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The atmosphere gos through many cycles and changes. The significant gases in our atmosphere have not changed substantially in the past several centuries. The primary gas is still Nitrogen, then Oxygen.
the appearance of oxygen-producing organisms
The Gaia hypothesis, thought of by scientist James Lovelock in the 1960s, is a preposition that the Earth behaves like a living organism. This is through interactions of the biosphere, lithosphere, atmosphere, and hydrosphere. It suggested that the Earth is capable of responding to changes in its environment like a living cell.
it is the ozone layer in the atmosphere because it is what keeps the atmosphere in check of what is happening in the atmosphere.
condensation
When plants and animals evolved, this made changes in the atmosphere on Earth
The atmosphere gos through many cycles and changes. The significant gases in our atmosphere have not changed substantially in the past several centuries. The primary gas is still Nitrogen, then Oxygen.
the appearance of oxygen-producing organisms
Because the composition of the atmosphere changes from day to day (specifically, the composition of particulates). These are what scatter sunlight in ways that can make sunsets colorful.
The air we breathe near sea level is approximately 78% nitrogen, 21% oxygen, and 1% other. The exact composition changes at different levels in the atmosphere.
Chemical Changes
The composition of everything and transfer of electrons. Changes in bonding and structure of compounds.
The Gaia hypothesis, thought of by scientist James Lovelock in the 1960s, is a preposition that the Earth behaves like a living organism. This is through interactions of the biosphere, lithosphere, atmosphere, and hydrosphere. It suggested that the Earth is capable of responding to changes in its environment like a living cell.
Chemical composition
Changes that occur when the composition remains the same
independent varibles
Chemical changes