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Çѱ¹¼öÀÚ¿øÇÐȸ / v.38, no.12, 2005³â, pp.1051-1060
·¹ÀÌ´õ ÃßÁ¤°­¿ìÀÇ ¼ö¹®ÇÐÀû Ȱ¿ë (II): ºÒÈ®½Ç¼º ÇØ¼®
( Hydrologic Utilization of Radar-Derived Rainfall (II) Uncertainty Analysis )
±èÁøÈÆ;À̰浵;¹è´öÈ¿; ¼¼Á¾´ëÇб³ Åä¸ñȯ°æ°øÇаú;(ÁÖ)À¥¼Ö·ç½º;¼¼Á¾´ëÇб³ ¹°ÀÚ¿ø¿¬±¸¼Ò Åä¸ñȯ°æ°øÇаú;
 
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º» ¿¬±¸¿¡¼­´Â °ü¾Ç»ê ·¹ÀÌ´õ ÀÚ·á·ÎºÎÅÍ ¼Ò¾ç°­ À¯¿ª¿¡¼­ ÃÖÀû ÃßÁ¤µÈ ·¹ÀÌ´õ °­¿ì·Î ÁØºÐÆ÷Çü TOPMODELÀÇ Àû¿ë¼ºÀ» Æò°¡Çϰí Monte Carlo³­¼ö¹ß»ý ±â¹ý°ú ¿¬°èÇÑ ¾Ó»óºí À¯·®¸ðÀÇ ±â¹ýÀ» ±¸ÃàÇÏ¿© ·¹ÀÌ´õ ÃßÁ¤°­¿ì°¡ °¡Áú ¼ö ÀÖ´Â ºÒÈ®½Ç¼ºÀÌ ¼ö¹®¸ðÇü¿¡ ¹ÌÄ¡´Â ¿µÇâÀ» ¸ðÇüÀÇ ¸Å°³º¯¼ö¿Í ¿¬°èÇÏ¿© ºÐ¼®ÇÏ¿´´Ù. ·¹ÀÌ´õ ÃßÁ¤°­¿ì¸¦ Ȱ¿ëÇÏ¿© ¼Ò¾ç°­ À¯¿ªÀÇ À¯·®°è»êÀ» 2003³â 7¿ùÀÇ »ç·Ê±â°£ µ¿¾È ¼öÇàÇÑ °á°ú ½Ç½Ã°£ ÆíÂ÷º¸Á¤ ±â¹ýÀ¸·Î ¼öÁ¤µÈ ·¹ÀÌ´õ ÀԷ°­¿ìÀÇ °æ¿ì °üÃøÀ¯·®°ú ºñ±³ÇÏ¿© ¸Å¿ì Àß ÀÏÄ¡ÇÏ´Â °ÍÀ¸·Î ³ªÅ¸³ª ·¹ÀÌ´õ ÃßÁ¤°­¿ìÀÇ ¼ö¹®ÇÐÀû Ȱ¿ë¼ºÀº ¸Å¿ì ³ôÀº °ÍÀ¸·Î ÆÇ´ÜµÈ´Ù. ºÒÈ®½Ç¼º ºÐ¼®¿¡¼­´Â ·¹ÀÌ´õ °­¿ì°¡ °¡Áú ¼ö ÀÖ´Â ºÒÈ®½Ç¼ºÀÌ ¼ö¹®¸ðÇüÀÇ ¸Å°³º¯¼ö ºÒÈ®½Ç¼ºº¸´Ù ´ú ¹Î°¨ÇÏ°Ô ¿µÇâÀ» ¹ÌÄ¡´Â °ÍÀ¸·Î °ËÅäµÇ¾ú°í ·¹ÀÌ´õ °­¿ì¿Í ¸Å°³º¯¼ö°¡ È¥ÇÕµÈ ºÒÈ®½Ç¼ºÀÌ À¯·®¸ðÀÇ¿¡¼­ °¡Àå Å« ¿ÀÂ÷¸¦ º¸ÀÏ ¼ö ÀÖ´Â °ÍÀ¸·Î °ËÅäµÇ¾ú´Ù.
The present study analyzes hydrologic utilization of optimal radar-derived rainfall by using semi-distributed TOPMODEL and evaluates the impacts of radar rainfall and model parametric uncertainty on a hydrologic model. Monte Carlo technique is used to produce the flow ensembles. The simulated flows from the corrected radar rainfalls with real-time bias adjustment scheme are well agreed to observed flows during 22-26 July 2003. It is shown that radar-derived rainfall is useful for simulating streamflow on a basin scale. These results are diagnose with which radar-rainfall Input and parametric uncertainty influence the character of the flow simulation uncertainty. The main conclusions for this uncertainty analysis are that the radar input uncertainty is less influent than the parametric one, and combined uncertainty with radar and Parametric input can be included the highest uncertainty on a streamflow simulation.
 
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·¹ÀÌ´õ ÃßÁ¤°­¿ì;ºÒÈ®½Ç¼º;ÁØºÐÆ÷Çü TOPMODEL;Monte Carlo ±â¹ý;¾Ó»óºí À¯·®;radar-derived rainfall;uncertainty;semi-distributed TOPMODEL;Monte Carlo technique;ensemble flow;
 
Çѱ¹¼öÀÚ¿øÇÐȸ³í¹®Áý / v.38, no.12, 2005³â, pp.1051-1060
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1226-6280
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO200508824142538)
¾ð¾î : Çѱ¹¾î
³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø
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ȸ»ç¼Ò°³ ±¤°í¾È³» ÀÌ¿ë¾à°ü °³ÀÎÁ¤º¸Ãë±Þ¹æÄ§ Ã¥ÀÓÀÇ ÇѰè¿Í ¹ýÀû°íÁö À̸ÞÀÏÁÖ¼Ò ¹«´Ü¼öÁý °ÅºÎ °í°´¼¾ÅÍ
   

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