Much of the Bearded Seal's habitat encompasses seasonal
ice zones where first - year sea ice is renewed every winter but melts completely every summer.
Not exact matches
Every doctor who's ever examined you puts that
ice - cold stethoscope on your triangle of auscultation, a quiet
zone in between three major muscles near the base of your shoulder blade,
where it's easier to hear your lungs.
This isolated cavity of seawater, down at the grounding
zone, sits deep beneath the back corner of the
ice shelf — 850 kilometers back from
where the edge of the
ice meets the open sea.
The crack remained dormant for decades, stuck in a section of the
ice shelf called a suture
zone, an area
where glaciers flowing into the
ice shelf come together.
The grounding
zone —
where the
ice lifts off the muddy bottom of what would be the Antarctic shoreline if there were no
ice, and begins to float on the ocean — serves as a brake, controlling the speed of the glaciers feeding into it.
It could scan Mars and map out subsurface pockets of water
ice and even assist in X-marking a safe and sound landing
zone for astronauts
where they can draw on water for oxygen - sustaining needs as well as for concocting rocket fuel.
So if you think of going in [a] warming direction of 2 degrees C compared to a cooling direction of 5 degrees C, one can say that we might be changing the Earth, you know, like 40 percent of the kind of change that went on between the
Ice Age; and now are going back in time and so a 2 - degree change, which is about 4 degrees F on a global average, is going to be very significant in terms of change in the distribution of vegetation, change in the kind of climate
zones in certain areas, wind patterns can change, so
where rainfall happens is going to shift.
Chris Borstad, a geophysicist at the University Centre in Svalbard, Norway, is particularly interested in Larsen C's «suture
zones» — areas
where glacial
ice flows off land and merges.
The apparent decline is greatest around the
ice sheet's edges, but it also is occurring in the high elevation interior known as the dry snow
zone,
where the reflectivity is effectively reset each winter by new snowfall.
With more research, astrobiologists working to identify planets in the universe with temperature levels that could allow for the presence of liquid water may be able to expand the
zones they consider potentially habitable to include planets
where water is found as
ice.
The wind changes were found to be heaving warm currents from deeper waters up into a
zone where the Antarctic
ice sheet is vulnerable to melt and crumble from beneath — the area
where towers of
ice sit atop submerged ground.
The best explanation is that it was forced under the
ice crust, in a «subsumption»
zone similar to Earth's subduction
zones where rocky crust slides beneath rocky crust.
Ice appears to form in areas called growth zones, but since the moon itself isn't growing, no one knew where this new ice we
Ice appears to form in areas called growth
zones, but since the moon itself isn't growing, no one knew
where this new
ice we
ice went.
At some point, when it looked liked we were doing well, Pangar entered a rage - state
where he somehow gained
ice attacks and would call forth large
ice crystals to box you into certain
zones trapping you with Pangar with no room to escape.
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A good example is in the
ice - themed
zone,
where playing as Sonic, you'll suddenly see Tails pop up and announce «I'll take over from here!»
And it means more time must be spent on those
ice sheets, both in the melt
zones and the places
where accumulation of snow still dominates — including Swiss Camp, which I visited on the flanks of the
ice sheet in 2004:
Other pages display maps of individual glaciers, with white regions indicating the «accumulation
zone,»
where snow falls and adds to the mass, and gray stippled areas showing the «ablation
zone,»
where melting eats away at the
ice.
The glacier goes afloat at the grounding
zone where bedrock, till, and
ice meet the ocean waters about 600 meter below sea level (Rignot, 1996).
Tivy (University of Alaska Fairbanks); 5.7 Million Square Kilometers; Statistical This method is based on a simple regression
where the predictor is the previous summer (May / June / July) sea surface temperature (SST) in the North Atlantic and North Pacific oceans near the marginal
ice zone.
It contains the full range of positions of the marginal
ice zone (MIZ)
where sea
ice interacts with open water.
An area of ocean that extends from the permanent
ice zone to the boundary
where winter
ice extent is at a maximum.
The accumulation
zone is the area of the glacier
where snow accumulates and packs into
ice.
The remote location of the Antarctic and Greenland polar
ice sheets may leave us with the impression that developments in these regions have little effect on the climate and life in the temperate
zones of the Earth,
where most of us live.
There are
zones where new deep water is formed, mostly at the edges of the polar
ice caps.
Grounding line /
zone - The junction between a glacier or
ice sheet and
ice shelf; the place
where ice starts to float.
In the map below, major
ice storm impacts (mentioned earlier) are seen in the transition
zone where the warm flow of moisture from the south is being chemically nucleated.