印尼苏门答腊三次大地震与中国珠江洪水关系的研究
摘要
本文研究印尼苏门答腊大地震与中国珠江流域大洪水之间的关系[1].印尼苏门答腊以南的板块俯冲带,是强烈地震活跃地区.近200年来发生3次大地震:1833年11月24日8.7级地震、1861年2月21日8.5级地震和2004年12月26日Mw9.3级地震.每次地震后,第二年都在中国华南珠江流域发生巨灾.巨大地震产生宽阔的地震破裂带,引起地壳中放出携热水汽.由于地下裂隙的复杂性和不畅性,放气效应到达地表可滞后于地震断续达一年以上.排出的水汽被搭载在西南气流上到达华南地区.
In this paper,it is studied that the relationship between the Sumatra Earthquake and the Pearl River Floods.The subduction zones in south of Sumatra are trouble spots of strong earthquakes.In the past 200 years,serious earthquakes took place for three times,Ms 8.7 Nov.11th,1833,Ms8.5 Feb.21st,1861,Ms 9.3 Dec. 26th,2004.The second year after the earthquakes,heavy floods happened in the Pearl River Basin in South China.The earthquakes caused broad zones of fracture,which made hot water vapours release from the earth's crust.Because of complex and obstructed fissures,the water vapours rose up to the earth surface one year later after the earthquakes.The water vapours moved to South China with the southwest air current.
In this paper,it is studied that the relationship between the Sumatra Earthquake and the Pearl River Floods.The subduction zones in south of Sumatra are trouble spots of strong earthquakes.In the past 200 years,serious earthquakes took place for three times,Ms 8.7 Nov.11th,1833,Ms8.5 Feb.21st,1861,Ms 9.3 Dec. 26th,2004.The second year after the earthquakes,heavy floods happened in the Pearl River Basin in South China.The earthquakes caused broad zones of fracture,which made hot water vapours release from the earth's crust.Because of complex and obstructed fissures,the water vapours rose up to the earth surface one year later after the earthquakes.The water vapours moved to South China with the southwest air current.
引文
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[22]叶守.冬季低纬气流与云南罕见大雪[J].气象,1985.11(3):225.Ye S.The current in low latitudes in winter and rare heavy-snow in Yunnan[J].Meteorological Monthly,1985.11(3):225.
[23]赵永平,陈永利,白学志,等.南海-热带东印度洋海温年际变化与南海季风爆发关系的初步分析[J].热带气象学报,2000,16(2):115~122.Zhao Y P,Chen Y L,Bai X Z,Wang F.The relations be-tween the SST anomalies in South China Sea-Tropical easternIndian Ocean and the South China Sea monsoon[J].Journalof Tropical Meteorology,2000,16(2):115~122.
[24]王黎娟,何金海,管兆勇.苏门答腊地区对流活动及其与南海夏季风建立的关系[J].南京气象学院学报,2004,27(4):451~460.Wang L J,He J H,Guan Z Y.Characteristics of convectionactivities over sumatra area and its relationship with SCSsummer monsoon onset[J].Journal of Nanjing Institute ofMeteorology,2004,27(4):451~460.
[25]阎俊岳.南海西南季风爆发的气候特征[J].气象学报,1997.55(2):174~186.Yan J Y.Climatological characteristics on the onset of theSouth China Sea Southwest monsoon[J].Acta MeteorologicaSinica,1997.55(2):174~186.
[26]曾庆存,李建平.南北两半球大气的相互作用和季风的本质[J].大气科学,2002,26(4):433~448.Zeng Q C,Li J P,Interactions between the northern andsouthern hemispheric atmospheres and the essence of mon-soon[J].Chinese Journal of Atmospheric Sciences,2002,26(4):433~448.
[27]马宗晋,叶洪.2004年12月26日苏门答腊-安达曼大地震构造特征及地震海啸灾害[J].地学前缘,2005.12(1):281~287.Ma Z J,Ye H.The Dec.26,2004 sumatra-andaman earth-quake:Tectonic setting and the tsunami disaster[J].EarthScience Frontiers,2005.12(1):281~287.
[28]徐杰,高祥林,陈国光,等.2004年12月26日印度尼西亚8.7级大地震构造背景的初步分析[J].地震地质,2005.27(2):324~331.Xu J,Gao X L,Chen G G,et al.A preliminary analysis ofseismotectonics for the M 8.7 Indonesia earthquake on De-cember 26,2004,[J].Seismology and Geology,2005.27(2):324~331.
[29]Lay T,kanamori H,Ammon C J,Nettles M,et al.The greatSumatra-andaman earthquake of 26 december 2004[J].Sci-ence,2005,308:1127~1133.
[30]Stein S,Okal E A.Speed and size of Sumatra earthquake[J].Nature,2005,434:581~582.
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