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Çѱ¹¼öÀÚ¿øÇÐȸ / v.35, no.4, 2002³â, pp.453-461
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ÀÓ¿ø¿¡¼ÀÇ 1983³â µ¿ÇØ ÁߺΠÁöÁøÇØÀÏ ¼öÄ¡¸ðÀÇ: 2. ÀÓ¿øÇ׿¡¼ÀÇ ¹ü¶÷
( Numerical Simulations of 1983 Central East Sea Tsunami at Imwon: 2. Run-up Process at Imwon Port ) |
| ÀÌÈ£ÁØ;±è°æÈñ;Á¶¿ë½Ä; ±¹¸³¹æÀ翬±¸¼Ò;±¹¸³¹æÀ翬±¸¼Ò;ÇѾç´ëÇб³ °ø°ú´ëÇÐ Åä¸ñ°øÇаú;
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| µ¿ÇØ¿¡¼ ¹ß»ýÇÑ 1983³â ÁöÁøÇØÀÏÀÇ µ¿Çؾȿ¡¼ ó¿À¸§ °úÁ¤À» ¼öÄ¡ÇØ¼®ÇÏ¿´´Ù. ºñ¼±Çü õ¼ö¹æÁ¤½Ä¿¡ ±Ù°ÅÇÑ À¯ÇÑÂ÷ºÐ ¼öÄ¡¸ðÇüÀ» ÀÌ¿ëÇÏ¿´À¸¸ç, ÀÓ¿ø¿¡¼ ÃÖ´ë ó¿À¸§³ôÀ̸¦ ¿¹ÃøÇÏ¿´´Ù. ¿¹ÃøµÈ °á°ú´Â ÇöÀå °üÃøÀÚ·á¿Í ºñ±³Àû Àß ÀÏÄ¡ÇÏ¿´´Ù. ÁöÁøÇØÀÏ ¹ü¶÷ À§ÇèÀ» °Á¶Çϱâ À§ÇØ Ã³¿À¸§³ôÀ̸¦ ±Ù°ÅÇÑ ½ÃÇèÀûÀÎ ÃÖ´ë¹ü¶÷µµ¸¦ Á¦ÀÛÇÏ¿´´Ù. |
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| The run-up process of the 1983 Central East Sea Tsunami along the Eastern Coast is numerically investigated in this study. A finite difference numerical model based on the nonlinear shallow-water equations is employed. The maximum run-up height at Imwon is predicted and compared to field observation. A good agreement is observed. A maximum inundation map is made based on the maximum run-up heights to accentuate hazards of tsunami flooding. |
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| ÁöÁøÇØÀÏ;ó¿À¸§;¹ü¶÷;ºñ¼±Çü õ¼ö¹æÁ¤½Ä;¹ü¶÷µµ;tsunami;run-up;inundation;nonlinear shallow-water equations;inundation map; |
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Çѱ¹¼öÀÚ¿øÇÐȸ³í¹®Áý / v.35, no.4, 2002³â, pp.453-461
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1226-6280
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO200218718191432)
¾ð¾î : Çѱ¹¾î |
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| ³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø |
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