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Shyness is the cause of much unhappiness for a great many people. Shy people are (1) and serf-conscious; that is, they are (2) concerned with their own appearance and actions. (3) thoughts are (4) occurring in their minds: What kind of impression am I makingIt is obvious that such (5) feelings must affect people adversely. A person’s self-concept is (6) in the way he or she behaves, and the way a person behaves affects other people’s reactions. (7) , the way people think about themselves has a profound effect on all areas of their lives.Shy people, having low (8) , are likely to be passive and easily influenced by others. They need reassurance (9) they are doing "the fight thing". Shy people are very (10) to criticism; they feel it (11) their inferiority. A shy person may (12) to a compliment with a statement like this one: "You’re just saying that to make me feel good." It is clear that, (13) self-awareness is a healthy quality, overdoing it is harmful.Can shyness be completely (14) , or at least reduced Fortunately, people can overcome shyness with determined and patient effort in building self-confidence. Since shyness goes (15) with lack of serf-esteem, it is important for people to accept their weakness as well as their strengths. For example, most people would like to be "A" students in every subject. It is not fair for them to (16) themselves inferior because they have difficulty (17) some areas. People’s expectations of themselves must be (18) Each one of us is a unique, worthwhile individual. The better we understand ourselves, the easier it becomes to (19) our full potential. Let’s not allow shyness to block our chances for a rich and (20) life. 11()

A. unfriendly
B. unbelievable
C. unimaginable
D. uncomfortable

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Text 4The recent, apparently successful prediction by mathematical models of an appearance of El Nifio—the warm ocean current that periodically develops along the Pacific coast of South America -- has excited researchers. Jacob Bjerkness 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 oscillations between appearance of the warm El Nifio and the cold so-called anti-El Nifio. The answer, al 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 Niflo, two conditions exist: (1) unusually warm water extends along the eastern Pacific, principally along the coasts of Ecuador and Peru, and (2) 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 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 Nifio, which raise sea level in the east, simultaneously send a signal to the west lowering sea 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 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 carrying 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 negative 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 cold cycle-ending positive Kelvin waves beginning another warming cycle. Which of the following would most seriously undermine the validity of the model of El Nifio mentioned()

A. During some years El Nifio extends significantly farther along the coasts of Ecuador and Peru than during other years.
B. During periods of unusually cool temperature along the eastern Pacific, an El Nifio is much colder than normal.
C. The variations in the time it takes Rossby waves to cross the Pacific depend on the power of the winds that the waves encounter.
D. The western boundary of the Pacific basin is so irregnlar that it hinders most coastal Kelvin waves from heading eastward.

Text 2SoBig. F was the more visible of tile two recent waves of infection, because it propagated itself by e-mail, meaning that victims noticed what was going on. SoBig. F was so effective that it caused substantial disruption even to those protected by anti-virus software. That was because so many copies of the virus spread that many machines were overwhelmed by messages from their own anti-virus software. On top of that, one common counter-measure backfired, increasing traffic still furthers. Anti-virus software often bounces a warning back to the sender of an infected e-mail, saying that the e-mail in question cannot be delivered because it contains a virus. SoBig. F was able to spoof this system by "harvesting" e-mail addresses from the hard disks of infected computers. Some of these addresses were then sent infected e-mails that had been doctored to look as though they had come from other harvested addresses. The latter were thus sent warnings, even though their machines may not have been infected.Kevin Haley of Symantec, a firm that makes anti-virus software, thinks that one reason SoBig. F was so much more effective than other viruses that work this way is because it was better at searching hard-drives for addresses. Brian King, of CERT, an internet-security center at Carnegie- Mellon University in Pittsburgh, note that, unlike its precursors, SoBig. F was capable of "multi- threading": it could send multiple e-mails simultaneously, allowing it to dispatch thousands in minutes.Blaster worked by creating a "buffer overrun in the remote procedure call". In other word, that means it attacked a piece of software used by Microsoft’s Windows operating system to allow one computer to control another. It did so by causing that software to use too much memory.Most worms work by exploiting weaknesses in an operating system, but whoever wrote Blaster had a particularly refined sense of humor, since the website under attack was the one from which users could obtain a program to fix the very weakness in Windows that the worm itself was exploiting.One way to deal with a wicked worm like Blaster is to design a fairy godmother worm that goes around repairing vulnerable machines automatically. In the case of Blaster someone seems to have tried exactly that with a program called Welchi. However, according to Mr. Haley, Welchi has caused almost as many problems as Blaster itself, by overwhelming networks with "pings" -- signals that checked for the presence of other computers.Though both of these programs fell short of the apparent objectives of their authors, they still caused damage. For instance, they forced the shutdown of a number of computer networks, including the one used by the New York Times newsroom, and the one organizing trains operated by CSX, a freight company on America’s east coast. Computer scientists expect that it is only a matter of time before a truly devastating virus is unleashed. SoBig. F damaged computer programs mainly by()

A. sending them an overpowering number of messages.
B. harvesting the addresses stored in the computers.
C. infecting the computers with an invisible virus.
D. destroying the anti-virus software of the computers.

Text 3Of all the truths that this generation of Americans hold self-evident, few are more deeply embedded in the national psyche than the maxim "It pays to go to college." Since the GI Bill trans-formed higher education in the aftermath of WWII, a college diploma, once a birthright of the leisured few, has become an attraction for the upwardly mobile, as integral to the American dream as the pursuit of happiness itself. The numbers tell the story: in 1950s, 43% of high-school graduates went on to pursue some form of higher education; at tile same time, only 6% of Americans were college graduates. But by 1998, almost 2 to out of 3 secondary-school graduates were opting for higher education -- and 21% of a much larger U.S. population had college diplomas. As Prof. Herbert London of New York University told a commencement audience last June: "the college experience has gone from a rite passage to a right of passage."However, as the class of 2004 is so painfully discovering, while a college diploma remains a requisite credential for ascending the economic ladder, it no longer guarantees the good life. Rarely since the end of the Great Depression has the job outlook for college graduates appeared so bleak: of the 1.1 million students who received their bachelor degrees last spring, fewer than 20% had lined up full-time employment by commencement. Indeed, an uncertain job market has precipitated a wave of economic fear and trembling among the young. "Many of my classmates are absolutely terrified," says one of the fortunate few who did manage to land a permanent position. "They wonder if they’ll ever find a job."Some of this recession-induced anxiety will disappear if a recovery finally begins to generate jobs at what economists consider a normal rate. But the sad fact is that for the foreseeable future, college graduates will in considerable surplus, enabling employers to require a degree even for jobs for which a college education is really unnecessary. According to Kristina Shelley of the Bureau of Labor Statistics -- who bases her estimate on a "moderate projection" of current trends -- 30 per- cent of college graduates entering the labor t0rce between now and the year 2008 will be unemployed or will find employment in jobs for which they will be overqualified, joining what economists call the "educationally underutilized."Indeed, it may be quite a while-- if ever -- before those working temporarily as cocktail waitresses or taxi drivers will be able to pursue their primary, career paths. Of course waiting on tables and bustling cab fares are respectable ways to earn a living. But they are not quite what so many young Americans -- and their parents -- had in mind as the end product of four expensive years in college. According to the passage, what causes educationally underutilizing()

A. College graduates are more than the society needs.
B. It's fashionable to be waitresses or taxi drivers.
C. People respect those who once did physical work.
D. The payment to blue-collar workers is much higher than that to white-collar employees.

经常出现意识障碍的疾病是

A. 精神分裂症
B. 躯体疾病所致精神障碍
C. 神经衰弱
D. 心身疾病
E. 急性焦虑症

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