Sentences with phrase «warmer ice layers»

Researchers were surprised to find a 7,700 - square - mile piece (about the size of Wales) missing, but they theorized that it had moved over warmer ice layers until it collided with another plate and was forced beneath the surface, out of view.

Not exact matches

I roast chicken backs and parts or use leftover chicken or turkey bones then use a electric instapot style pressure cooker set on chicken / high temp for an hour then let it naturally depressurize let cool then refrigerate overnight take the grease layer off following day as it will congel on top its easy to remove then warm it back up to liquify and put it into ice cube trays mix 17 ice cubes (1 cup) too 1 or 2 cups water depending on strength you want the best stock on earth

Increased atmospheric heat obviously makes temperatures warmer, which leaves less time for ice to form and solidify and create new layers on glaciers and ice sheets.

While the mashed potatoes are still warm, ice the first layer.

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The sun shines warmer this week, evidenced by puddles that have replaced layers of ice pack and the softening -LSB-...]

When I used to make the traditional version of these, I always rolled in powdered sugar while still warm and then dusted again when cool to get that gooey melty layer that turns to a sort of icing.

There's good old fashioned Warm Chocolate Cake ($ 11.5) with vanilla bean ice cream and raspberry sauce but, for a true New York experience, go for my personal favorite: the six - layer Lemon Dodger Cake ($ 12.50) with lemon buttercream icing and lemon glaze.

Horchata, traditional Mexican iced sweetened rice drink, is given a twist and mixed with the warming spices and assam black tea of traditional Indian masala chai tea to create the sweet, layered horchaita.

Under certain conditions, the warm water of the lower layer can reach the surface and melt the ice.

If sunlight must penetrate the dust covering a comet's water ice in order to warm it and produce jets, Sunshine says the Deep Impact findings suggest the ices on such dormant comets may not have run out but merely become sealed — by layers of debris, for example.

Bacteria and diatoms inhabit those liquid veins, and Hajo Eicken, a glaciologist at the University of Alaska at Fairbanks, suspects that similar habitats could exist in the lower, warmer layers of ice on Europa, and perhaps on the other moons as well.

Frigid Europa may be warmed by a layer under its crust that moves heat and ice to and from its poles — and alien microbes could be hitching a ride

Beneath an ice layer about 10 to 15 miles (15 - 25 kilometers) thick, the moon is thought to harbor a liquid water ocean, possibly warmed by geologic processes originating in the planet's core.

There's evidence, Johnson says, that Europa's ice shell has a two layers: a thin outer lid of very cold ice that sits atop a layer of slightly warmer, convecting ice.

He proposed that the bottom layers of Europa's ice shell would be slightly warmer than the ice on top, due to heating from both the ocean below and the crushing pressure of the miles - thick ice above.

If the heat is weaker (right), Europa might have a thick layer of warm ice atop its ocean.

The ice shelf floats within a pool of its own cold meltwater that sits atop a deeper, saltier and warmer layer; the two layers generally don't mix, like oil and water.

The areas that appeared bright in the radio images but dark in the laser observations correspond to warmer patches on Mercury, where ice would be stable only if buried under a 10 - centimetre - thick layer of other material.

At one time the Arctic Ocean was covered with substantially more ice and experienced very little mixing of warm and cool layers of water.

Raymond says this could be due to a combination of two effects: small landslides revealing ice previously hidden beneath a layer of dust, and ice in areas that aren't usually sunlit being warmed enough to turn into water vapour.

That means it sinks into the deeper layers of the ocean, and the contrast between this warm water and the undersea ice canyons contributes an unknown but substantial amount of sea level rise, said Josh Willis, an oceanographer at JPL in Pasadena, California.

In fact, Natural Resources Canada has a collection of ice cores that contain layers deposited up to 8,000 years ago — a time when the earth was far warmer than today.

This warm air layer gets its heat reflected downwards during cloudy periods, especially during long night extensive cloudy periods, as a result, Arctic ocean ice doesn't thicken so much during darkness and leaves it up to summer sunlight (if there is some) to finish off what is left of it.

Those people in New England and D / FW who are shivering now are experiencing cold * weather * (although note it was an ice storm, not a snow storn, which means there was a warm layer aloft).

Bacteria, however, have remained Earth's most successful form of life — found miles deep below as well as within and on surface rock, within and beneath the oceans and polar ice, floating in the air, and within as well as on Homo sapiens sapiens; and some Arctic thermophiles apparently even have life - cycle hibernation periods of up to a 100 million years while waiting for warmer conditions underneath increasing layers of sea sediments (Lewis Dartnell, New Scientist, September 20, 2010; and Hubert et al, 2010).

«The reason for the layering is that global warming in parts of Antarctica is causing land - based ice to melt, adding massive amounts of freshwater to the ocean surface,» said ARC Centre of Excellence for Climate System Science researcher Prof Matthew England an author of the paper.

The research published in Nature Communications found that in the past, when ocean temperatures around Antarctica became more layered - with a warm layer of water below a cold surface layer - ice sheets and glaciers melted much faster than when the cool and warm layers mixed more easily.

Thankfully my layers and giant scarf helped keep me warm, otherwise I would have turned into an ice sculpture on the spot!

If you go in winter, take boots with grips for the ice and layers of light, warm clothing.

This warm air layer gets its heat reflected downwards during cloudy periods, especially during long night extensive cloudy periods, as a result, Arctic ocean ice doesn't thicken so much during darkness and leaves it up to summer sunlight (if there is some) to finish off what is left of it.

I have observed greater variations in Arctic Inversions lately, the tendency is towards less steep inversions, this is expected when the Arctic lower atmosphere warms during winter, if the models maintain a stronger inversion while its observed weakening this may explain why sea ice models fail, strong boundary layers appear to be collapsing.

There is of course a lot of uncertainty about the details, that affect the melt rates, we just don't know how quickly warmer seawater will undercut floating glaciers, and buildup of darker older snow / ice layers will increase the amount of absorbed sun light.

As a result, while a layer of ice - cold fresh water sits just beneath the sea ice, about 20 meters (65 feet) down there is a layer of denser, saltier water that has been gradually warmed by the sun's rays.

'» This argument cuts both ways: The media could point out that ice storms are the result of a warm front overriding a thin layer of colder surface air.

Lower Atmosphere is warming, oceans upper layers are warming, arctic summer sea ice is disappearing, WAIS and Greenland are both losing mass annually and the majority of the earths glaciers are losing mass too.

We have fairly high confidence that we observe the history of Heinrich events (huge discharges of ice - rafted debris from the Laurentide ice sheet through Hudson Bay that are roughly coincident with large southern warming, southward shift of the intertropical convergence zone, extensive sea ice in the north Atlantic, reduced monsoonal rainfall in at least some parts of Asia, and other changes), and also cold phases of the Dansgaard / Oeschger oscillations that lack Heinrich layers and are characterized by muted versions of the other climate anomalies I just mentioned.

[BTW, it's possible that it was NOT warm when the ice man died... maybe he even died from the cold & there was ice and snow on the ground then... and then layers of snow and ice piled on top of him.]

If continental ice melting (Greenland, Antarctic, terrestrial glaciers) is accelerating and if warming of the 0 - 700 m (and deeper) oceanic layer is still on, you shoud observe a higher rate of sea - level rise.

I suppose that for a 3,7 W / m2 forcing, the additional energy of forcing + feedbacks is used for faster processes (melting ice, evaporation, warming of subsurface oceanic layers, etc.) and the new equilibrium is reach on a quite short timescale.

The resulting weaker density stratification allowed more vertical mixing of the water column during storms in late September and early October, leading to the observed warming of the near - bottom layer in the still ice - free Laptev Sea... Warmer water temperatures near the seabed may also impact the stability of the shelf's submarine permafrost.»

Close to the surface of the bedrock, the lowest layers of the ice are warmed by the heat of the Earth.

The scientists were particularly interested in crystals found in layers deposited during the «Little Ice Age,» approximately 300 to 500 years ago, and during the «Medieval Warm Period,» approximately 500 to 1,000 years ago.

Although the sea ice layer is more massive than the atmosphere, the clouds persist long enough in each storm episode to affect heat conduction through the snow and noticeably warm the sea ice while they are present.

«We can see that the red layers of the ocean floor is formed during the Ice Age's warm periods, and that proves that every time the temperature rose, water from the melting ice was poured into the ocean», says RasmussIce Age's warm periods, and that proves that every time the temperature rose, water from the melting ice was poured into the ocean», says Rasmussice was poured into the ocean», says Rasmussen.

The high reflectivity of this new planetary layer, the Lucrosphere, will radically incease our planet's albedo, and so compensate for the loss of reflective Arctic sea ice that threatens to accelerate global warming.

The Arctic is warming twice as fast as the rest of the planet, for reasons that may include its layered atmosphere, which traps heat, and the loss of sea ice and snow cover, which when present help reflect the sun's energy.

The climate models have gotten more complex, for sure, with thousands of estimated parameters for warming potential, vorticity, circulation patterns, absorption of heat, pressure, energy, and momentum by various layers or atmosphere, land, ocean, and sea - ice.

Nelson's Bay Cave, a deep cave somewhat above the high - water line which we explored several days ago, has layers from the last ice age and into our present warm period; their tools included projectile weapons, and, judging from the bones they discarded, they had gotten good at bringing home the bacon and dealing with the ill - tempered Cape buffs, among the most dangerous animals in Africa.

Causes in the real world tend to come in layers, and there is an underlying 1,500 - year cycle in North Atlantic ice rafting that goes back 100,000 years, in both our warm period and the antecedent ice age.