Not exact matches
Lay them on a baking
sheet and drizzle
melted coconut oil
over them.
Spoon the meat mixture
over the cheese and place baking
sheet in the oven to bake 5 - 6 minutes or until cheese
melts.
When eaten warm, and I mean, straight off the baking
sheet, the chocolate is still all
melted and just oozing
over the cookie dough.
I was met with cookies that spread ALL
OVER the baking
sheet, cookies that didn't spread at all, cookies that looked perfect but had the texture of crumbly cake, and cookies that seemed to
melt into something that tasted like sand after taking a bite.
Apply
melted butter all
over the thin rolled
sheet.
Pastry chefs routinely spread
melted chocolate
over sheet pans, wait until the chocolate is set to the exact right consistency, and then use a metal spatula (and considerable sleight of hand) to scrape up ruffles and ribbons and all kinds of extravagant shapes.
After fooling around in the kitchen for a while, I spread a thin coat of
melted chocolate, paper thin, on a
sheet of wax paper, smoothed a second
sheet of wax paper
over the chocolate, then rolled the whole thing up into a tight roll and slipped it into the fridge.
1) Pre-heat oven to 300 deg Fahrenheit (150 deg cel) 2) Line one large baking
sheet (0r two medium baking
sheets) with parchment paper 3) In a large bowl, combine the oats, chia seeds, flax seeds, raisins, almonds and other nuts, and mix well 4) In a smaller bowl, whisk together the honey, light brown sugar,
melted butter and cinnamon until smooth and sugar has dissolved 5) Pour the honey mixture
over the dry ingredients and stir well until you get a homogeneous mixture 6) Pour the mixture
over the baking
sheets and spread evenly with a spatula, then season lightly with sea salt 7) Bake for 15 minutes, then stir the granola gently (to make sure all sides are cooked) 8) At this point, you may need to switch the baking
sheets (if you are using 2) so the granola cooks evenly 9) Bake for another 15 minutes, then stir again, before cooking for a final 15 minutes or until golden brown 10) Remove granola from the oven and place on cooking racks until completely cool and crisp 11) Store granola in air - tight containers at room temperature.
We like whole slices of provolone for the topping — the way it
melts over the top in «
sheets» is rather yummy — but shredded would work brilliantly also.
Remove the top
sheet of parchment paper and pour the
melted chocolate
over the rolled out dough.
10) Place the circle of pizza dough (on the parchment paper) on top of a pizza pan or round baking
sheet, and bake for at least 15 to 20 minutes until golden brown and crispy 11) Once crispy, remove pizza crust from oven and spread tomato sauce
over, top generously with the caramelized onions and shredded chicken and sprinkle with mozzarella cheese 12) Return pizza to the oven to heat up for 5 minutes and for cheese to
melt 13) Once cheese is
melted, sprinkle fresh parsley on top of the pizza, cut and serve.
Make each packet by laying 1
sheet of filo on work surface and brush with
melted butter, (Keep remaining filo covered with plastic wrap and a damp towel
over the plastic to prevent drying out).
Over hundreds or thousands of years, vast ice
sheets can
melt away, further decreasing the planet's reflectivity.
It's known that when ice
sheets start to
melt, cooling the air in that region, the winds
over the Southern Ocean strengthen, Toggweiler says.
With longer
melting seasons
over the past few years, the algae have more time to bloom and darken the
sheet, Tranter says.
Scientists have a pretty good idea of how thermal expansion and
melting mountain glaciers will play out
over the long term, but when it comes to the ice
sheets, «we have no idea,» Willis says.
Pettersen is hopeful that, with more data analysis
over longer periods of time, researchers will find more answers yet to account for the
melting ice
sheet and the subsequent sea level rise that has already had an impact on regions across the planet.
The slipperiness, caused by films of water spread
over large areas, helps ascertain how quickly a
melting ice
sheet will slide into the sea as the climate warms — and thus how quickly sea levels will rise.
A new study led by the University of Texas Institute for Geophysics has found that wind
over the ocean off the coast of East Antarctica causes warm, deep waters to upwell, circulate under Totten Ice Shelf, and
melt the fringes of the East Antarctic ice
sheet from below.
«Warming greater than 2 degrees Celsius above 19th - century levels is projected to be disruptive, reducing global agricultural productivity, causing widespread loss of biodiversity and — if sustained
over centuries —
melting much of the Greenland ice
sheet with ensuing rise in sea levels of several meters,» the AGU declares in its first statement in four years on «Human Impacts on Climate.»
«Sea - level rise could nearly double
over earlier estimates in next 100 years: Researchers model effects of
melting Antarctic ice
sheets.»
Totten Glacier, the largest glacier in East Antarctica, is being
melted from below by warm water that reaches the ice when winds
over the ocean are strong — a cause for concern because the glacier holds more than 11 feet of sea level rise and acts as a plug that helps lock in the ice of the East Antarctic Ice
Sheet.
On a clear day, anyone flying
over Greenland on the route between North America and Europe can look down and see the bright blue patches of
melted water atop the flat, blindingly white expanse of the ice
sheet that covers the island, the second largest chunk of ice on Earth.
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.
Contrary to what you might expect, the third IPPC report predicted that global warming would most likely lead to a thickening of the ice
sheet over the next century, with increased snowfall compensating for any
melting cause by warming.
The ice
sheet is made up of annual layers of snow that never
melted and became compacted into ice
over thousands of years.
A relatively small amount of
melting over a few decades, the authors say, will inexorably lead to the destabilization of the entire ice
sheet and the rise of global sea levels by as much as 3 meters.
A new review analyzing three decades of research on the historic effects of
melting polar ice
sheets found that global sea levels have risen at least six meters, or about 20 feet, above present levels on multiple occasions
over the past three million years.
A new study by scientists at NASA's Jet Propulsion Laboratory (JPL) in Pasadena, California, and the University of California, Irvine, shows that while ice
sheets and glaciers continue to
melt, changes in weather and climate
over the past decade have caused Earth's continents to soak up and store an extra 3.2 trillion tons of water in soils, lakes and underground aquifers, temporarily slowing the rate of sea level rise by about 20 percent.
These findings suggest that Greenland's glaciers have been experiencing increasing ice loss for at least three decades — a result that may reinforce scientists» concerns
over the stability of the
melting ice
sheet.
«This makes future projections extremely challenging — anything from 10 centimeters to
over a meter is currently on the table for sea - level rise due to
melting ice
sheets,» Landerer said in an email.
Wiens is careful not to get out in front of the data, but he does say that
over a long period of time, there is a danger the West Antarctic ice
sheet will
melt.
Scientists Sound Alarm
Over Melting Antarctic Ice
Sheets by Steve Connor, Science Editor in San Francisco February 16, 2007 The lndependent / UK
Peter send the chapters on ice
sheets and
melting my way and I will go
over them promptly.
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).»
Either the glaciers would have to flow into the ocean at unrealistic rates, or rapid
melting would have to be triggered
over a much larger area of the ice
sheet than current evidence suggests.
When projecting how sea levels could rise
over the coming centuries, one of the most difficult factors for scientists to gauge is how much of the Earth's vast ice
sheets will
melt, and how quickly.
Combined with
melting from mountain glaciers and the Greenland Ice
Sheet, this could result in flooding of low - lying areas of Earth
over the next century.
But in July 2012, a combination of soot from fires in Siberia coupled with warm temperatures caused a record - setting 95 percent of the ice
sheet to
melt over the course of a week.
«Climate models show that ice -
sheet melt will dominate sea - level rise
over the coming centuries, but our understanding of ice -
sheet variations before the last interglacial 125,000 years ago remains fragmentary.
Researchers attributed the surprising early
melt this year to weather conditions, and more specifically, a warm midlatitude air mass getting stuck
over the ice
sheet.
The cookies
melted and ran off the cookie
sheet all
over the oven!
[Response: Here's a simple back - of - envelope consideration for the future: if the Greenland ice
sheet melts completely
over the next ~ 1,000 years (Jim Hansen argues in the current Climatic Change that the time scale could be centuries), this would contribute an average flux of ~ 0.1 Sv of freshwater to the surrounding ocean.
«As the ice
sheet in Greenland
melts over thousands of years and becomes lower, the temperature will increase because of the elevation loss.
Extent of surface
melt over Greenland's ice
sheet on July 8, 2012 (left), and July 12, 2012 (right).
(1) One is the ice
sheet and glacier mechanical collapse, which doesn't require a whole lot more warming, but will happen with some set minimum amount of warming
over some time period; and (2) the other is global warming that keeps increasing beyond the level needed to cause # 1, which among other things will perhaps lead to positive carbon feedbacks (e.g., from
melting permafrost and hydrates).
In one projected event, large parts of the ice
sheet melt and drain into the ocean
over the next millennia, raising global sea levels by several tens of meters.
Wilson (1964); Wilson (1966); Wilson (1969); Wilson's starting - point was the suggestion that the center of Antarctica was at the pressure
melting point, see Robin (1962), p. 141, who adds that «one would not expect the ice to surge
over a large part of Antarctica at one time»; the role of frictional heat in ice -
sheet instability was pointed out back in 1961 (in partial support of Ewing - Donn theory), drawing on earlier work by G. Bodvarsson, by Weertman (1961).
In May 2007, a team of scientists from NASA and the University of Colorado reported satellite data showing widespread snow -
melt on the interior of the Antarctic ice
sheet over an area the size of California.
Totten Glacier, the largest glacier in East Antarctica, is being
melted from below by warm water that reaches the ice when winds
over the ocean are strong — a cause for concern because the glacier holds more than 11 feet of sea level rise and acts as a plug that helps lock in the ice of the East Antarctic Ice
Sheet.