There is already strong evidence that anthropogenic forcing has played a significant role in the collapse of ice shelves on the Antarctic Peninsula, cause by significant
melting at the surface during summer.
(Of course, things can certainly sped up if we start getting lots and lots and lots of
melt at the surface all the way to the summit, but we're not there yet (it's still only a few days / year and a few hours / day up there.
Changing this profile — even with major
melting at the surface — will take on order of the characteristic response time, of about 3000 m / 0.25 m / year (height over accumulation rate) = 12,000 years.
Finally, there is another way how ice sheets can contribute to sea level rise: rather than
melting at the surface, they can start to flow more rapidly.
Nearly the entire ice cover of Greenland, from its thin, low - lying coastal edges to its 2 - mile - thick (3.2 - kilometer) center, experienced some degree of
melting at its surface, according to measurements from three independent satellites analyzed by NASA and university scientists.
As ice in Greenland
melts at the surface, water carves fissures and reaches the base, where ice meets land.
According to NOAA's 2012 Arctic Report Card, the duration of
melting at the surface of the ice sheet in summer 2012 was the longest since satellite observations began in 1979, and the total amount of summer melting was nearly double the previous record, set in 2010 (satellite records of melting go back to 1979.)
What is actually happening is that ice is
melting at the surface and forming lakes that drain down into the crevasses.
Scenarios of deglaciation (Meehl et al., 2007 Section 10.7.4.4) assume that any such increase would be outweighed by accelerated discharge of ice following weakening or collapse of an ice shelf due to
melting at its surface or its base (*).
Most of the massive ice sheet that covers roughly four fifths of Greenland
melts at the surface in summer.
This means that a clean snowpack (one with no impurities) that has
melted at the surface can have a lower broadband albedo than a cold snowpack with impurities, despite the fact that the clean snowpack might still appear brighter to our eyes.
Not exact matches
Chilled pie dough plus a lightly floured work
surface will give you the best shot
at rolling out your dough while avoiding a
melted mess.
1)
Melt butter 2) Dissolve sugar in
melted butter 3) Mix sugar butter mixture with self - raising flour until homogenously mixed 4) Knead cookie dough with your hands on a cool, flat
surface, using a rolling pin to flatten it to 0.7 cm thickness 5) Use a round cookie cutter to cut out round pieces 6) Arrange the cookie dough pieces on a greased baking tray 7) Bake
at 200 deg cel for 8 — 10 minutes or until they turn slightly golden brown 8) Spread dulce de leche on one cookie, and cover it with another cookie 9) Coat the sides of the cookie sandwich (the parts where dulce de leche is exposed) with shredded coconut
So, working with one bagel
at a time brush the rounded
surface with some of the
melted butter.
«We can control whether the carbon forms one or two monolayers on the
surface of the material by manipulating the intensity of the laser and the depth of the
melting,» says Jay Narayan, the John C. Fan Distinguished Chair Professor of Materials Science and Engineering
at NC State and senior author of a paper describing the work.
Over the course of time, this may have led to peaks in deep mantle
melting and possibly to major volcanic events
at the Earth's
surface.
«One example of this interfacial slip phenomenon is when the polymer
melts slip
at the mold boundary and causes
surface roughness or cracking,» says Sohdam Jeong of Energy and Chemical Engineering
at UNIST, the first author of the study.
Located approximately 16 to 2,300 feet below the glacier, the five ocean sensors are connected to a weather station
at the
surface, creating the first cabled observatory on a floating, moving, and rapidly
melting Greenland glacier.
At one point, 97 per cent of the sheet's
surface was
melting, leading to floods that washed away bridges.
On Pluto, a slurry of nitrogen and water ice
melted by subsurface heat stands in for lava, the team suggests, freezing solid once it is exposed
at the
surface.
A strong sun will
melt surface snow, which then refreezes
at night into an icy crust, off of which the next layer of snow can easily slip.
«Instead of emerging
at the
surface, much of that heat is
melting the ice shelves,» Hansen says, producing more fresh water and amplifying the feedback.
Untersee is a good model for Mars, he says, because it is supplied by subglacial
melt — water that accumulates
at the bottom of an ice pile — rather than from
surface melting, which does not occur on Mars.
Box pointed to nearly ice - sheet - wide
melting on Greenland, with extensive
surface melting documented for first time
at the highest elevations of ice sheet, and the longest
melt season since satellite observations began in 1979.
David Ullman, a postdoctoral researcher
at Oregon State University and lead author on the study, said there are two mechanisms through which ice sheets diminish — dynamically, from the jettisoning of icebergs
at the fringes, or by a negative «
surface mass balance,» which compares the amount of snow accumulation relative to
melting.
When snow
melts in response to warming, more sunlight can be absorbed
at Earth's
surface because most
surfaces have a lower reflectivity than snow.
The great ice sheets of Greenland and Antarctica, which rise to over 13,000 feet above sea level, accumulate ice over most of their
surfaces and
melt only
at their lower elevations near the edges.
This represents the stage
at which the planet's solid rocky core begins to
melt, creating a molten material that sloshes around in Mercury's mantle before erupting onto the
surface.
The first is «sintering,» a process similar to
melting, in which the Teflon is heated
at a very high temperature and pressed firmly onto a
surface.
Volcanologists
at the University have discovered that a process called frictional
melting plays a role in determining how a volcano will erupt, by dictating how fast magma can ascend to the
surface, and how much resistance it faces en - route.
That's because the IPCC models only take into account temperature changes
at the
surface of glaciers, but not the rapid
melting that occurs when glaciers calve and break up into the ocean, Rignot said.
Kattenhorn and Prockter saw ice volcanoes on the overriding plate, possibly formed through
melting and absorption of the slab as it dove below the
surface, and a lack of mountains
at the subduction zone, implying material was pushed into the interior rather than crumpled up as the two plates mashed against each other.
However, ice is a poor conductor so, unless ice is very thin or the geothermal heat flux very high, tends not to influence
melt at the ice
surface.
However, it's quite a different matter
melting a long - lived massive ice sheet up to 1.5 km thick that covers over 70 % of the land
surface (as happened
at the end of the last glacial period), from
melting isolated and much thinner ice caps / sheets that only cover about 11 % of the land
surface (i.e. present - day).»
«The DIC lakes are situated within bedrock troughs in mountainous terrain, exist
at temperatures well below the pressure -
melting point, do not receive
surface meltwater input, and likely consist of hypersaline water derived from dissolution of a surrounding salt - bearing geological formation,» the researchers reported.
In 2015, a team led by the University of Michigan's Sharon Glotzer used high - performance computing
at the Department of Energy's (DOE's) Oak Ridge National Laboratory [ORNL] to study
melting in two - dimensional (2 - D) systems, a problem that could yield insights into
surface interactions in materials important to technologies like solar panels, as well as into the mechanism behind three - dimensional
melting.
Zircons in rocks
at the
surface of the planet would not likely have survived in the vast
melt sheets.
Unlike the great ice sheet of Antarctica, the Greenland ice sheet is
melting both on its
surface and also
at outlet glaciers that drain the ice sheet's mass through deep fjords, where these glaciers extend out into the ocean and often terminate in dynamic calving fronts, giving up gigaton - sized icebergs
at times.
As Arctic temperatures rise
at about double the rate of the planet as a whole, Greenland's
surface has been
melting at a steady clip, contributing about 30 percent of the foot of global sea level rise since 1900.
One year without a net loss also doesn't buck the long - term trend of Greenland losing ice, both from
surface melt and from ocean waters eating away
at glaciers that flow out to sea.
During the first burn keep your candle lit for
at least 2.5 hours and preferable until the entire
surface has
melted.
Because it has less
surface area than individual cubes, it will
melt at a much slower pace.
Personages of sorts, they are crown - wearing, multi-scoop stacked cones, often inhabited by sleepy shrine groupies that hold to disconnected phone receivers or lick
at melting, sugary
surfaces.
But
at the same time, every discrete element appears to be
melting in paint drips down the
surface.
Collar's exhibitions and performances include: A rock that keeps tigers away, group exhibition, Kunstverein München, Munich, July 2017; a performance event and micro residency, Kunstraum, London, June 2017; Plural
Melts at Yvonne Lambert, Berlin, 2017; Tall Tales, touring group exhibition and performance, Freud Museum, London, Touchstones Gallery and Museum, Rochdale and Glasgow Women's Library 2016; Tarantallegra, group exhibition, Hester, New York, July - Aug 2016; Secret
Surface, group exhibition, KW, Berlin, Feb - May 2016; 11/50, solo exhibition, Fig - 2, ICA, London, March 2015; Probably, Like a Melon Rolling Off a Table: Part II, solo performance for Saturday Live, Serpentine Galleries, London, Jan 2015; Secret Agents, group exhibition, Finnish Museum of Photography, Helsinki, Sept - Oct 2015; PALIMPSEST, performance collaboration with William Cobbing
at Hayward Gallery Project Space, London, 2014; Let's Make Another Possible Now, group performance event as part of ANTIKNOW
at Flat Time House, London, 2014.
Richard B. Alley, an expert on Greenland's ice sheet
at Penn State, told me it's still possible that flows of meltwater from
surface lakes could start large areas of ice moving seaward, particularly if the
melt zones continue to expand inland as they have been doing for years now.
The physical processes by which energy might be added into the glacier material include: (A) convection between the glacier
surfaces and local surrounding atmosphere and water, (B) direct radiation onto the exposed
surfaces of the material, (C) addition of material that is
at a temperature higher than the
melting temperature onto the top of the glacier (rain, say), (D) Sublimation of the ice directly into the atmosphere, and (E) conduction into the material from the contact areas between the glacier and surrounding solid material.
Winter snow tends to accumulate in the crevasses and gullies, so that
at the end of winter there is already ice
at the
surface — so the
melt season very close to the margin is very long.
BTW, my fearless «denialism forecast» for the next month is for declining mentions of
surface temperature trends, 30 - 50 % chance of more scientist bashing, and sporadic outbreaks of «Arctic sea ice recovery» —
at least until the
melting season gathers some steam.
The point about heating (adding energy) vs warming (temperatures going up) is a very good one — it might help if the scientists involved with the major temperature series people look
at (GISS, RSS, etc) also produced a global
surface energy change index that accounted for things like
melting ice, which absorb heat without raising temperatures.