If I assume surface melting of 1M / year over the interior, say 500e3 KM ** 2 due to warmer climate &
darker ice surface (old wet ice versus clean dry snow) that would contribute 1.4 mm / year to sea levels.
Not exact matches
Unlike Saturn's bright rings, which are made almost entirely of
ice particles, Mars's rocky ring will be
dark and largely invisible from Earth, although the cloud of orbiting Phobos bits will at first be dense enough to cast a shadow on the Red Planet's
surface during some parts of the planet's orbit around the sun, the researchers say.
«The fact that a large portion of the western flank of the Greenland
ice sheet has become
dark means that the melt is up to five times as much as if it was a brilliant snow
surface.»
Cassini also resolved a longstanding mystery about why one half of the moon's
surface is 10 times as bright as the other: The leading hemisphere of the moon picks up
dark debris that is warmed by the sun, while brighter
ices condense on the colder, trailing hemisphere.
Quaoar has a
dark surface and «is probably made out of half rock and half
ice,» Trujillo says.
On January 14, the Huygens probe will parachute to the
surface and show what lies beneath the haze: Light areas may be
ice continents;
darker regions could be chilly ethane seas.
Quantitative analysis has evidenced the acceleration system of melting
ice:
dark water
surfaces absorb more heat than white
ice surfaces, thus melting
ice and making more water
surfaces in the Arctic Ocean.
Thinner
ice means a
darker surface, which increases the region's capacity to store heat and thus enables more melting.
Sunlight tends to bounce off the white, reflective
surfaces of glaciers and
ice sheets, but the
darker surfaces of dirty ground
ice can absorb greater amounts of solar radiation.
The flybys produced superb images of the
surfaces of Jupiter's large Galilean satellites, revealing sulphurous volcanoes on Io,
ice chasms on Europa, huge ringed impact craters on Callisto, and polygonal
dark regions on Ganymede.
As the sea
ice melts, its white reflective
surface is replaced by a relatively
dark ocean
surface.
«It's fairly intuitive to expect that replacing white, reflective sea
ice with a
dark ocean
surface would increase the amount of solar heating,» said Pistone.
That makes it likely that the
surface is
dark and dusty rather than coated in clean
ice.
The spacecraft also took measurements of the planet's
surface with a laser, which again suggested patches of
ice — although some of the bright regions in the radar images showed up
dark in the laser's readings.
Buie thinks Pluto's
darker appearance is due to evaporation and redistribution of
ice on the
surface, which is in a delicate equilibrium with the thin atmosphere.
Adapted to cold,
dark and nutrient - poor environments, below
ice and snow, the charr's activity rhythms reflect the above -
surface daily photoperiod.
But when sea
ice melts, it exposes the
darker surface of the underlying water, which absorbs solar energy.
The
surface is composed of three major types of terrain: bright, rough regions that are similar to Xanadu Regio,
dark regions that are rich in water
ice, and
dark regions that are covered by fields of dunes.
As part of the UK's Filchner
Ice Shelf System (FISS) Project, it was sent deep below the
surface, exploring the
dark and mysterious underbelly of the oversized floating glacier.
This is because when the Earth warms, snow and
ice melt, uncovering
darker land and ocean
surfaces.
According to scientists, the
dark skin is due to the higher level of ultraviolet rays that such people get, which is reflected from the
ice and snow
surface during the summer season, and the vitamin D that they obtain from eating fish and seal.
Asphalt and tarmac is an increased risk in winter because
ice tends to be invisible on the
dark surface.
The water
ice counteracts the traditional danger of living above ground by serving as a radiation barrier, offsetting fears of solar exposure that have, until now, projected Martian architecture into a
dark underworld — buried beneath a regolithic
surface that is believed to contain perchlorates, gypsum and other substances hazardous to human life.Water as a Radiation Shield By taking advantage of water -
ice's ability to filter the sun's rays and protect against radiation,
ICE HOUSE prioritizes a life above ground and celebrates the human presence on the planetary
surface.
This process should accelerate over time, with years - old soot coming to the
surface and making it ever
darker and more heat absorbent, until all the
ice is gone.
Surface melt on the
ice sheet is constrained by the albedo, but a lake is
dark and could absorb much more solar radiation.
For example: 1) plants giving off net CO2 in hot conditions (r / t aborbing)-- see: http://www.climateark.org/articles/reader.asp?linkid=46488 2) plants dying out due to heat & drought & wild fires enhanced by GW (reducing or cutting short their uptake of CO2 & releasing CO2 in the process) 3) ocean methane clathrates melting, giving off methane 4) permafrost melting & giving off methane & CO2 5)
ice & snow melting, uncovering
dark surfaces that absorb more heat 6) the warming slowing the thermohaline ocean conveyor & its up - churning of nutrients — reducing marine plant life & that carbon sink.
Since the
darker ocean
surface absorbs more sunlight than the bright
ice, this warms the region even further.
It is easy to see why this feedback amplifies the climate change, because reduction of
ice sheet size due to warming exposes a
darker surface, which absorbs more sunlight, thus causing more warming.
As the earth's natural air conditioner, white sea
ice moderates solar heating by increasing the reflectivity of Earth's
surface and decreasing the amount of heat that would otherwise by absorbed by
darker ice - free Arctic seas.
Still, they indicate that some areas of the ocean are heating up especially fast, such as the Arctic Ocean — which this year had its lowest winter
ice year on record — and is absorbing much more solar energy as melting
ice cover exposes new
dark surfaces.
From that link's words, the DMI «green line» IS the best way to consistently compare the daily estimate of NORTH areas of the arctic — those areas north of 70 latitude to 83 north latitude NASA - GISS extrapolates «
surface» ground - based temperatures as far as 1200 km from where their land - based measurements were made from 60 - 70 latitude over the ever - greening (and
darker) tundra and forests OUT to the open sea where where the arctic sea
ice actually is present.
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.
On the other hand they melt fast when a rising ocean hits their boundary and turns landlocked
ice directly into
dark ocean
surface with no intermediate state of
ice - free land
surface.
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.
In one of the troubling feedback loops of the changing climate,
dark ice is partially caused by the warmer Arctic summers climate change has brought us: More warmth means less fresh snowfall to cover areas of accumulated sediment, changes to the shape and size of
ice grains that make them less reflective, and more liquid near the
surface.
When melting
ice disappears from the arctic, it exposes more of the ocean's
dark surface, which absorbs the sun's warming rays.
As the planet warms,
ice and snow melt, causing the
surface to be
darker, absorb more sunlight and warm further.
Surface ice algae produce dark pigments to protect themselves from high intensity radiation, further darkening the sheet surface, Stiba
Surface ice algae produce
dark pigments to protect themselves from high intensity radiation, further darkening the sheet
surface, Stiba
surface, Stibal said.
All this melting has begun to expose rock and soils (and ocean in areas where sea
ice has melted), which in turn causes further melting, because
darker surfaces absorb more heat.
As sea -
ice melts, it exposes a much
darker ocean
surface, which absorbs more radiation — amplifying the warming.
To avoid long response times in extreme climates, today's
ice sheets are assigned
surface properties of the tundra, thus allowing them to have a high albedo snow cover in cold climates but
darker vegetation in warm climates.
Amplifying feedbacks include increased absorption of sunlight as melting exposes
darker surfaces and speedup of iceberg discharge as the warming ocean melts
ice shelves that otherwise inhibit
ice flow.
This increases the
surface area of exposed,
dark ocean water, and promotes a self - reinforcing cycle of land and sea
ice melting and climate warming.
As sea
ice melts,
darker ocean water is exposed; the additional energy absorbed by the
darker surface then melts more
ice, setting in motion a self - reinforcing feedback.
When sea
ice melts, the
dark - coloured ocean
surface is exposed.
As the
ice on the
surface of the Arctic Ocean melts away, there is a smaller area of white
ice to reflect the Sun's heat back into space and more open,
dark water to absorb it.
Tedstone's idea could explain why during the warm summers of 2010, 2012, and 2016 the
surface of the
dark ice zone darkened dramatically, whereas in the cooler summer of 2015, the color changed little.
This is because when the Earth warms, snow and
ice melt, uncovering
darker land and ocean
surfaces.
Surface impurities can indeed reduce albedo in the visible part of the electromagnetic spectrum — light with wavelengths from 400 to 700 nanometers — and make snow and
ice appear
darker to our eyes.