¶óÆæÆ®¦¢Ä«Æä¦¢ºí·Î±×¦¢´õº¸±â
¾ÆÄ«µ¥¹Ì Ȩ ¸í»çƯ°­ ´ëÇבּ¸½Ç޹æ Á¶°æ½Ç¹« µ¿¿µ»ó°­ÀÇ Çѱ¹ÀÇ ÀüÅëÁ¤¿ø ÇÐȸº° ³í¹®
ÇÐȸº° ³í¹®

Çѱ¹°Ç¼³°ü¸®ÇÐȸ
Çѱ¹°ÇÃà½Ã°øÇÐȸ
Çѱ¹µµ·ÎÇÐȸ
Çѱ¹»ý¹°È¯°æÁ¶ÀýÇÐȸ
Çѱ¹»ýÅÂÇÐȸ
Çѱ¹¼öÀÚ¿øÇÐȸ
Çѱ¹½Ä¹°ÇÐȸ
Çѱ¹½Ç³»µðÀÚÀÎÇÐȸ
Çѱ¹ÀÚ¿ø½Ä¹°ÇÐȸ
Çѱ¹ÀܵðÇÐȸ
Çѱ¹Á¶°æÇÐȸ
Çѱ¹Áö¹Ý°øÇÐȸ
Çѱ¹ÇÏõȣ¼öÇÐȸ
Çѱ¹È¯°æ»ý¹°ÇÐȸ
Çѱ¹È¯°æ»ýÅÂÇÐȸ

Çѱ¹¼öÀÚ¿øÇÐȸ / v.35, no.4, 2002³â, pp.453-461
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;
 
ÃÊ ·Ï
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.
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.
 
Ű¿öµå
ÁöÁøÇØÀÏ;ó¿À¸§;¹ü¶÷;ºñ¼±Çü õ¼ö¹æÁ¤½Ä;¹ü¶÷µµ;tsunami;run-up;inundation;nonlinear shallow-water equations;inundation map;
 
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
³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø
¸ñ·Ïº¸±â
ȸ»ç¼Ò°³ ±¤°í¾È³» ÀÌ¿ë¾à°ü °³ÀÎÁ¤º¸Ãë±Þ¹æÄ§ Ã¥ÀÓÀÇ ÇѰè¿Í ¹ýÀû°íÁö À̸ÞÀÏÁÖ¼Ò ¹«´Ü¼öÁý °ÅºÎ °í°´¼¾ÅÍ
   

ÇÏÀ§¹è³ÊÀ̵¿