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Çѱ¹¼öÀÚ¿øÇÐȸ / v.21, no.2, 1988³â, pp.183-192
µ¿Áö³ªÇØÀÇ ¼¼°ÝÀÚ 2Â÷¿ø $M_2$Á¶¼®¸ðÇü
( A fine grid two-dimensional $M_2$ tidal model of the East China Sea )
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À°ºØ»óÀÇ À¯µ¿Çö»óÀ» »ó¼¼ÇÏ°Ô ÇØ»ó½Ã۱â À§ÇØ ±â º¸°íµÈ µ¿Áö³ªÇØÀÇ 2Â÷¿ø ºñ¼±ÇüÁ¶¼®¸ðÇü(ÃÖ, 1980)À» À§µµ»ó 4ºÐ, °æµµ»ó 5ºÐÀÇ °ÝÀÚ°£°ÝÀ» °®´Â À¯ÇÑÂ÷ºÐ°ÝÀÚü°è·Î °³¼±½ÃÄ×´Ù. ¼ö¸³µÈ ¼¼°ÝÀÚ¸ðÇüÀº µ¿Áö³ªÇØÀÇ $M_2$ Á¶¼® ¹× $M_4$Á¶¼®À» ÀçÇö½Ã۴µ¥ ÀÏÂ÷ÀûÀ¸·Î ÀÌ¿ëµÇ¾ú´Âµ¥ »êÁ¤µÈ Á¶¼®Ã¼°èÀÇ ½Å·Ú¼ºÀº ¸ðÇü»êÁ¤Ä¡¿Í È²ÇØµ¿ÃøÀÇ Á¶¼®°üÃø °á°ú¿ÍÀÇ Àü¹ÝÀûÀÎ ÀÏÄ¡·Î¼­ ÀÔÁõµÇ¾ú´Ù. À°ºØÀüü¿¡ °ÉÄ£ ÇØÀúÃִ븶ÂûÀÀ·Â ¹× Á¶¼®Ç×·ùÀÇ ºÐÆ÷°¡ Á¦½ÃµÇ¾úÀ¸¸ç ¶ÇÇÑ ÅäÀǵǾú´Ù.
The previous two-dimensional non-linear tidal model of the East China Sea(Choi, 1980) has been further refined to resolve the flow over the ocntinental shelf in more detail. The mesh resolution of the present finite-difference grid system used is 4 minutes latitude by 5 minutes longitude over the entire shelf. The developed fine grid two-dimensional model was utilized to reproduce the $M_2$ tide and $M_4$ tide for the East China Sea contnental shelf. There is general agreement between the model results and the current observation made in the Eastern Yellow Sea, which supports the calculated tidal regime over the shelf. Some preliminary results on maximum bottom stress and tidally-induced residual current were also examined and discussed.
 
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Çѱ¹¼öÀÚ¿øÇÐȸÁö / v.21, no.2, 1988³â, pp.183-192
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1738-9488
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO198811920092340)
¾ð¾î : ¿µ¾î
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