naturally sea ice would have the advantage of having a greater albedo
The reason the ice in the Antarctica does not melt away when sunlight shines upon it is because the whiteness of the ice reflects most of the light back into space. But as a result of global warming, much more ice are being melted now than before. And thus without the ice, more sea will appear. And with the sea, there were not as much ice to reflect the sunlight back into space, therefore more of the sunlight and its heat were absorbed by earth, and thus more and more ice will melt.
The albedo effect reflects the sun's radiation helping to slow the effects of global warming (like sea ice, white ice caps and glaciers). If (or when) these melt, then the reflection will stop and the warming will speed up!
A low albedo means that a surface absorbs more sunlight and heat, leading to warming. This can contribute to climate change by increasing temperatures and melting ice caps, which in turn can lead to rising sea levels and changes in ecosystems.
Sea ice has an albedo of between 0.5 and 0.7. This means that it reflects between 50 and 70% of the sun's radiation (that lands on the ice).Ice with snow on it has a higher albedo, between 70 and 90%.Of the 100% of the sun's radiation that reaches the earth, 4% is reflected by the earth's surface, with about 2% reflected by ice.
naturally sea ice would have the advantage of having a greater albedo
Sea ice helps keep the planet cool by reflecting sunlight back into space, which reduces the amount of heat absorbed by the Earth's surface. This process, known as the albedo effect, helps regulate the planet's temperature and climate.
"Albedo" is the refectivity of something. Snow and ice have a high albedo since they are white. Pavement has a low albedo since it is darker. Albedo is important because it reflects sunlight back into outer space. As more and more glaciers, snowpack and pack-ice at sea melt away, less sunlight is relected into space and more light is absorbed as heat by the land and sea. This heat accelerates global climate change.
The reason the ice in the Antarctica does not melt away when sunlight shines upon it is because the whiteness of the ice reflects most of the light back into space. But as a result of global warming, much more ice are being melted now than before. And thus without the ice, more sea will appear. And with the sea, there were not as much ice to reflect the sunlight back into space, therefore more of the sunlight and its heat were absorbed by earth, and thus more and more ice will melt.
The albedo effect reflects the sun's radiation helping to slow the effects of global warming (like sea ice, white ice caps and glaciers). If (or when) these melt, then the reflection will stop and the warming will speed up!
A low albedo means that a surface absorbs more sunlight and heat, leading to warming. This can contribute to climate change by increasing temperatures and melting ice caps, which in turn can lead to rising sea levels and changes in ecosystems.
Melting ice does not directly affect sea surface temperatures because the temperature of the ice is already at freezing point (0°C). However, as the ice melts, it can impact local water temperatures through changes in albedo and heat absorption. This can contribute to overall changes in global sea surface temperatures over time.
Sea ice has an albedo of between 0.5 and 0.7. This means that it reflects between 50 and 70% of the sun's radiation (that lands on the ice).Ice with snow on it has a higher albedo, between 70 and 90%.Of the 100% of the sun's radiation that reaches the earth, 4% is reflected by the earth's surface, with about 2% reflected by ice.
This would alter the snow-albedo feedback. Darkening the surface of snow/ice greatly lowers the albedo (reflectivity) of the surface. This would cause the snow/ice surface to absorb more solar radiation by virtue of its lower albedo, which would allow it to heat up more. Normally most solar radiation is simply reflected by snow back into the atmosphere and mostly out to space, so by causing it to absorb more you are heating up the lower atmosphere. By doing this, you are more likely to melt the snow/ice, whereby the albedo will be even lower, which would then absorb more radiation, etc.. This is called a positive feedback loop.
During an ice age, sea levels typically drop because a significant amount of water becomes locked up in glaciers and ice sheets on land. As the ice sheets expand, they draw water from the oceans, causing sea levels to decrease.
During the ice age, a significant amount of water was locked up in glacial ice, causing sea levels to drop. This resulted in more water being stored on land in the form of ice sheets, which led to lower sea levels globally.
When glaciers and sea ice melt, they reduce the Earth's albedo (reflectivity), causing more sunlight to be absorbed rather than reflected back to space. This leads to increased warming and further melting of glaciers and sea ice. Additionally, as ice melts, it exposes darker surfaces underneath (like water or land), which absorb more heat and perpetuate the melting cycle.