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Çѱ¹¼öÀÚ¿øÇÐȸ / v.37, no.10, 2004³â, pp.823-836
À̵¿°­¿ì¿¡ ÀÇÇÑ À¯Ã⿵ÇâºÐ¼®
( Runoff Analysis due to the Moving Storm )
ÇѰǿ¬;Àü¹Î¿ì;ÃÖ±ÔÇö; °æºÏ´ëÇб³ Åä¸ñ°øÇаú;ÃæºÏ´ëÇб³ Åä¸ñ°øÇаú;°æºÏ´ëÇб³ Åä¸ñ°øÇаú;
 
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µÎ°³ÀÇ ÁöÇ¥¸é°ú ±× »çÀÌ¿¡ ÀÖ´Â Çϵµ·Î ÀÌ·ç¾îÁø À¯¿ªÀ» °¡Á¤ÇÏ¿© À̵¿°­¿ì¿¡ ´ëÇÑ À¯ÃâÀ» ¿îµ¿ÆÄ ÀÌ·ÐÀ» Àû¿ëÇϹǷμ­ ÇØ¼®ÇÏ¿© ´Ù¾çÇÑ °­¿ìÀ̵¿¼ÓµµÀÇ °æ¿ì¸¦ ºñ±³ ºÐ¼®ÇÏ¿´´Ù. À̵¿°­¿ì´Â ÇÏõÀÇ »ó·ù¹æÇâ, ÇÏ·ù¹æÇâ, Ⱦ¹æÇâÀ¸·Î 0.25¡­2.0m/sÀÇ ¼Óµµ·Î À̵¿½ÃÄ×À¸¸ç, À̶§ °­¿ìºÐÆ÷ÇüÀº ±ÕµîºÐÆ÷Çü, ÀüÁøÇü, Áö¿¬Çü, Áß¾ÓÁýÁßÇüÀ» Àû¿ëÇÏ¿´´Ù. Ⱦ¹æÇâ À̵¿°­¿ìÀÇ °æ¿ì¿¡ ÷µÎÀ¯·®ÀÌ °¡Àå Å©°Ô ³ªÅ¸³µ°í, »ó·ù¹æÇâÀÇ À̵¿°­¿ì¿¡ ´ëÇÑ Ã·µÎÀ¯·®ÀÌ °¡Àå ÀÛ°Ô ³ªÅ¸³µ´Ù. °­¿ìºÐÆ÷Çü¿¡ ´ëÇÑ À¯ÃâÀÇ ¹Î°¨µµ´Â °­¿ìÀ̵¿¼Óµµ°¡ ºü¸¦¼ö·Ï °¨¼ÒÇÏ¿´´Ù. °­¿ìÀ̵¿¼Óµµ°¡ ºü¸¦¼ö·Ï ÷µÎ½Ã°£ÀÌ »¡¶óÁö¸ç, ¼ö¹®°î¼±Àº ±Þ°ÝÈ÷ ¾ã¾ÆÁüÀ» ¾Ë ¼ö ÀÖ´Ù.
Using the simple geometry for the idealized catchment consisting of two plane surfaces and a stream between them, runoff was analysed for the moving storms based on the kinematic wave equation. The storm velocity applied in this study was 0.25¡­2.0 m/s moving up, down and cross direction of catchment. Applied rainfall distribution types are uniform, advanced, delayed, intermediate type. The results indicate that the moving storms of cross direction generate the largest peak runoff, and the smallest runoff appears in the case of up stream direction. The sensitivity of runoff to rainfall distribution types decreases as storm velocity increases. It is clear that faster storm velocity generates faster peak time and becomes thin hydrographs rapidly.
 
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À̵¿°­¿ì;°­¿ìºÐÆ÷Çü;¿îµ¿ÆÄ ¹æÁ¤½Ä;Ⱦ¹æÇâ;»ó·ù¹æÇâ;moving storm;rainfall distribution types;kinematic wave equation;cross direction;upstream direction;
 
Çѱ¹¼öÀÚ¿øÇÐȸ³í¹®Áý / v.37, no.10, 2004³â, pp.823-836
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1226-6280
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO200411922948756)
¾ð¾î : Çѱ¹¾î
³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø
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