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剧情简介
剧名:日本海啸是如何发生的类型:剧情、纪录制作:英国电视四台语言:英文上映时间:2011年03月日本海啸是如何发生的日本海啸是如何发生的水下地震、火山爆发或水下塌陷和滑坡等大地活动都可能引起海啸 当地震发生于海底,因震波的动力而引起海水剧烈的起伏,形成强大的波浪,向前推进,将沿海地带一一淹没的灾害,称之为海啸 海啸在许多西方语言中称为“tsunami”,词源自日语“津波”,即“港边的波浪”(“津”即“港”) 这也显示出了日本是一个经常遭受海啸袭击的国家 目前,人类对地震、火山、海啸等突如其来的灾变,只能通过观察、预测来预防或减少它们所造成的损失,但还不能阻止它们的发生 新华社东京3月12日电:日本东北地区太平洋海域11日下午发生芮氏8 8级的巨大地震,引发的海啸几乎袭击了日本列岛太平洋沿岸的所有地区 专家认为,海啸规模如此之大原因有二,一是地震本身规模大且震源浅,二是震源所在海域海岸地形特殊,放大了海啸能量 此次地震是日本有地震观测史以来震级最高的一次,其能量相当於芮氏7 3级的阪神大地震的178倍 地震后,仙台新港等太平洋沿岸各地出现了10米高的大 海啸 东京大学地震研究所教授古村孝志认为,海啸规模巨大是由於震源浅且地震规模大造成的 据日本气象厅最新修正,本次地震震源深度约24公里 该研究所副教授酒井慎一说:“对海底海啸仪的数据进行分析后发现,在地震发生后五六分钟,海面至少上升了3 5米 这是首次观测到海面高度出现这么大的变化 以前的海啸最多也就导致海面出现数釐米的升高 ”地震后仅30分钟,就有3米高的海啸到达了陆地 港湾空港技术研究所研究员高桥重雄说:“海啸高度和受灾区域之广都是国内迄今最大的,属百年一遇规模 ” 高桥指出,今后还有可能发生海啸,“退回海裏的海啸有时在折返陆地后,会变得更大 目前居民仍有必要继续在尽量远离海岸的高地避难” 日本气象厅也指出: “由於地震规模巨大,海啸有可能持续一天左右 ”海啸袭击了日本列岛的广阔范围,但是以岩手县为中心的三陆海域是裏亚斯型海岸(属沉降海岸),有可能导致灾害更为严重 气象厅地震海啸监视科科长横山博文指出,裏亚斯型海岸的特殊地形有可能使海啸的巨大能量进一步被放大 京都大学防灾研究所教授间濑肇指出:“据推测,冲上陆地的海水量可以与(2004年)印度尼西亚苏门答腊岛附近海域发生地震时相匹敌 而在三陆海域的那种 裏亚斯型海岸,有很多外侧宽广而内侧狭窄的‘三角形海湾’,越向海湾内侧,海浪就越容易升高 ”他预想,在海湾深处等地点,海啸也许达到了30米高 三陆地区是经常遭到海啸袭击的地方 1896年,一场震感不大的地震,却引发了超过20米高的海啸,死者和失踪者达到约2 2万人 1933年的三陆地震也引发了超过20米的海啸,死者和失踪者达到约3000人
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