When he pushing up daisies, the daisies will grow better in a high CO2 environment.
Originally Posted by Ripmany
hilarious sir..
So excessive emissions of Co2 into the atmosphere warms the Earth's surface to the point of catastrophic proportions? So, let's just start from the basics there is only three ways in which to warm a surface, Convection, Conduction and Solar Radiation. Scientists know that but they aren't explaining how Co2 correlates with any one of these modes of warming. They just come up with anecdotal evidence to skirt the actual truth. They don't know how much Co2 was in the atmosphere 3 million years ago. There is no way of knowing so much of what they try to explain is mere speculation. Global Warming has become a Political Phenomenon and it's ridiculous. It's constantly being talked about but never a real solution.
Originally Posted by Levianon17
your 1st question answered:
Scientists determine past levels primarily through direct measurements from ice cores for recent geological history and geochemical proxies for more ancient eras.
Analyzing Ice Cores
First, For the last 800,000 years, scientists use ice cores drilled from ice sheets in Antarctica and Greenland. As snow falls, it traps tiny air bubbles. When the snow compresses into ice, these bubbles become "time capsules" of the ancient atmosphere. Scientists crush the ice in a vacuum to release the gas and measure the concentration of carbon dioxide directly using mass spectrometry.
Step 2: Studying Stomatal Density
For older periods, researchers examine fossilized leaves. Plants exchange gases through microscopic pores called stomata. There is an inverse relationship between atmospheric and stomatal density: when levels are high, plants require fewer stomata to obtain the necessary carbon for photosynthesis. By counting stomata on fossil leaves, scientists can estimate ancient concentrations.
Step 3: Utilizing Geochemical Proxies
When ice cores are unavailable, scientists use chemical signatures in marine sediments:
Boron Isotopes: The ratio of boron isotopes in the calcium carbonate shells of ancient marine organisms (foraminifera) depends on ocean pH. Since ocean pH is controlled by atmospheric CO2, this ratio serves as a proxy for gas levels.
Alkenones: These are organic molecules produced by certain algae. The carbon isotope fractionation within these molecules changes based on the amount of dissolved C02 available in the water during photosynthesis.
and your 2nd question answered:
Carbon dioxide causes global warming by acting as a heat-trapping greenhouse gas in the atmosphere. It absorbs infrared radiation (heat) emitted from the Earth's surface and re-emits it in all directions, including back toward the surface, preventing it from escaping into space. Increased concentration from human activity strengthens this natural effect.
The Mechanism:
Molecules absorb infrared energy at specific wavelengths (2,000–15,000 nm). Upon absorption, the molecules vibrate and release the energy as heat.
The "Blanket" Effect: While CO2 is a small fraction of the atmosphere, it functions like an insulating blanket. As human activities, such as burning fossil fuels and deforestation, increase concentrations, this blanket becomes thicker.
Energy Balance: The Earth absorbs energy from sunlight and emits it back as infrared, which traps heat. More CO2 means less heat escapes, leading to an increased average global surface temperature.
Responsible for Warming:
CO2 is the most important long-lived greenhouse gas, responsible for roughly 80% of the heating influence from human-produced gases since 1990.
any more questions..