaporation occurs when the sun's heat causes water on the Earth's surface to change from a liquid to a vapor form, which then rises into the atmosphere.
Yes, carbon dioxide is a heavy, odorless, colorless gas that is formed during respiration and by the decomposition of organic substances. It is absorbed by plants during photosynthesis to produce oxygen.
The upper layer of the atmosphere is formed by ozone layer. This is a layer of ozone gas.
Earth's early atmosphere was primarily composed of gases like methane, ammonia, and carbon dioxide due to volcanic activity. Over time, the atmosphere transformed as oceans formed and primitive life evolved, leading to the development of oxygen as a dominant gas. Today's atmosphere is mostly nitrogen and oxygen, which supports complex life forms.
In the past 50 to 100 years, man has burned about one halve of all the oil which formed through the ages, plus large amounts of coal, lumber, and natural gas. This is the source of the carbon dioxide. It would be worse except the oceans absorbed some of the carbon dioxide increase.
Methane is a gas fossil fuel that can be found in deep oceans. It is the main component of natural gas and is formed by the decomposition of organic matter in anaerobic conditions under high pressure and low temperatures in deep ocean sediments.