大学英语六级分类模拟题420及答案解析.doc
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1、大学英语六级分类模拟题 420 及答案解析(总分:340.00,做题时间:90 分钟)一、Part Writing(总题数:5,分数:269.00)1.Directions: For this part, you are allowed 30 minutes to write an essay commenting on the remark “There isn“t anything noble about being superior to another person. True nobility is in being superior to the person you once w
2、ere.“ You can give examples to illustrate your point and then explain what you will do to stay modest. You should write at least 150 words but no more than 200 words. Write your essay on Answer Sheet 1. (分数:106.50)_2.Directions : For this part, you are allowed 30 minutes to write an essay on perseve
3、rance by referring to the saying “What you do every day matters more than what you do every once in a while.“ You can cite examples to illustrate your point and then explain what you will do to enhance your perseverance. You should write at least 150 words but no more than 200 words. Write your essa
4、y on Answer Sheet 1. (分数:106.50)_3.Directions: For this part, you are allowed 30 minutes to write an essay commenting on the saying “Better three hours too soon than a minute too late.“ You can cite examples to illustrate your point. You should write at least 150 words but no more than 200 words. (分
5、数:20.00)_4.Directions : For this part, you are allowed 30 minutes to write an essay entitled On Aiming Higher by commenting on the saying “Who aims at excellence will be above mediocrity; who aims at mediocrity will be far short of it.“ You should write at least 150 words but no more than 200 words.
6、 (分数:20.00)_5.Directions: For this part, you are allowed 30 minutes to write a short essay on the major ranking in university. You should write at least 150 words but no more than 200 words. Write your essay on Answer Sheet 1. (分数:16.00)_二、Part Reading Compr(总题数:0,分数:0.00)Blowing Hot and ColdA. Clim
7、ate change may be slow and uncertain, but that is no excuse for inaction. One reason why uncertainty over climate change looks to be with us for a long time is that the oceans, which absorb carbon from the atmosphere, act as a time-delay mechanism. Their massive thermal inertia means that the climat
8、e system responds only very slowly to changes in the composition of the atmosphere. Another complication arises from the relationship between carbon dioxide (CO 2 ), the principal greenhouse gas (GHG), and sulphur dioxide (SO 2 ), and a common pollutant. Efforts to reduce man-made emissions of GHGs
9、by cutting down on fossil-fuel use will reduce emissions of both the gases. The reduction in CO 2 will cut warming, but the concurrent SO 2 cut may mask that effect by contributing to the warming. B. There are so many such fuzzy factorsranging from aerosol particles to clouds to cosmic radiationthat
10、 we are likely to see disruptions of familiar climate patterns for many years without knowing why they are happening or what to do about them. Tom Wigley, a leading climate scientist and member of the UN“s Intergovernmental Panel on Climate Change (IPCC), goes further. He argues in an excellent book
11、 published by the Aspen Institute, “US Policies on Climate Change: What Next?“, that whatever policy changes governments pursue, scientific uncertainties will “make it difficult to detect the effects of such changes, probably for many decades.“ C. As evidence, he points to the negligible short-to me
12、dium-term difference in temperature resulting from an array of emission “pathways“ on which the world could choose to embark if it decided to tackle climate change. He plots various strategies for reducing GHGs that will lead in the next century to the stabilization of atmospheric concentrations of
13、CO 2 at 550 parts per million (ppm). That is roughly double the level which prevailed in preindustrial times, and is often suggested by climate scientists as a reasonable target. But even by 2040, the temperature differences between the various options will still be tinyand certainly within the magn
14、itude of natural climatic variance. In short, in another four decades we will probably still not know if we have over-or under-shot. D. However, that does not mean we know nothing. We do know, for a start, that the “greenhouse effect“ is real: without the heat-trapping effect of water vapor, CO 2 ,
15、methane and other naturally occurring GHGs, our planet would be a lifeless 30 or so colder. Some of these GHG emissions are captured and stored by “sinks“, such as the oceans, forests and agricultural land, as part of nature“s carbon cycle. E. We also know that since the industrial revolution began,
16、 mankind“s actions have contributed significantly to that greenhouse effect. Atmospheric concentrations of GHGs have risen from around 280ppm two centuries ago to around 370ppm today, thanks chiefly to mankind“s use of fossil fuels and, to a lesser degree, to deforestation and other land-use changes
17、. Both surface temperatures and sea levels have been rising for some time. F. There are good reasons to think temperatures will continue rising. The IPCC has estimated a likely range for that increase of 1.4-5.8 over the next century, although the lower end of that range is more likely. Since what m
18、atters is not just the absolute temperature level but the rate of change as well, it makes sense to try to slow down the increase. G. The worry is that a rapid rise in temperatures would lead to climate changes that could be devastating for many (though not all) parts of the world. Central America,
19、most of Africa, much of south Asia and northern China could all be hit by droughts, storms and floods and otherwise made miserable. H. The colder parts of the world may benefit from warming, but they too face danger. One is the conceivable collapse of the Atlantic “conveyor belt“, a system of curren
20、ts that gives much of Europe its relatively mild climate; if temperatures climb too high, say scientists, the system may undergo radical changes that damage both Europe and America. That points to the biggest fear: warming may trigger irreversible changes that transform the earth into a largely unin
21、habitable environment. I. Given that possibility, extremely remote though it is, it is no comfort to know that any attempts to stabilize atmospheric concentrations of GHGs at a particular level will take a very long time. Because of the oceans“ thermal inertia, explains Mr. Wigley, even once atmosph
22、eric concentrations of GHGs are stabilized, it will take decades or centuries for the climate to follow suit. And even then the sea level will continue to rise. This is a vast challenge, and it is worth bearing in mind that mankind“s contribution to warming is the only factor that can be controlled.
23、 So the sooner we start drawing up a long-term strategy for climate change, the better. J. That is why the long-term objective for climate policy must be a transition to a low-carbon energy system. Such a transition can be very gradual and need not necessarily lead to a world powered only by bicycle
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