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词汇 example_english_ice-cap
释义

Examples of ice cap


These examples are from corpora and from sources on the web. Any opinions in the examples do not represent the opinion of the Cambridge Dictionary editors or of Cambridge University Press or its licensors.
Distinct layers of firn were observed to the south, where the icecap ends in a small cliff of 19 m in height.
Most of the island is covered by an icecap that rises to 35 m above sea level, as determined by airborne laser scanning.
All of them are located along the crest of the icecap.
They noted a strongly bisected coastline, with inlets reaching towards the icecap, and numerous meltwater lakes, often without apparent external discharge.
There is widespread evidence from terrestrial samples of ice and snow, including icecap cores that contain organic compounds.
Their results confirmed from space the 2001 airborne measurements of an icecap up to 35 m high, and an island of 2 km extent.
During this visit it became clear that there was only one island, not a group of islets, and that the icecap was higher than previously estimated.
In addition to the official flag hoisting and the geodetic measurements, three samples of gravel and one sample with moss were collected north of the icecap.
It was traditionally just the north polar icecap that was melting, but there is now melting at both poles.
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Instead of a polar icecap we have large icebergs detaching themselves and starting off on courses which cannot be foreseen or known in advance.
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It is covered with a very deep and thick icecap.
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There would also be a progressive growth in the weight of the icecap of "between 100 and 400 billion tons per year".
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There is evidence of melting of the polar icecap at both poles.
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They can go round the world under the icecap or in any other way they like.
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The marked route ends at the bushline and the remainder of the climb is on tussock, rock, and eventually the summit icecap glacier.
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Until 12,000 years ago, the plateau was covered by an icecap, leaving it largely devoid of soil and lacking in resources.
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Further north beyond the icecap, annual precipitation decreases.
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As the research program expanded, a permanent icecap base was needed for deep drilling and other large-scale projects.
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Ice sheet is considered the more correct term, as icecap generally refers to less extensive ice masses.
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The study also considered the possibility of exploratory mid-winter expeditions across the polar icecap.
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An icecap will typically feed a series of glaciers around its periphery.
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The icecap has a maximum thickness of 880m 0, and has been steadily shrinking since 1985.
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The marathon course takes the runners over the permanent, 3 km thick icecap and through tundras, moraine landscapes, glaciers, among other outstanding nature sceneries.
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A permanent icecap of about in area covers the summit region, extending down to roughly on the north side and on the south.
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The icecap was 200to300 ft thick where it touched the mountain.
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It is subglacial, meaning that it is permanently covered by the largest icecap in the world.
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The icecap in the north is of a lower altitude than the one in the south.
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Essentially the entire planet had an icecap climate.
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Polaria is a chain of mountainous islands covered for at least part of the year by the southern polar icecap.
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This icecap is centered at, and is at an elevation of 1889m 0.
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It is also sometimes referred to as an icecap.
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The entire summit area is covered by a substantial icecap, and several large glaciers descend the flanks of the cone.
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This peak used to have an icecap, but it was last seen in 1989 and by 2003 it was totally gone.
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The total land area including the land covered by the icecap is over 500,000 km.
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It bears heavy glacial traces as a huge icecap covered it during the last ice age.
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It is possible that the area of this icecap may be shrinking due to localized climate change or more widespread global warming.
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The icecap is approximately 50m ft thick on average.
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A large body of glacial ice astride a mountain, mountain range, or volcano is termed an icecap or ice field.
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It includes the north polar icecap, which has a swirl pattern and is roughly 1,100 km across.
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The central part under the icecap was eroded.
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Significant areas of till are found in the central highlands arranged roughly in a circle around the former icecap.
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Nevertheless, as all the explorers who travelled closer and closer to the pole reported, the polar icecap is quite thick, and persists year-round.
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Precipitation is nearly non-existent in icecap climates.
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The other notable feature of this area are deep, steep valleys cut by water that poured through this area as the icecap melted.
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Likewise, the melting of the northern polar icecap which is composed of floating pack ice would not significantly contribute to rising sea levels.
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Based on estimates of lake volume and decaying icecap size, values of 0.41.2 m circulate.
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By 2003 the icecap had shrunk in area by a total of 40% of its 28.4km2 sqmi area of 1976.
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Between 2004 and 2006, the icecap was thinning at a rate of 1 m per year.
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If the icecap melted, it would be under water.
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Gradually, as the temperature increased the growth of the glaciers lessened and eventually they began to recede to what is now the polar icecap.
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Each southern winter, the icecap covers the surface to a latitude of 50.
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The outer edges of the icecap are contaminated with dust (0.15% by weight) and are mostly water ice.
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The icecap covers the caldera of a volcano high, which has erupted relatively frequently since the last ice age.
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As a result, vegetation such as the longleaf pine and other pine species were associated to the coastal regions of the unexposed icecap areas.
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Its summit rises more than 1000mft -2 above the average surface of the icecap plateau.
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The only place where water ice is visible at the surface is at the north polar icecap.
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In an icecap climate, no plants can grow, and ice gradually accumulates until it flows elsewhere.
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The municipality has an area of 225,500 km (87,066 mi), a large portion of which is icecap area.
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Due to mapped crevasses, the icecap route was far from a straight line.
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The ice ramp is still used for scientific access to the icecap, including supply trains to mid-ice sites.
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Likewise, shrinkage/expansion of the northern polar icecap which is composed of floating pack ice do not significantly affect sea level.
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Part of the icecap consists of dry ice, solid carbon dioxide.
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The surface composition of the northern icecap in middle spring (after a winter's accumulation of seasonal dry ice) has been studied from orbit.
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In the mountains and on the icecap itself, annual precipitation can reach to between 4,000 and 5,000 mm, for the most part in the form of snow.
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To evaluate the contribution of polar ice caps to the observed changes, regular observation of large polar areas is necessary.
It comprises a series of chapters written by international experts on sea ice, ice sheets, and glaciers and ice caps.
Polar lows can form over relatively mild ocean waters when cold air sweeps in from the icecap, leading to upward motion and convection, usually in the form of snow.
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Many of the smaller ice caps are stagnant, and have no outlet glaciers.
The residual southern icecap is misplaced.
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The mineral may have formed through the melting of acidic snow, or the melting and discharge of sulfur-rich water from the base of the polar icecap.
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The seasonal frosting of some areas near the southern icecap results in the formation of transparent 1-metre-thick slabs of dry ice above the ground.
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The seasonal frosting of some areas near the southern icecap results in the formation of transparent 1 m thick slabs of dry ice above the ground.
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The seasonal frosting of some areas near the southern icecap results in the formation of transparent 1 metre thick slabs of dry ice above the ground.
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The rest is polar ice caps, deserts and mountain ranges.
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Far more grave is the carbon dioxide build-up, with its greenhouse effect and the possibly devastating results of partially melting the polar ice caps.
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We can also look at the way in which ice caps are melting in the northern and southern hemispheres.
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The challenge of dealing with a hole in the ozone layer, melting ice caps, rising sea levels and climate change.
From Europarl Parallel Corpus - English
It may well be found under the ice caps in almost unlimited quantities.
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The melting of the polar ice caps and warming of the sub-polar regions—the tundra—lead to increased emissions of methane, which results in a faster melt.
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That in turn will cause a global warming, the melting of the polar ice caps and the invasion of much land by rising sea levels.
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The global warming process is held to offer potential risks: the break-up of the ice caps and rogue icebergs on shipping lanes.
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The evidence that the polar ice caps are disintegrating in the long run is weak.
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Clearly, we are only at the early stages of man exploiting the natural resources under the sea and the ice caps.
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We have heard about the possible greenhouse effect, with the heating up of the planet and the consequential melting of the polar ice caps.
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As we know, the polar ice caps are already melting at an alarming rate and mountain glaciers are retreating.
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Or will it, as some scientists think, cause a wind flow to the poles which will increase the ice caps and lower sea levels?
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The melting of the glaciers and the ice caps on land, however, will raise the sea level.
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The biggest problem, however, we are dealing with is what will happen to the ice caps and the ice-sheets.
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If the ice caps melt and fresh water is released, salinity and water movements will be affected.
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The ice caps are measurably melting.
From Europarl Parallel Corpus - English
The situation is that serious: forests that have existed for millions of years could disappear, and we are seeing the polar ice caps melting and the oceans rising.
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We now come to what might be considered the 64,000 dollar—we might as well call it the 6,000 million dollar—question; namely, what happens to the ice caps?
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More specifically, the melting of the ice caps is opening up new opportunities in the creation of new navigation routes and the exploitation of natural resources.
From Europarl Parallel Corpus - English
These examples are from corpora and from sources on the web. Any opinions in the examples do not represent the opinion of the Cambridge Dictionary editors or of Cambridge University Press or its licensors.
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