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Английский язык. Учебное пособие для аспирантов консерваторий и вузов искусств

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Climate Change (IPCC), by anywhere between 2.5 and 10.4 degrees Fahrenheit (1.4 to 5.8 degrees Celsius) over the course of this century. This warming is not, and will not be, uniform. Warming in the Arctic is projected to be two to three times the global average; already, tempera­ture increases in the region are far exceeding those in more temperate zones. In Alaska and western Canada, winter temperatures have in­creased by as much as 5–7 degrees F (3–4 degrees C) over the past fifty years; over the next 100 years, annual average temperatures are project­ed to rise 5–9 degrees F (3–5 degrees C) over land and up to 13 degrees F (7 degrees C) over the ocean. Winter temperatures are projected to in­crease by 7–13 degrees F (4–7 degrees C) over land and by 13–18oF (7– 10 degrees C) over the ocean.
Sea Ice
Sea ice (literally, the frozen surface of the sea) is an essential ele­ment of the Arctic marine ecosystem. On its underside grows algae which support the entire food chain. It provides shelter for species such as arctic cod, and is an essential habitat for migratory birds, for seals and walruses, for polar bears, and for Native peoples.
However, sea ice is in retreat throughout the Arctic. Over the past thirty years, annual average sea ice extent has decreased by about" 8%, or approximately 386,000 square miles (one million square kilometers), an area the size of Texas and Arizona (or Norway, Sweden, and Den­mark) combined. Additional declines of 10–50% in annual average sea­ice extent are projected by 2100, with summer sea ice declines projected to be around 50%, and some models predicting near-complete disappear­ance of summer sea ice.
The remaining sea ice is also thinner. Reductions in average thick­ness levels across the Arctic are estimated at 10–15%, with some areas showing reductions of up to 40% between the 1960s and late 1990s.
Glaciers
With increasing temperatures, most glaciers have been in retreat across the Arctic since the early 1960s, a trend that sped up in the 1990s. About half of the estimated loss of mass in glaciers worldwide is in western Alaska, while seasonal surface melt on the Greenland ice sheet­by far the largest area of land ice in the northern hemisphere-has been increasing since satellite observations began in 1979. Climate models predict that local warming over Greenland may be one to three times the
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global average, which additional models suggest could eventually lead to a near-complete melting of the Greenland ice sheet.
Habitat Change
Climate change is projected to cause northward shifts in vegetation, and because warmer temperatures favor taller, denser vegetation, boreal forests will encroach on the arctic tundra, and the tundra will shift northward into the realm of the polar desert. The consequences of such change will be varied and sometimes seemingly contradictory: tree growth rates will increase in some areas and decline in others; disturb­ances such as fires and floods will likely either speed up or inhibit forest growth; and although the range of trees such as black and white spruce may expand, higher temperatures and drier conditions will make them more vulnerable to disease and to insect pests such as the spruce bark beetle and the black-headed budworm, which in turn will benefit from those changing conditions.
As a result of encroaching forests and rising sea levels, tundra area is expected to shrink to its lowest extent in at least the past 21,000 years, potentially reducing the breeding area for many migratory bird species and the grazing areas for land animals that depend on the open landscape of tundra and polar desert habitats.
Wildlife Impacts
Changes in habitat will inevitably affect distribution and abundance of associated wildlife populations. For example, mosses and lichens are particularly vulnerable to warming which, because they form the basis of important food chains (providing, for example, primary winter food sources for reindeer/caribou), will have significant repercussions throughout the ecosystem. Caribou (the North American form of the species Rangifer tarandus) and reindeer (Eurasian form of the same spe­cies) will be affected not only by declines in some of their food sources, but also by increased difficulty in reaching some of those food sources as a result of climatic changes. For example, numbers of Peary caribou on Canada's arctic islands plummeted from 26,000 in 1961 to 1,000 by 1997, apparently largely as a result of autumn rains icing the winter food supply and crusting the snow cover, limiting access to forage. Mild weather and wet snow prompt the collapse of under-snow spaces that provide burrows for lemmings and voles, affecting population cycles of
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those species and leading to declines in their populations, with impacts on their predators, such as snowy owls, skuas, weasels, and ermine.
Changes in the thickness and extent of sea ice are likely to affect the species which live on sea ice habitat, and indeed there is evidence that such impacts are already occurring. For example, a 1999 study showed that polar bears in Hudson Bay suffered 15% declines in average weight and the number of cubs born between 1981 and 1998. These changes are likely correlated to late sea-ice formation in fall and early break-up in spring, which leads to a longer winter fasting period for fe­males, for whom healthy fat reserves are essential to survival and repro­ductive success.
According to the Arctic Climate Impact Assessment, a study con­ducted on behalf of the Arctic Council, polar bears "are unlikely to sur­vive as a species if there is an almost complete loss of summer sea-ice cover, which is projected to occur before the end of this century by some climate models."
Human Impacts
Melting of permafrost – the layer of permanently-frozen soil that is a defining characteristic of polar and alpine environments—is already causing collapses in the ground above it, leading to structural failures in buildings and roadways throughout the Arctic and subarctic. Continued melting is likely to make construction and transportation in the region increasingly problematic. Conversely, disappearing sea ice is likely to lead to significantly more navigable seaways: for example, the naviga­tion season for the Northern Sea Route (the passage across the north of Russia from Novaya Zemlya to the Bering Strait) is projected to increase from the current 20-30 days per year to 90–100 days by 2080. While this may be a boon to international commerce, it will increase the risk of ac­cidents, oil spills, and the chronic air and water pollution associated with shipping activities.
Retreating sea ice and melting permafrost also increase the likeli­hood of erosion in many areas. In some coastal Arctic regions, retreating sea ice has left low-lying coastal areas more vulnerable to storm surges, with sometimes dramatic consequences. The village of Shishmaref, for example, located on an island off the coast of northern Alaska, has been increasingly battered and damaged bу storms. Several houses have been evacuated and moved to high ground, and now the entire village is likely to be relocated to the mainland.
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For many Native peoples of the Arctic, a warming climate and sub­sequent environmental changes are already profoundly altering their tra­ditional, subsistence way of life. For example, predicted northward movement of sea ice is expected to reduce the availability of seabirds as food resources for many arctic communities, while reduced sea ice ex­tent and thickness is also making it more difficult and dangerous to find and hunt for marine mammals.
Global Consequences
At the same time, melting arctic ice, combined with increased pre­cipitation and river runoff, may lead to a freshening of the ocean in the North Atlantic, disrupting the critical salinity balance and leading to a collapse in the ocean circulation pattern that brings warm water to Eu­rope from the tropics. As a consequence, global warming could lead to regional cooling in the Northeast Atlantic region.
B. GREENPEACE BRIEFING: NEWS AND VIEWS
CONSERVATION NOT EXPLOTATION
CETACEANS AND THE OCEANS CRISIS
As human activities continue to degrade the world's oceans, species and populations of cetaceans (the collective name for whales, porpoises and dolphins) are under increasing threat. Global warming, ozone deple­tion, toxic chemicals, noise pollution, over fishing and ship strikes all impact cetaceans and are symptoms of a wider crisis in the oceans. In view of the oceans crisis outlined above, Greenpeace believes that com­mercial hunting of cetacean species should be stopped and that the Inter­national Whaling Commission (IWC) should make conservation its pri­mary focus to ensure that these animals are preserved for future genera­tions.
Climate change and Ozone depletion
The devastating impacts of anthropogenic climate change are al­ready being felt across the globe and the oceans and their inhabitants are not immune. In particular cetacean species, which inhabit Polar Regions, are likely to be severely impacted by the temperature rises predicted for these areas. The Southern Ocean around Antarctica, where a large pro­portion of the world's great whales feed, is already being affected as ob-
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served by the substantial melting and collapses of the Larsen A and В ice shelves. Higher temperatures are resulting in a reduction in sea ice, im­pacting the primary productivity of the region and consequently the en­tire Antarctic marine food web. Sea ice forms a highly productive envi­ronment, with phytoplankton growing in high densities under the ice. The phytoplankton is grazed upon by substantial numbers of small crus­taceans including krill, which in turn is the primary prey item of most Antarctic species including the great whales.
Until recently a population estimate of 760,000 was generally ac­cepted for the population of Southern Ocean minke whales, (the species targeted by Japan's-called 'scientific' whaling programme in the Antarc­tic). However when the IWC Scientific Committee examined more re­cent data, they came to the conclusion that the real figure was 'apprecia­bly' lower and might be less than half of what was previously thought. The IWC scientists so far have not been able to agree an explanation for the apparent decline but have not been able to rule out that a real decline is occurring.
Unsustainable fishing practices
Of all the threats facing the oceans, over fishing is perhaps the sin­gle greatest threat. The United Nations Food and Agriculture Organiza­tion (FAO) estimates that 71–78% of the world's fish stocks are fully ex­ploited, overexploited, or depleted. Cetaceans, far from being the cause of collapsing fish stocks as claimed by the Fisheries Agency of Japan and the pro-whaling lobby, are themselves the victims of over fishing and industrialized fisheries.
There is evidence to suggest that industrial fishing methods and the vast volumes of fish being removed from the oceans ecosystems is hav­ing major impacts on marine ecosystems and ecosystems dynamics. For example, a study by US whale biologists suggests that the virtual remov­al of the North American Grand Banks stock of herring by over fishing in the 1960s, removed a major prey source for baleen whales in the area.
Prey depletion is not the only impact of the vast expansion of the global fishing industry on cetaceans. A more direct impact is that of in­cidental capture in fishing gear. Every year hundreds of thousands of ce­taceans become entangled in fishing nets and drown. For example, by catch of small cetaceans is an urgent problem in the North East Atlantic. In the area of the English Channel, Celtic Sea and Bay of Biscay an es­timated 10,000 dolphins and porpoises are being killed each year.
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Of particular concern is the current situation affecting different populations of harbour porpoises in the North Atlantic. A range of fish­eries using gillnets off the coasts of the US, Canada and Ireland and within the North Sea have all been shown to incidentally capture large numbers of this species. For instance it is estimated that approximately 7,000 harbour porpoises are taken every year by the Danish set net fish­eries in the North Sea.
Scientists estimate that this could represent as much as 5% of some species' populations in this area being killed in fishing gear annually: a rate of over 1% of a population is internationally recognized to be cause for concern. Despite evidence that particular fisheries are directly re­sponsible (such as the sea bass pair trawling fishery) and an obligation to protect cetacean species under the EU Habitats Directive, no action has been taken at EU level that will effectively stop this incidental killing.
Toxic pollution
The release of toxic chemicals into the marine environment present a major and insidious threat to cetaceans. Of prime concern are the fol­lowing groups of chemicals: persistent organic pollutants (POPs) which including PCBs and DDT, heavy metals such as mercury and endocrine disrupting chemicals.
Many POPs readily concentrate in fatty tissue such as blubber and as a consequence high body burdens have been found in cetaceans, which are positioned near the top of the food web, such as dolphins and other toothed whales. However some baleen whales also carry signifi­cant loadings. Endocrine disrupters, which interfere with reproduction even at very low concentrations, have immense potential for harm. There is little published research identifying the impacts of endocrine disrupt­ing substances on cetaceans, however as noted by an IWC Scientific Committee workshop on chemical pollution and cetaceans '...wherever endocrine disrupting chemicals have been sought within cetacean tissue they have been found.'
The build up of toxic contaminants in cetacean species are also a health risk for consumers of whale and dolphin products. Last year a Norwegian scientific committee concluded that the 500 tonne stockpile of frozen minke whale blubber which was being kept in the hope that it could be exported to Japan was too toxic for human consumption. Janneche Utne Skaare, deputy director of the National Veterinary Insti­tute and a scientist on the panel was quoted by Reuters as saying that
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"Human consumption of whale blubber would lead to unacceptable lev­els of PCBs" and that a single gram of minke blubber would contain al­most a tenth of the maximum weekly intake of PCBs under European Union guidelines.
Ocean noise
Cetaceans are highly reliant on their hearing for their survival. Many species have acute hearing and use sound for prey location, navi­gation and communication – often over considerable distances in the case of several of the large baleen whale species. Many cetacean biolo­gists are becoming increasingly concerned that noise pollution in the oceans emanating from shipping, seismic surveys, oil drilling, marine construction and active sonar devices may be negatively impacting ceta­cean populations. In extreme cases noise pollution may cause actual physiological damage but more often it interferes with the natural behav­iour of the animals.
One of the most worrying sources of marine noise pollution is the deployment of low-frequency active sonar (LFAS). Developed by the military to detect enemy submarines, LFAS uses the same low frequen­cies that whales use to communicate and are most acoustically sensitive to. Although not the first case, the strongest evidence that high-power "active" sonar systems can and do kill marine animals surfaced in March of 2000, when a stranding of 14 beaked whales, along with two minke whales and a spotted dolphin in the Bahamas coincided with the U.S. Navy's use of extremely loud active sonar (mid-frequency sonar). De­spite a marine mammal scientist's and others' attempts to save the ani­mals, seven of them died. Autopsies showed that all but one of the ani­mals suffered from hemorrhages in and around their ears. And in Febru­ary 2001, it was observed that at least one of the whale species that stranded in the Bahamas had virtually disappeared from the area, raising questions about impacts well beyond initial strandings and deaths. That LFAS can be lethal to cetaceans was given further credence when in September 2002, 15 more beaked whales washed up on beaches on the Canary Islands of Fuerteventura and Lanzarote. NATO militaries, in­cluding ships from the U.S., were conducting a major naval exercise at the time.
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Ship strikes
A more localized threat is that posed by ship collisions, however it may be a significant threat to some local populations; for example there is concern about the number of collisions between fin whales and high speed ferries in the waters mid-way between the French mainland and Corsica which are preferred summer feeding grounds for the fins. For the North Atlantic right whale reducing ship strikes is essential if the species is to survive into the next century.
Despite having been internationally protected from hunting since 1935, the North Atlantic right whale has failed to recover and is close to becoming extinct. Only a few hundred animals remain and these are found along the eastern shores of North America. The situation is made acute by the fact that every year a number of these slow moving whales are the victims of ship collisions and entanglement in fishing gear. With such a small population, the death of even a single individual is of enor­mous significance.
Cetaceans on a knife edge
The western North Pacific population of gray whales is one of the most threatened populations of whales and provides a useful case study on how a combination of human-induced threats may actually push a population over the brink. This population is facing 'an extremely high risk of extinction in the immediate future'. Numbering fewer than 100 individuals, this poorly known population is genetically distinct from the eastern population of gray whales, and shows no sign of recovery having been heavily depleted in the past by commercial whaling. To date only 14 reproductive females have been identified in the population.
The greatest threat to this population are the oil and gas develop­ments taking place to the Northeast of Sakhalin Island – the location of an area, 5–10km wide and 70 km long, which constitutes the sum­mer/autumn feeding grounds of the western North Pacific grays. The oil and gas developments present a variety of threats to the western North Pacific grays. Oil spills; routine pollution from drilling, increased vessel and air traffic and seismic surveys could all have negative impacts.
This situation is exacerbated by the fact that many of the whales are so called 'skinny whales', emaciated animals with their bones show­ing through their blubber suggesting that they are already having diffi­culty finding enough of the benthic organisms on which they feed. Such 'skinny' whales have also been observed in the eastern North Pacific
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population of gray whales and in 1999 a number of these emaciated ani­mals were found dead along the eastern North Pacific coastline. It has been suggested that the cause of these strandings was a reduction in the availability of the whales' principle prey – amphipod crustaceans – in the Bering and Chukchi Seas and this was linked to increased sea tempera­tures – a phenomenon concurrent with anthroprogenic climate change.
Strengthening the conservation agenda of the IWC
Last year's agreement to strengthen the conservation agenda of the IWC makes it clear that conservation of whales, dolphins and porpoises without lethal exploitation, is a legitimate position and focus for the Commission and its Scientific Committee and favoured by the majority of its members. The establishment and operation of the conservation committee, which is strongly supported by Greenpeace, is likely to be energetically opposed by Japan, its paid supporters and other pro­whaling countries.
The conservation committee can build on the important conserva­tion decisions taken by the IWC in the past and shift the focus of the IWC from exploitation to conservation. By virtue of its global reach and considerable scientific expertise, the IWC is in a unique position to de­liver significant conservation benefits for cetaceans and the oceans as a whole.
From the report Whales in a Degraded Ocean, Greenpeace 2001
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Приложение
КРАТКИЕ УКАЗАНИЯ ПО ПЕРЕВОДУ
С АНГЛИЙСКОГО ЯЗЫКА НА РУССКИЙ
При переводе с английского языка на русский помните сле-
дующее.
Сначала прочитайте заголовок и постарайтесь догадаться, о чем этот текст. После этого прочитайте весь текст, для того чтобы составить общее представление о нем. Далее читайте текст по абза­цам и переводите на русский язык.
Если текст содержит новые слова, о значении которых трудно догадаться по контексту, пользуйтесь большим англо-русским сло­варем.
В словарях все слова даются в алфавитном порядке, при этом учитывается не только первая, но и вторая, третья, четвертая и по­следующие буквы. Чтобы быстро найти слово, необходимо хорошо знать английский алфавит.
Слово обычно сопровождается транскрипцией, с помощью ко­торой можно правильно прочитать любое неизвестное английское слово, а затем идет буква или сочетание нескольких букв, указыва­ющих на то, какой частью речи является данное слово. Например: book n (noun – имя существительное) или with prep (preposition – предлог).
Слова в словаре даются в исходной, или основной, форме, то есть существительные даются в единственном числе, глаголы – в неопределенной форме и т. д. Таким образом, очень важно выяс­нить исходную форму слова, а затем уже искать ее в словаре. Например, в тексте вы встретили слово remedies. В такой форме в словаре его пет. Чтобы найти исходную форму (remedy), нужно от­бросить окончание -es и заменить букву i на у (сравните: city –
cities).
Если вам нужно найти значение слова grabbed, то сначала найдите его исходную форму (grab). Для этого вы отбрасываете -ed (окончание прошедшего времени или причастия прошедшего вре­мени) и букву b, которая появилась в результате удвоения конечной согласной для сохранения краткости чтения гласных (сравните: stop
stopped).
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