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Çѱ¹¼öÀÚ¿øÇÐȸ / v.36, no.3, 2003³â, pp.437-445
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¸Å°³º¯¼ö¿¡ µû¸¥ ÁöÁøÇØÀÏÀÇ Ã³¿À¸§³ôÀÌ ¿¹Ãø
( Estimation of Tsunami Run-up Heights with Parameters ) |
| ¾È¿µÃ¢;Ȳ±Ô³²;Á¶¿ë½Ä; (ÁÖ) °ÇÀÏ¿£Áö´Ï¾î¸µ Ç׸¸ºÎ;ÀüºÏ´ëÇб³ Åä¸ñȯ°æ°øÇаú;ÇѾç´ëÇб³ Åä¸ñ°øÇаú;
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| ¿ì¸®³ª¶ó ³²ÇØ¾È Áö¿ªÀº ´ÙµµÇØ Áö¿ªÀ̹ǷΠ´ë±Ô¸ð ÁöÁøÇØÀÏÀÌ ¹ß»ýÇÏ¿´À» ¶§ ¼¶°ú ¼¶ »çÀÌÀÇ »óÈ£°£¼·À¸·Î ÀÎÇÑ ¿¹±âÄ¡ ¾ÊÀº ÁöÁøÇØÀÏ ÇÇÇØ°¡ ¿ì·ÁµÉ ¼öµµ ÀÖ´Ù. º» ¿¬±¸¿¡¼´Â µÎ°³ÀÇ ¿øÇü ¼¶ »çÀÌÀÇ Ã³¿À¸§³ôÀÌ º¯È¸¦ ÀÔ»çÆÄ Æø°ú µÎ ¼¶ »çÀÌÀÇ °Å¸®¿Í °°Àº ¸Å°³º¯¼ö¸¦ ÀÌ¿ëÇÏ¿© °è»êÇÏ¿´´Ù. µÎ °³ÀÇ ¿øÇü¼¶ ÁÖÀ§¿¡¼ ÀÔ»çÆÄ ¼öÆò±æÀ̰¡ µÎ ¼¶ÀÇ ¾ç³¡ ¹Ù±ùÂÊ ÇØÀúÁö¸§ °Å¸®º¸´Ù Ŭ °æ¿ì µÎ ¼¶ ¾ÈÂÊ ºÎºÐ¿¡¼ ó¿À¸§³ôÀ̰¡ ±Þ°ÝÈ÷ Áõ°¡ÇÏ¿´À¸¸ç, µÎ¼¶ »çÀÌÀÇ °£°ÝÀÌ ÁÙ¾îµé¼ö·Ï ÀÔ»çÆÄÀÇ Ã³¿À¸§³ôÀ̰¡ Áõ°¡ÇÏ¿´´Ù. |
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| Since many islands are located in the South Sea, unexpected damage by tsunamis could be caused by mutual interferences between adjacent islands. In this study, the variation of run-up heights is investigated by using different crest lengths of incident waves and different distances between two adjacent islands. The run-up height sharply increases when the crest length of Incident waves is greater than the distance bewteen outer boundaries of two islands. The run-up height also increases as the distance between two adjacent islands decreases. |
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| Ű¿öµå |
| ÁöÁøÇØÀÏ;ó¿À¸§³ôÀÌ;ÀÔ»çÆÄ Æø;õ¼ö¹æÁ¤½Ä;tsunami;run-up height;crest length of incident wane;shallow-water equations; |
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Çѱ¹¼öÀÚ¿øÇÐȸ³í¹®Áý / v.36, no.3, 2003³â, pp.437-445
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1226-6280
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO200302612607966)
¾ð¾î : Çѱ¹¾î |
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| ³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø |
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