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Çѱ¹¼öÀÚ¿øÇÐȸ / v.20, no.2, 1987³â, pp.151-160
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ÇѰ°¨Á¶±¸°£ÀÇ Á¶¼®ÀüÆÄ
( Tidal Propagation in the Han River ) |
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| ÇѰÇÏ·ùºÎ °¨Á¶±¸°£ÀÇ Á¶¼®ºñ´ëĪÇö»óÀÇ ¹ß´Þ°úÁ¤ ¹× ÇÏõÀ¯Ãâ¼öÀÇ Á¶¼®ÀüÆÄ¿¡ÀÇ ¿µÇâÀÌ 1Â÷¿ø ¹æÁ¤½ÄÀÇ ¼öÄ¡ÀûºÐ¹ý¿¡ ÀÇÇØ Á¤·®ÀûÀ¸·Î Á¶»çµÇ¾ú´Ù. ¸ðµ¨ °á°ú´Â $,$,$ ºÐÁ¶¸¦ Æ÷ÇÔÇÏ´Â ÀϺκÐÁ¶µéÀÇ ÁøÆøÀÌ ÀϺÎÇÏõ±¸°£¿¡¼ È®ÆøµÇ´Â °ÍÀ» Á¦½ÃÇÏ¿´´Ù. Áõ°¡µÇ´Â ÇÏõÀ¯Ãâ¼öÀÇ Á¶¼®¿¡ ´ëÇÑ ¿µÇâÀ» »êÁ¤ÇÑ °á°ú´Â ÀÌ·ÐÀûÀÎ Ãß·Ð(Godin, 1985)°úµµ ÀÏÄ¡ÇÏ´Â °á°ú¸¦ °¡Á³´Ù. |
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| The development of the tidal asymmetries and the effect of an increased discharge on tide propagating into the Han River was studied quantitatively via numerical integration of one-demensional equations. The model results indicated that some tidal components including $, $, $ were actually be amplified over a segment of the river. The computed results on the effects of increased discharges on the tide were in good agreement with theoretical inference(Godin, 1985). |
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Çѱ¹¼öÀÚ¿øÇÐȸÁö / v.20, no.2, 1987³â, pp.151-160
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1738-9488
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO198711920091905)
¾ð¾î : Çѱ¹¾î |
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| ³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø |
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