2015考研英语阅读地震学与海啸

　　Seismology and tsunamis

　　地震学与海啸

　　Making waves

　　掀起新浪潮

　　A better tsunami-prediction system is now underdevelopment

　　更精准的海啸预测系统现已在开发中

　　Next time, they might see it coming

　　下次海啸来袭时，人们可提前准备

　　GEOLOGISTS have long known that some marine earthquakes generate fierce tsunamis andsome do not.

　　地质学家们早已知道有的海洋地震会引起强烈海啸，而有的则不会。

　　But, as the situation in Japan makes painfully clear, there is no good way for people beingtossed around by a tremor to know the difference until a wave arrives.

　　但是，日本的惨痛教训告诉我们，被地震震得惊慌失控的人们根本意识不到一场海啸即将到来。

　　A new earthquake-monitoringsystem developed by Andrew Newman and Jaime Convers at the Georgia Institute ofTechnology may, however, help to change that.

　　而现在，由乔治亚理工学院的安德鲁?纽曼与亚伊梅?康弗斯共同研发的最新地震监测系统有望改变现状。

　　During an earthquake, the Earth s crust is uplifted.

　　地震时，地壳板块隆升。

　　If the epicentre is on the seabed, that also lifts the water above the bed, creating a wave.

　　如果震中位于海底，板块运动带动上方海水起伏，形成波浪。

　　However, the size of this wave varies with the nature of the uplift.

　　波浪大小因板块隆升性质而定。

　　For tsunami-generating purposes, earthquakes can generally be divided into two sorts.

　　按照是否引发海啸，地震可分两类。

　　Deep ones generate small or non-existent tsunamis because their uplifting effects areabsorbed by the overburden.

　　一是深震，隆升通常被表层所吸收，因此不引发海啸或只引发小型海啸。

　　Shallow ones, whose full crust-displacing force is felt at the surface, are the danger.

　　二是浅震，由于地表震感强烈，因此也更危险。

　　The problem is deciding which is which.

　　当前的问题是如何区分这两者。

　　Once all the data are in, an earthquake s depth can be worked out with reasonableaccuracy.

　　只要有全面的数据，则可较精准地测算地震的深度。

　　But that takes time.

　　然而，这一过程需花费一定时间。

　　The recent Japanese quake, for example, was thought initially to have happened 83kmdown.

　　例如，近期日本地震最初深度测算为地下83km，

　　The latest measurements suggests its depth was actually 30km.

　　而最近的一次测算结果却显示，深度实为30km。

　　Normally, that would still put it in the class of safe earthquakes, but it was so powerful thatthe usual rules did not apply.

　　通常来说，30km仍可划入安全等级。但此次地震能量巨大，以往的经验概不管用。

　　The secret of the new method is that depth changes an earthquake s character in ways otherthan just its tsunami-generating propensity.

　　新系统的秘密在于地震深度对地震性质的改变不仅仅停留在是否引发海啸的问题上。

　　The rupture in the rock that causes a deep earthquake propagates rapidlyat about 3km asecond.

　　岩层断裂引发深震传播速度很快大约3km/秒。

　　A shallow rupture moves more slowly: 1?km a second is common.

　　而浅震传播速度较慢：一般约1.5km/秒。

　　The speed seems related to the rigidity of the rock that is rupturing, and deep rock, which isunder more pressure, is more rigid.

　　速度可能与断裂岩层的坚硬程度有关，深层岩体受压力更大，也更坚硬。

　　Shallow rocks bend, and that slows the rupture down.

　　浅层岩体有韧度，可减缓断裂。

　　The effect is to give seismologists a tool they can use to make an instant estimate of anearthquake s depth and thus, if it is submarine, the risk of its creating a big tsunami.

　　地震学家可据此迅速估算地震深度，如果是海洋地震，还能估算地震是否引发强烈海啸。

　　The system Dr Newman and Mr Convers have developed taps into hundreds of seismicmonitoring stations around the world.

　　纽曼博士与康弗斯先生研发的新系统接入了世界各地几百所地震监测站。

　　When an earthquake is detected, the software immediately looks at the size of the tremorand the location of its epicentre.

　　当检测到地震时，该系统软件立即测算地震规模与震中位置。

　　If the quake s magnitude is greater than 6.5 and the epicentre is underwater, it thenrequests information from the relevant stations on how long the earthquake took frombeginning to end.

　　如果级数超过6.5级且震中位于水下，系统则要求相关监测站报送地震全程持续时间。

　　That allows it to work out how quickly energy was released by the earthquake, and thushow fast the rupture propagated.

　　这一信息可帮助计算地震能量释放速度，并以此计算岩层断裂速度。

　　An energy-release rate indicating a rupture rate of 1?km a second or less sets the alarmbells ringing, for the earthquake has probably spawned a tsunami.

　　岩层断裂速度达1.5km/秒以下的能量释放速度将会拉响警报，而这时极有可能引发海啸。

　　though the system is also sensitive to the actual earthquake magnitude, and adjustsaccordingly, so it did not miss the tsunami-creating potential of the Japanese earthquakeeither.

　　尽管如此，该系统也能检测出地震级数并作出相应调整，因此也检测出了日本地震会引发海啸的风险。

　　The two researchers tried their invention out last year and analysed a great many quakes,including one of magnitude 7.8 that happened on October 25th in western Indonesia.

　　两位研究者去年对该发明进行了测试，用以分析了许多地震，包括去年10月25日印尼西部发生的里氏7.8级地震。

　　The epicentre was 70km from the Mentawai islands, and the quake was felt there onlyweakly.

　　震中位于距民大威群岛70km处，岛上只有轻微震感。

　　But it still raised a devastating tsunami that killed more than 400 islanders.

　　但是，地震随后引发了一次破坏力极强的海啸，导致400多位岛民死亡。

　　The system quickly detected this quake and the two researchers reported recently inGeophysical Research Letters that it automatically identified the tsunami threat 8?minutes after the earthquake began.

　　该系统迅速检测到印尼地震，两位研究者近期在向《地理物理研究快报》的报告中指出，系统在地震开始后8.5分钟自动检测到震后海啸威胁。

　　It then ran a series of checks, and after 16? minutes was completely certain that conditionswere right for a tsunami to form.

　　随后，系统启动了一系列检查程序，震后16.5分钟便完全确定海啸即将发生。

　　Since it took 35 minutes for the tsunami to come ashore, the system could, had it been usedto sound the alarm, have given people 18? minutes to flee.

　　因为海啸将在震后35分钟后到达，如果使用该系统发出警报，则为人们赢得了18.5分钟宝贵的逃生时间。

　　Unfortunately, it was not then attached to any sort of alarm that could let the Mentawaiislanders know that they were in danger.

　　不幸的是，该系统当时还未与警报系统结合，因此无法及时通知民大威群岛岛民海啸险情。

　　With luck, such a lack of warning will not happen again.

　　而幸运的是，缺乏警报机制的这种情况以后不会再有了。

　　By the summer the system should be hooked up to alarms around the world, and will be ableto determine tsunami risk within seven minutes of a shock being detected.

　　今年夏天之前，该系统将会与全世界警报系统相连接，并将会在检测到地震后7分钟内确定海啸发生的概率。

　　It will then be up to local authorities to have evacuation plans in place.

　　随后则由地方政府开展撤离计划。

　　But they will no longer be able to say they did not see it coming.

　　到那时，政府便不可能再推脱说不知道海啸会来了。

　　词语解释

　　1.prediction n.预言;预报

　　Recent discoveries will bear his prediction out.

　　近来的种种发现将会证实他的预言。

　　2.marine a.海的;海事的

　　His father is a marine biologist.

　　他父亲是位海洋生物学家。

　　3.earthquake n.地震

　　There has been a dreadful earthquake in Iran.

　　伊朗发生了一次可怕的地震。

　　4.epicentre n.震中;中心

　　The roads towards the epicentre are clogged with such convoys.

　　通往震中的道路上挤满了这样的车队。

　　5.generate v.产生;发生

　　75% of France s electricity is generated by nuclear reactors.

　　法国75%25的电能产生于核反应堆。