The gas concentrations in atmosphere are large. Even if we try, we can change small amounts.
Nothing. It is a gas that is found at various concentrations in our atmosphere.
No, carbon dioxide is a colourless transparent gas.
No, carbon monoxide is colourless transparent gas.
Showing gas concentrations as percentages of dry air allows for easier comparison of the relative amounts of different gases in the atmosphere. Dry air is a consistent reference point because its composition is relatively stable, making it a convenient baseline for expressing variations in gas concentrations.
A change in Earth's total insulation can be caused by variations in the Sun's output, changes in Earth's orbit, or alterations in the composition of Earth's atmosphere such as increased greenhouse gas concentrations.
The earth's atmosphere is projected to change due to human activities, leading to increases in greenhouse gas concentrations and global temperatures. This will likely result in more extreme weather events, rising sea levels, and changes in precipitation patterns. Adapting to these changes and reducing emissions are key to mitigating the impacts on the atmosphere.
The Earth's atmosphere has changed over time due to various factors such as volcanic activity, changes in greenhouse gas concentrations, and natural variations in solar radiation. Human activities, such as the burning of fossil fuels and deforestation, have also significantly impacted the composition of the atmosphere, leading to an increase in greenhouse gas emissions and global warming.
I would say helium because it is used commercially all over the world.
It would make the greenhouse effect stronger.
No, 'atmosphere' is NOT a change at all! It is a mixture of gasses and dust, mist or rain.
stomatal movements( it depends on light, temperature, condition of the plant, glucose & sucrose concentrations, ion concentrations....) , intra cellular gaps in spongy paranchyma, atmospheric & plant pressure, amount of gases in the atmosphere, ...... are the factors which effect the gas exchange.
The stratospheric region of the atmosphere is actually a region containing a thick layer of ozone gas which is known as the ozone layer. this ozone layer contains the maximum concentrations of ozone. thus the stratosphere can be regarded as the zone of the maximum concentrations of ozone.