大学英语六级分类模拟题382及答案解析.doc
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1、大学英语六级分类模拟题 382及答案解析(总分:100.00,做题时间:90 分钟)一、Reading Comprehensio(总题数:0,分数:0.00)The recent, apparently successful prediction by mathematical models of an appearance of EI Ninothe warm ocean current that periodically develops along the Pacific coast of South Americahas excited researchers. Jacob Bjerk
2、nes pointed out over 20 years ago how winds might create either abnormally warm or abnormally cold water in the eastern equatorial Pacific. Nonetheless, until the development of the models no one could explain why conditions should regularly shift from one to the other, as happens in the periodic os
3、cillations between appearances of the warm EI Nino and the cold so-called anti-El Nino. The answer, at least if the current model that links the behavior of the ocean to that of the atmosphere is correct, is to be found in the ocean. It has long been known that during an El Nino, two conditions exis
4、t: unusually warm water extends along the eastern Pacific, principally along the coasts of Ecuador and Peru, and winds blow from the west into the warmer air rising over the warm water in the east. These winds tend to create a feedback mechanism by driving the warmer surface water into a “pile“ that
5、 blocks the normal upwelling of deeper, cold water in the east and further warms the eastern water, thus strengthening the wind still more. The contribution of the model is to show that the winds of an El Nino, which raise sea level in the cast, simultaneously send a signal to the west lowering sea
6、level. According to the model, that signal is generated as a negative Rossby wave, a wave of depressed, or negative, sea level, that moves westward parallel to the equator at 25 to 85 kilometers per day. Taking months to traverse the Pacific, Rossby waves march to the western boundary of the Pacific
7、 basin, which is modeled as a smooth wall but in reality consists of quite irregular island chains, such as, the Philippines and Indonesia. When the waves meet the western boundary, they are reflected, and the model predicts that Rossby waves will be broken into numerous coastal Kelvin waves carryin
8、g the same negative sea-level signal. These eventually shoot toward the equator, and then head eastward along the equator propelled by the rotation of the Earth at a speed of about 250 kilometers per day. When enough Kelvin waves of sufficient amplitude arrive from the western Pacific, their negativ
9、e sea-level signal overcomes the feedback mechanism tending to raise the sea level, and they begin to drive the system into the opposite cold mode. This produces a gradual shift in winds, one that will eventually send positive sea-level Rossby waves westward, waves that will eventually return as col
10、d cycle-ending positive Kelvin waves, beginning another warming cycle.(分数:20.00)(1).Which of the following best describes the organization of the first paragraph?(分数:4.00)A.A model is described and its value assessed.B.A result is reported and its importance explained.C.A phenomenon is noted and its
11、 significance debated.D.A hypothesis is introduced and contrary evidence presented.(2).According to the passage, which of the following features is characteristic of an El Nino?(分数:4.00)A.Cold coastal water near Peru.B.Wind blowing from the west.C.Random occurrence.D.Worldwide effects.(3).Which of t
12、he following, if true, would most seriously undermine the validity of the model El Nino that is presented in the passage?(分数:4.00)A.El Nino extends much farther along the coasts of Ecuador and Peru during some years.B.The rising of cold water in the eastern Pacific depends on the local characters.C.
13、The variations in the time for Rossby waves to cross the Pacific rely on the wind power.D.The Pacific irregular western coast hinders most Kelvin waves from heading eastward.(4).According to the model presented in the passage, which of the following normally signals the disappearance of an El Nino?(
14、分数:4.00)A.The arrival in the eastern Pacific of negative sea-level Kelvin waves.B.A shift in the direction of the winds produced by an anti-El Nino.C.The reflection of Kelvin waves reaching the eastern border of the Pacific.D.An increase in the speed at which negative Rossby waves cross the Pacific.
15、(5).The primary purpose of the text as a whole is to _.(分数:4.00)A.introduce a new explanation of physical phenomenonB.explain the difference between two natural phenomenaC.illustrate the limits of applying mathematics to complex problemsD.clarify the distinction between an old explanation and a new
16、modelAided by the recent ability to analyze samples of air trapped in glaciers, scientists now have a clearer idea of the relationship between atmospheric composition and global temperature changing over the past 160,000 years. In particular, determination of atmospheric composition during periods o
17、f glacial expansion and retreat (cooling and warming) is possible using data from the 2,000 meter Vostok ice core drilled in Antarctica. The technique involved is similar to that used in analyzing cores of marine sediments, where the ratio of the two common isotopes of oxygen, 180 and 160, accuratel
18、y reflects past temperature changes. Isotopic analysis of oxygen in the Vostok core suggests mean global temperature fluctuations of up to 10 degrees centigrade over the past 160,000 years. Data from the Vostok core also indicate that the amount of carbon dioxide has fluctuated with temperature over
19、 the same period: the higher the temperature, the higher the concentration of carbon dioxide and the lower the temperature, the lower the concentration. Although change in carbon dioxide content closely follows change in temperature during periods of deglaciation, it apparently lags behind temperatu
20、re during periods of cooling. The correlation of carbon dioxide with temperature, of course, does not establish whether changes in atmospheric composition causing the warming and cooling trends or were caused by them. The correlation between carbon dioxide and temperature throughout the Vostok recor
21、d is consistent and predictable. The absolute temperature changes, however, are from 5 to 14 times greater than would be expected on the basis of carbon dioxide“s own ability to absorb infrared radiation, or radiant heat. This reaction suggests that, quite aside from changes in heat-trapping gases,
22、commonly known as greenhouse gases, certain positive feedbacks are also amplifying the temperature change. Such feedbacks might involve ice on land and sea, clouds, or water vapor, which also absorb radiant heat. Other data from the Vostok core show that methane gas also correlates closely with temp
23、erature and carbon dioxide. The methane concentration nearly doubled, for example, between the peak of the penultimate glacial period and the following interglacial period. Within the present interglacial period it has more than doubled in just the past 300 years and is rising rapidly. Although the
24、concentration of atmospheric methane is more than two orders of magnitude lower than that of carbon dioxide, it cannot be ignored: the radiative properties of methane make it 20 times more effective, molecule for molecule, than carbon dioxide in absorbing radiant heat. On the basis of a simulation m
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