A massive ice sheet almost completely covers Greenland, and as summertime temperatures climb and sunlight hours lengthen,
parts of the ice sheet surface usually melt, especially at lower elevations near the coast.
Not exact matches
1) Mix flour, butter and
icing sugar in a bowl using two knives to cut the butter until the mixture resembles fine breadcrumbs 2) Add in the egg yolks and vanilla extracts and mix well, then add
iced water until the dough starts to come together 3) Shape the dough into a ball on a cool, flat, floured
surface 4) Flatten dough into a disc and then wrap in plastic wrap, and chill in the refrigerator for at least 30 minutes 5) Meanwhile, peel, core and slice the apples into as thin slices as possible 6) Mix sugar and ground cinnamon powder with sliced apples and let it rest for a while 7) Pre-heat oven to 180 deg cel 8) Once dough has chilled, roll pastry dough on a
sheet of parchment paper until it has expanded to the size
of the tart mold (I used a rough mold the size
of a large pizza) 9) Leaving at least an inch
of dough free, arrange apple slices by overlapping them slightly in the shape
of a circle, starting from the outermost
part of the circle, until you reach the inside 10) Fold the edges
of dough over the filling and then sprinkle the dough with a bit
of sugar 11) Bake for about 40 - 45 minutes, or until the crust is golden brown and the apples are soft 12) Serve warm, with a side
of whipped cream or
ice cream (optional)
Water that collects in valleys underneath the
ice sheet, in the Gamburtsev Mountains, refreezes when it passes under thinner
parts of the
ice sheet that are less insulated from cool
surface temperatures.
«The beds at the margins
of the
ice sheet... are probably one
of the least explored
parts of Earth's
surface,» said Ian Howat, a glaciologist at Ohio State University who did not participate in the research.
... Polar amplification explains in
part why Greenland
Ice Sheet and the West Antarctic
Ice Sheet appear to be highly sensitive to relatively small increases in CO2 concentration and global mean temperature... Polar amplification occurs if the magnitude
of zonally averaged
surface temperature change at high latitudes exceeds the globally averaged temperature change, in response to climate forcings and on time scales greater than the annual cycle.
Other factors would include: — albedo shifts (both from
ice > water, and from increased biological activity, and from edge melt revealing more land, and from more old dust coming to the
surface...); — direct effect
of CO2 on
ice (the former weakens the latter); — increasing, and increasingly warm, rain fall on
ice; — «stuck» weather systems bringing more and more warm tropical air ever further toward the poles; — melting
of sea
ice shelf increasing mobility
of glaciers; — sea water getting under
parts of the
ice sheets where the base is below sea level; — melt water lubricating the
ice sheet base; — changes in ocean currents -LRB-?)
Huge
sheets of ice (glaciers) cover large
parts of the Earth's
surface.
Second, and less important but still rather spectacular, was the melting
of virtually every square inch
of the
surface of this
ice sheet over a short period
of a few days during the hottest
part of the summer, a phenomenon observed every few hundred years but nevertheless an ominous event considering that it happened just as the aforementioned record
ice mass loss was being observed and measured.
The base is currently buried about 35 meters below the
surface but the
part of the
ice sheet that covers the camp may start to melt by the end
of the century if current warming trends continue, scientists warned.
The remaining amount is coming from increased
surface melting, which is no longer confined to the southern
part of the
ice sheet — the amount
of ice accumulating in the inland
part of the
ice sheet is starting to decline as well.