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naturally sea ice would have the advantage of having a greater albedo
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!
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.
Warming temperatures are melting sea ice in the Arctic. There is an albedo effect at the moment, which means that a lot of the sun's heat is reflected off the ice and back into space. If the ice melts then that reflective matter disappears and the darker sea below will absorb more heat and warm more quickly.
During the Ice Age, a significant amount of the water on Earth's surface was frozen, trapped in glaciers on land. This caused sea levels to lower. When the sea level lowered, what had been the sea floor between Russia and Alaska was exposed. This permitted many animals, including humans, to cross from Russia to Alaska, and that is how the first people arrived in the Americas.
naturally sea ice would have the advantage of having a greater albedo
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!
In rural settings, albedo is typically higher due to more natural surfaces like forests and grasslands that reflect sunlight. In urban settings, albedo is lower because of extensive pavement and buildings that absorb and retain heat, leading to the urban heat island effect.
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.
Warming temperatures are melting sea ice in the Arctic. There is an albedo effect at the moment, which means that a lot of the sun's heat is reflected off the ice and back into space. If the ice melts then that reflective matter disappears and the darker sea below will absorb more heat and warm more quickly.
During the Ice Age, a significant amount of the water on Earth's surface was frozen, trapped in glaciers on land. This caused sea levels to lower. When the sea level lowered, what had been the sea floor between Russia and Alaska was exposed. This permitted many animals, including humans, to cross from Russia to Alaska, and that is how the first people arrived in the Americas.
It does? Yes, it does. Before it melts, the ice reflects the sun's rays back out into space. This is called the albedo effect. After it melts, the sun's rays land on the black waters of the Arctic Ocean, which doesn't reflect the rays, but absorbs them, and the water gets hotter. This is how the melting ice causes more warming.
The albedo effect, characterised by changes in the reflection and absorption of sunlight, does play a small role in global warming, but requires global warming to be underway before it can play that part. As the world warms, ice caps and sea ice melt. Ice reflects much of the sun's energy back into space, but when the ice disappears the open sea and land absorb much of the sun's energy, becoming warmer. This accelerates global warming.
Any white or light colored surfaces reflect the sun's energy. The main ones are the Arctic sea ice, the Greenland ice cap, the whole of Antarctica and glaciers and snow cover all round the world. This reflective effect is called the albedo effect.
LAKI is an abbreviation for Limit of All Known Ice. This is a definition on the amount of time given between sightings of iceberg or sea-ice infested waters and ice-free waters.
Earth's seal levels drop during periods of glaciation, and are dependent on the amount of water locked away in the glacial ice.
Sea ice contains frozen minerals, such as salt, that is not frozen into freshwater ice.