Not exact matches
These bars can be served chilled or warm with a big scoop of
ice cream if desired.You can
change to various fruits
during the summer time, like cherries, any type of berries and recreate this amazing dessert with various flavors.
Rule 74 — Too Many Men on the
Ice 74.1 Too Many Men on the Ice — Players may be changed at any time during the play from the players» bench provided that the player or players leaving the ice shall be within five feet (5») of his players» bench and out of the play before the change is ma
Ice 74.1 Too Many Men on the
Ice — Players may be changed at any time during the play from the players» bench provided that the player or players leaving the ice shall be within five feet (5») of his players» bench and out of the play before the change is ma
Ice — Players may be
changed at any time
during the play from the players» bench provided that the player or players leaving the
ice shall be within five feet (5») of his players» bench and out of the play before the change is ma
ice shall be within five feet (5») of his players» bench and out of the play before the
change is made.
However, at least half the decline in Alpine
ice during the past 150 years is «certainly due to human - induced climate
change,» he says.
Scientists may also become able to distinguish between different scenarios sooner by studying the physics of local
ice - sheet
changes and refining reconstructions of
changes during warm periods in geological history.
But
during the Little
Ice Age, a period from roughly 1400 to 1850 when temperatures in Europe were cooler and many of Earth's glaciers expanded, the biggest
changes came from the Intertropical Convergence Zone shifting to the south.
But when average temperatures rise, as is happening in many places around the world because of climate
change, big blocks of
ice melt more quickly than they can grow
during the winter.
Their field - based data also suggest that
during major climate cool - downs in the past several million years, the
ice sheet expanded into previously
ice - free areas, «showing that the
ice sheet in East Greenland responds to and tracks global climate
change,» Bierman says.
For example, the
ice ages
during the last several million years — and the warmer periods in between — appear to have been triggered by no more than a different seasonal and latitudinal distribution of the solar energy absorbed by the Earth, not by a
change in output from the sun.
Climate
change and the resulting loss of sea
ice during the summer have opened new hunting territory for the killer whales in the eastern Canadian Arctic, but scientists knew very little about these animals until they tapped into the traditional knowledge of Inuit hunters who shared unique firsthand descriptions of orca hunting tactics.
These data were used to quantify
changes in the
ice cover's composition, revealing a substantial reduction of about 14 percent in the area of multiyear
ice in winter
during the period from 1978 to 1998.
Interior Secretary Dirk Kempthorne, however, made clear several times
during a press conference announcing the department's decision that, despite his acknowledgement that the polar bear's sea
ice habitat is melting due to global warming, the ESA will not be used as a tool for trying to regulate the greenhouse gas emissions blamed for creating climate
change.
Projects funded
during the 2007 - 2008 International Polar Year, for example, documented different Arctic native populations» rich vocabulary for different types of sea
ice and plumbed the communities» observation of
changing caribou behavior.
Erosion has also increased
during winter; shrinking lake
ice — a product of climate
change — does not protect the dune from winter winds as it has in the past.
«Detailed chemical measurements in Antarctic
ice cores show that massive, halogen - rich eruptions from the West Antarctic Mt. Takahe volcano coincided exactly with the onset of the most rapid, widespread climate
change in the Southern Hemisphere
during the end of the last
ice age and the start of increasing global greenhouse gas concentrations,» according to McConnell, who leads DRI's ultra-trace chemical
ice core analytical laboratory.
Remarkably, they found that the decrease in the mass of
ice during this period was mirrored in GOCE's measurements, even though the mission was not designed to detect
changes over time.
During the first two - thirds of the Quaternary, the
ice advanced and retreated roughly every 41,000 years — the same tempo as the
changes in the tilt of Earth's axis.
Guliya is thought to be the best record of midlatitude climate
during the last
ice age, and its
ice may well turn out to be a Rosetta Stone for interpreting how Asia responds to a
changing climate.
Both tree species have seen many climate
changes during their time on Earth — from extremely warm periods to
ice ages — and have slowly advanced across the landscape.
Scientists believe they have discovered the reason behind mysterious
changes to the climate that saw temperatures fluctuate by up to 15 °C within just a few decades
during the
ice age periods.
«Counterintuitively, rapid climate
changes during the
ice age were, at times, highly beneficial for megafauna when rapid warming allowed grasses and forbs to briefly spread before peatlands had a chance to take over the landscape and degrade forage quality,» said Groves.
The
ice reconstruction in this study provides a fascinating image of a
changing Europe
during the time prehistoric humans came to populate the continent.
New research shows that small fluctuations in the sizes of
ice sheets
during the last
ice age were enough to trigger abrupt climate
change.
The spectacular
ice cave at Scărișoara fills a crucial piece of the puzzle of past climate
change in recording what happens
during winter.»
However, the simulations indicate that the sea -
ice driven precipitation
changes resemble the global rainfall patterns observed
during that drought, leaving the possibility that Arctic sea -
ice loss could have played a role in the recent drought.
The preconditions which gave rise to rapid temperature
changes during the last
ice age do not exist today, but sudden climate
changes can not be excluded in future.»
The study, by an international team of scientists led by the University of Cambridge, examined how
changes in ocean currents in the Atlantic Ocean were related to climate conditions in the northern hemisphere
during the last
ice age, by examining data from
ice cores and fossilised plankton shells.
During the later period, when there was less sea
ice, the whales dove significantly longer and deeper than in the earlier period — presumably in search of prey as the animals, in turn,
changed their habits because of different ocean conditions brought on by sea
ice loss.
Professor Richard Pancost from the University of Bristol Cabot Institute, added: «When we account for the influence of the
ice sheets, we confirm that the Earth's climate
changed with a similar sensitivity to overall forcing
during both warmer and colder climates.»
An examination of these
changes gave them new insights into how much of the polar
ice cap's carbon dioxide freezes out of the atmosphere
during winter.
Precise interpolar phasing of abrupt climate
change during the last
ice age, Nature, 520, 661 - 665, doi: 10.1038 / nature14401.
The Marguerite Bay drainage basin, in contrast, would have been of the order of 10,000 to 100,000 km2
during the LGM, and the
ice streams draining this basin would have responded more rapidly to
changes in external forcing [47].
It is likely, therefore, that charr were able to detect subtle
changes in subsurface light - levels, even
during the polar night and under
ice.
While natural global warming
during the
ice ages was initiated by increased solar radiation caused by cyclic
changes to Earth's orbital parameters, there is no evident mechanism for correcting Anthropogenic Global Warming over the next several centuries.
While a 14 % loss is not an insignificant amount, it's smaller than some of the
changes in Antarctic sea
ice recorded
during the middle of the 20th century, as estimated from whaling ship logbooks, the paper says.
Consequences of
change and variability in sea
ice on marine ecosystem and biogeochemical processes
during the 2007 — 2008 Canadian International Polar Year program.
And through detailed studies of the local physics of
ice - sheet
changes and more refined reconstructions of
ice - sheet
changes during warm periods of the geological past, scientists may become able to distinguish between the two roads sooner.
Huybrechts, P., 2002: Sea - level
changes at the LGM from
ice - dynamics reconstructions of the Greenland and Antarctic
ice sheets
during the glacial cycles.
One study, published in Proceedings of the National Academy of Sciences in January, hinted at such a mechanism when it linked sea
ice decline to apparent
changes in the Arctic Oscillation
during several winters preceded by large sea
ice losses.
Going off these calculations, how much ppm
change during the
ice cycles?
During the fall, the heat that was added to the oceans gets released into the atmosphere as sea
ice reforms, and this added heat is bound to
change weather patterns somehow (this is a process known as «Arctic Amplification»).
So what is the time difference between CO2 levels
during the onset of a cooling period at the end of a warming period and the time history of the temperature
changes in the
ice cores?
That estimate was based in part on the fact that sea level is now rising 3.2 mm / yr (3.2 m / millennium)[57], an order of magnitude faster than the rate
during the prior several thousand years, with rapid
change of
ice sheet mass balance over the past few decades [23] and Greenland and Antarctica now losing mass at accelerating rates [23]--[24].
Precise interpolar phasing of abrupt climate
change during the last
ice age.
More recent studies, with much more precise correlation between
ice cores and global temperature records, have shown that temperature and CO2
changed synchronously in Antarctica
during the end of the last
ice age, and globally CO2 rose slightly before global temperatures.
During periods when
ice sheets have been relatively stable, such as the last several millennia (the late Holocene), sub-millennial sea - level variability arose primarily from
changes in atmosphere / ocean dynamics.
Acidity decline in Antarctic
ice cores during the Little Ice Age linked to changes in atmospheric nitrate and sea salt concentratio
ice cores
during the Little
Ice Age linked to changes in atmospheric nitrate and sea salt concentratio
Ice Age linked to
changes in atmospheric nitrate and sea salt concentrations.
The
ice sheet's thickness makes its temperature much more resistant to
change than the six inches of snow that might fall on your driveway
during a winter snowstorm.
It's possible that both animals entered the Atlantic via the Northwest Passage, which has been partially free of
ice for brief periods
during the past four years — a phenomenon attributed to climate
change.
This talk by Cleveland Art Museum Assistant Curator of Korean Art Sooa Im McCormick explores how climate
changes during the Little
Ice Age prompted eighteenth - century Korean rulers to exercise the politics of frugality, and eventually shaped eighteenth - century Korean visual culture and its distinctive aesthetics.
Olafur Eliasson is preparing his glacier,
ice installation, Ice Watch, which is to be placed in the Place de la République, in Paris, to highlight Climate Change during the COP
ice installation,
Ice Watch, which is to be placed in the Place de la République, in Paris, to highlight Climate Change during the COP
Ice Watch, which is to be placed in the Place de la République, in Paris, to highlight Climate
Change during the COP21.