[Response: Particularly amusing nonsense, since Jim has been pointing out the importance of black carbon deposition (which replaces the normally highly
reflective snow surface with highly absorbing particulates, thus enhancing surface warming) on Arctic warming for a number of years.
Not exact matches
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.
Examples of
reflective objects include a mirror, a smooth metal can, a car window, a glass bottle, ice,
snow or the watery
surface of a lake.
Well, almost encloses: Enceladus sprays geysers of water ice out into space, some of which settles back down to the moon's
surface in the form of
snow, making it the most
reflective planetary object in the solar system.
Global average temperature is lower during glacial periods for two primary reasons: 1) there was only about 190 ppm CO2 in the atmosphere, and other major greenhouse gases (CH4 and N2O) were also lower 2) the earth
surface was more
reflective, due to the presence of lots of ice and
snow on land, and lots more sea ice than today (that is, the albedo was higher).
This pollution darkens the bright,
reflective surfaces of ice and
snow, accelerating warming and melting.
Because darker
surfaces absorb more heat than lighter, more
reflective ones, if enough soot is deposited on
snow and ice it can accelerate melting.
The reason, Werner said, is because the loss of
snow and ice makes the earth's
surface less
reflective, meaning solar radiation — or heat — is absorbed in greater amounts by the exposed dark ocean or tundra.
Thawing permafrost also delivers organic - rich soils to lake bottoms, where decomposition in the absence of oxygen releases additional methane.116 Extensive wildfires also release carbon that contributes to climate warming.107, 117,118 The capacity of the Yukon River Basin in Alaska and adjacent Canada to store carbon has been substantially weakened since the 1960s by the combination of warming and thawing of permafrost and by increased wildfire.119 Expansion of tall shrubs and trees into tundra makes the
surface darker and rougher, increasing absorption of the sun's energy and further contributing to warming.120 This warming is likely stronger than the potential cooling effects of increased carbon dioxide uptake associated with tree and shrub expansion.121 The shorter
snow - covered seasons in Alaska further increase energy absorption by the land
surface, an effect only slightly offset by the reduced energy absorption of highly
reflective post-fire
snow - covered landscapes.121 This spectrum of changes in Alaskan and other high - latitude terrestrial ecosystems jeopardizes efforts by society to use ecosystem carbon management to offset fossil fuel emissions.94, 95,96
About 30 percent of the radiation striking Earth's atmosphere is immediately reflected back out to space by clouds, ice,
snow, sand and other
reflective surfaces, according to NASA.
When black carbon falls on ice and
snow, it smudges their bright white
reflective surfaces.
When soot falls on
snow and ice it increases the amount of light and heat that is absorbed, just like any
reflective surface.
What you don't want is bigger shrubs and trees that will lessen the albedo, making for a darker, less
reflective surface that warms the immediate vicinity and feeds into the normal
snow - loss albedo shift.