D) all of the above
methane, nirtous oxide, water vapour
because they all absorb solar radiation the atmosphere
The process most responsible for the increase in early Earth's atmospheric oxygen levels is photosynthesis. This is the process by which plants, algae, and some bacteria convert carbon dioxide and sunlight into oxygen and energy. Over time, the accumulation of oxygen from photosynthesis led to the rise in atmospheric oxygen levels.
Human activities have increased atmospheric carbon dioxide levels primarily through the burning of fossil fuels for energy, deforestation, and industrial processes.
Solar radiation is greater in a particular area due to factors such as proximity to the equator, low levels of atmospheric pollution, clear skies, and minimal cloud cover. Additionally, the angle of the sun's rays and altitude can also contribute to varying levels of solar radiation in different regions.
The process most responsible for the increase in early Earth's atmospheric oxygen levels is thought to be the evolution of photosynthetic organisms, such as cyanobacteria, which released oxygen as a byproduct of photosynthesis. This oxygen eventually accumulated in the atmosphere, leading to the Great Oxidation Event around 2.4 billion years ago.
Burning fossil fuels releases carbon dioxide into the atmosphere. This carbon dioxide acts as a greenhouse gas, trapping heat and leading to an increase in global temperatures. This contributes to the net increase in atmospheric carbon levels, as it adds to the overall concentration of greenhouse gases in the atmosphere.
An increase in the atmospheric levels of carbon dioxide is the biggest contributor to global warming.
An increase in the atmospheric levels of carbon dioxide is the biggest contributor to global warming.
An increased level of atmospheric carbon can have a massive impact on photosynthesis. It can boost photosynthesis in plants for example.
The process most responsible for the increase in early Earth's atmospheric oxygen levels is photosynthesis. This is the process by which plants, algae, and some bacteria convert carbon dioxide and sunlight into oxygen and energy. Over time, the accumulation of oxygen from photosynthesis led to the rise in atmospheric oxygen levels.
umm the greenhouse gets hotter
An increase in the atmospheric levels of carbon dioxide is the biggest contributor to global warming.
Human activities have increased atmospheric carbon dioxide levels primarily through the burning of fossil fuels for energy, deforestation, and industrial processes.
Yes, cyanobacteria can increase the levels of carbon dioxide in the atmosphere through the process of respiration. However, cyanobacteria also play a significant role in reducing atmospheric carbon dioxide levels through photosynthesis, where they convert carbon dioxide into organic compounds. Overall, the impact of cyanobacteria on atmospheric carbon dioxide levels depends on the balance between these two processes.
Solar radiation is greater in a particular area due to factors such as proximity to the equator, low levels of atmospheric pollution, clear skies, and minimal cloud cover. Additionally, the angle of the sun's rays and altitude can also contribute to varying levels of solar radiation in different regions.
Exposure to high levels of radiation can have immediate health effects, such as burns and radiation sickness. Long-term exposure to low levels of radiation can increase the risk of cancer and other health issues over time. It's important to minimize exposure to radiation through safety measures and regulations.
Exposure to high levels of radiation, around 1 to 10 sieverts, can lead to severe radiation sickness, organ failure, and ultimately death. Long-term exposure to lower levels of radiation can also increase the risk of cancer. It is important to minimize exposure to radiation as much as possible to protect health.
The process most responsible for the increase in early Earth's atmospheric oxygen levels is thought to be the evolution of photosynthetic organisms, such as cyanobacteria, which released oxygen as a byproduct of photosynthesis. This oxygen eventually accumulated in the atmosphere, leading to the Great Oxidation Event around 2.4 billion years ago.