Dark
seas absorb sunlight and continue to get warmer.
Not exact matches
A possible cause for the accelerated Arctic warming is the melting of the region's
sea ice, which reduces the icy, bright area that can reflect
sunlight back out into space, resulting in more solar radiation being
absorbed by the dark Arctic waters.
The shrinking
sea ice drives a classic positive feedback loop: as more ice melts, fewer patches of white snow reflect solar energy, and larger regions of dark,
sunlight -
absorbing seawater open up — both causing the ice to melt even faster.
Sea ice and snow cover loss create a feedback look that can accelerate global warming; with fewer reflective surfaces on the planet, more
sunlight can thereby be
absorbed, driving surface temperatures even higher, the scientists explained.
«The warming effect could be through the direct heating to the air, snow and
sea ice by
absorbing sunlight, and then accelerating the melting of snow and
sea ice,» Wang said.
During the melt season the albedo of seasonal ice is less than multiyear Seasonal ice
absorbs and transmits more
sunlight to ocean than multiyear Albedo evolution of seasonal
sea ice has 7 phases
This is of particular concern to scientists because of the albedo effect, where the replacement of highly reflective
sea ice with darker open water greatly increases heat
absorbed from
sunlight.
By melting
sea ice, warming in the Arctic regions allows more
sunlight to be
absorbed by the ocean which leads to yet more warming.
Additionally, the less
sea ice covers the surface of the ocean, the more
sunlight is
absorbed by the water, which scientists warn could accelerate the Arctic's warming.
But the Arctic
sea ice has hit near - record minimums of
sea ice since 2002, meaning the ocean is
absorbing more
sunlight, and heat, than it used to, leading to more ice melt.
Only little problem with that is that Antarctic
sea ice has no effect on
sunlight absorbed in the Arctic ocean.
In the polar regions, where few such storms occur, heating by greenhouse gases remains at the surface, and is exacerbated by the melting of bright
sea ice that exposes more of the dark ocean surface and causes more
sunlight to be
absorbed.
«This H2O negative - feedback effect on CO2 is ignored in models that assume that warm moist air does not rise and form
sunlight - reflecting clouds, but remains as humid air near
sea level,
absorbing infrared radiation from the sun, and approximately doubling the temperature rises predicted from atmospheric CO2 increases.
Essentially Arctic
sea ice is more important for the earth's energy balance because when it increasingly melts, more
sunlight is
absorbed by the oceans whereas Antarctic
sea ice normally melts each summer leaving the earth's energy balance largely unchanged.
As some had pointed out ever since the 19th century, in times when
sunlight fell more strongly on northern latitudes in the spring, snow and
sea ice would not linger so long; the dark earth and seawater would
absorb more
sunlight, and get warmer.