關(guān)于GRE試題和試題模板

1、關(guān)于GRE試題和試題模板GRE，全稱Graduate Record Examination，中文名稱為美國(guó)研究生入學(xué)考試，適用于除法律與商業(yè)外的各專業(yè)，由美國(guó)教育考試服務(wù)處（Educational Testing Service，簡(jiǎn)稱ETS)主辦。GRE試題16. UPBRAlD : REPROACH :(A) dote : like(B) lal: : stray(C) vex : please(D) earn : desire(E) recast : explainDirections: Each passage in this group is followed by questions

2、 based on its content.After reading a passage, choose the best answer to each question. Answer all questionsfollowing a passage on the basis of what is stated or implied in that passage.lt has been known for many decades that the appear-ance of sunspots is roughly periodic, with an averagecycle of e

3、leven years. Moreover, the incidence of solarflares and the flux of solar cosmic rays, ultraviolet radia-tion, and x-radiation all vary directly with the sunspot (5)cycle. But after more than a century of investigation. therelation of these and other phenomena, known collec-tively as the solar-activ

4、ity cycle, to terrescrial weatherand climate remains unclear. For example. the sunspotcycle and the allied rnagnetic-polarity cycle have been (10)linked to periodicities discerned in records of such vari-ables as rainhll. temperature, and winds. lnvariably,however, the relation is weak. and commonly

5、 ofdubiousstatistical significance.Effects of solar variability over longer terms have also (15)been sought. The absence of recorded sunspot activity inthe notes kept by European observers in the late seven-teenth and early eighteenth centuries has led some schol-ars to postulate a brief cessation o

6、f sunspot activity atthat time (a period called the Maunder minimum). The (20)Maunder minimum has been linked to a span of unusualcold in Europe extending from the sixteenth to the earlynineteenth centuries. The reality of the Maunder mini-mum has yet to be established, however, especially sincethe

7、records that Chinese naked-eye observers of solar (25)activity made at that time appear to contradict it. Scien-tists have also sought evidence of long-term solar period-icities by examining indirect climatological data, such asfossil recoras of the thickness of ancient tree rings. Thesestudies, how

8、ever, failed to link unequivocally terrestrial(30)climate and the solar-activity cycle, or even to contirmthe cycles past existenue.If consistPn! and re!iab!e geo!sgigal-arek-xologiealevidence tracing the solar-activity cycle in the distantpast could be found, it might also resolve an important(35)i

9、ssue in solar physics: how to model solar activity. Cur-rently, chere are two models of solar activity. The tirstsupposes that the Suns internal motions (caused byrotation and convection) interact with its large-scalemagnetic field to produce a dynamo. a device in which(40)mechanical energy is conve

10、rted into the energy of a mag-netic field. ln short. the Suns large-scale magnetic fieldis taken to be self-sustaining, so that the solar-activitycycle it drives would be maintained with little overallchangc for perhaps billions of years. The alternative(45)exp)anarion supposes that the Suns large-s

11、ca)e magneticfield is a remnant of the field the Sun acquired when itformed, and is not sustained against decay. In thismodel. the solar mechanism dependent on the SunsmagnetiC field runs down more quickly. Thus, the char-(50)acteristics of the solar-activity cycle uvuld be expected tochange over a

12、long period of time. Modern solar obser-vations span too short a time to reveal whether presentcyclical solar aCtivity is a long-lived feature of the Sun,or merely a transient phenomenon.17. The author focuses primarily on(A) presenting two competing scientific theories concerning solaractivity and

13、evaluating geological evidence often cited to support them(B) giving a brief overview of some recent scientifrc developmentsin solar physics and assessing their impact on future climatological research(C) discussing the difficulties involved in linkinl: ter- restrialphenomena with solar activity and

14、 indicating how resolving that issuecould have an impact on our understanding of solar physics(D) pointing out the futility of a certain line of sci- entific inquiryinto the terrestrial effects of solar activity and recommendine itaaban- donment in favor of purely physics-oriented research(E) outlin

15、ine the specific reasons why a problem in solar physics hasnot yet been solved and faulting the overly theoretical approach of modernphysicists.18. Which of th.e following statements about the two models of solaractivity. as they are described in lines 37-55, is accurate?(A) In both modgls cyclical

16、solar activity is regarded as a long-livedfeature of the Sun, persisting with little change over billions of years.(B) Tn both models the solar-activity cycle is hypothesized as beingdependent on the large-scale solar magnetic field.(C) Tn one model the Suns magnetic fieid is thought to play a role

17、incausing solar activ- ity, whereas in the other model it is not.(D) In one model solar activity is presumed to be unrelated to terrestrialphenomena. whereas in the other model solar activity is thought to haveobservable effects on the Earth.(E) In one model cycles of solar activity with peri- odici

18、ties longer thana few decades are con- sidered to be impossible, whereas in the other modelsuch cycles are predicted.19. According to the passage, late seventeenth- and early eighteenth-centuryChinese records are impor- tant for which of the following reasons?(A) They suggest that the data on which

19、the Maunder minimum was predicatedwere incorrect.(B) They syggest that the Maunder minimum can- not be related to climate.(C) Thcy suggest that the Maunder minimum might be -alid only for Europe.(D) They establish the existence of a span of unusu- ally cold weatherworldwide at the time of the Maunde

20、r minimum.(E) They establish that solar activity at the tirne of the Maunder minimumdid not significantly vary from its present pattern.20. The author implies which of the followine about currently availablegeological and archaeoloeical evidence concerning the solar-activity cycle?(A) It best suppor

21、ts the model of solar activity described in lines 37-45.(B) It best supports the model of solar activity described in lines 45-52.(C) It is insufficient to confirtn either model of solar activity describedin the third paragraph.(D) It contradicts both models of solar activity as they are presented i

22、nthe third paragraph.(E) It disproves the theory that terrestrial weather and solar activitv arelinked in some way.21. Tt can be inferred from the passage that the argu- ment in favor of themodel described in lines 37- 45 would be strengthened if which of the followingwere found ta he tme?(A) Episod

23、es of intense volcanic eruptions in the distant past occurred incycles having very long periodicities.(B) At the present time the global level of thunder- storm activity increasesand decreases in cycles with periodicities of approximately 11 years.(C) In the distant past cyclical climatic changes ha

24、d periodicities of longerthan 200 years.(D) In the last century the length of the sunspot cycle has been known tovary by as much as 2 years from its average periodicity of 11 years.(E) Hundreds of millions of years ago, solar- activity cycles displayed thesame periodicities as do present-day solap-a

25、ctivity cycles.22. lt can be inferred from the passage that Chinese observations of the Sunduring the late seventeenth and early eighteenth centuries(A) are ambiguous because most sunspots cannot be seen with the naked eye(B) probably were made under the same weather conditions as those made in Euro

26、pe(C) are more reliable than European observations . made during this period(D) record some sunspot activity during this period(E) have been employed by scientists seeking to argue that a change in solaractivity occurred during this period.23. It can be inferred from the passage that studies attempt

27、ing to use tree-ringthickness to locate possi- ble links between solar periodicity and terrestrialclimate are based on which of the following assump- tions?(A) The solar-activity cycle existed in its present form during the time periodin which the tree rings erew.(B) The biological mechanisms causing tree growth are unaffected by short-termweather pat- terns.(C) Average tree-ring thickness varies from species to species.(D) Tree-ring thicknesses reflecr changes in terres- trial climate.(E) Both terrestrial climate and the solar-activity cycle randomly afct tree