Plants utilize carbon dioxide (CO2) to perform photosynthesis. This is fortunate, because all living things produce CO2 as a byproduct of respiration and oxidation. If the plants didn't absorb it, it would build up in the atmosphere to dangerous levels, and life as we know would cease to exist.
your question is... How did the Earth`s atmosphere change composotion to became today`s nitrogen and oxygen atmosphere? Answer: it happend with the help of solar untraviolet (uv) radiation,the very thing what we worry about now for its cancer-causing ability
By slowing down the earths rotation but will not make effect to humans .
They smooth earths surface
water, ice, wind, and snow.
L
cuz they can
it will always change
Photosynthesis drastically increased the oxygen content of the atmosphere.
The earths atmophere came from your mom!
The origin of free oxygen
more oxygen was consumed
The earths atmosphere has significantly altered over the years. The process of the earth's atmosphere was recognized and evolved 2.7 billion years ago, forming the nitrogen-oxygen atmosphere that exists today. This change enabled the formation and beginning of the ozone layer (which along with magnetic fields) block solar radiation.
your question is... How did the Earth`s atmosphere change composotion to became today`s nitrogen and oxygen atmosphere? Answer: it happend with the help of solar untraviolet (uv) radiation,the very thing what we worry about now for its cancer-causing ability
Photosynthesis is the process by which green plants, algae, and some bacteria convert sunlight into chemical energy in the form of glucose while releasing oxygen as a byproduct. This process is vital for sustaining life on Earth as it helps to maintain oxygen levels in the atmosphere and plays a crucial role in the global carbon cycle by removing carbon dioxide from the atmosphere.
Water changes the earths surface by it running across the land and picking it up and carrying away. The faster the water the more erosion. Erosion is the picking up and carrying away of rock material.
The air becomes less dense, the higher you go. And generally, the temperature gets colder until you reach the thermosphere, which is the hottest part of Earths atmosphere.
The air molecules spreds out in space so there is not enough air to breathe for us there