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Çѱ¹¼öÀÚ¿øÇÐȸ / v.38, no.12, 2005³â, pp.1039-1049
·¹ÀÌ´õ ÃßÁ¤°­¿ìÀÇ ¼ö¹®ÇÐÀû Ȱ¿ë (I): ÃÖÀû ·¹ÀÌ´õ °­¿ì ÃßÁ¤
( Hydrologic Utilization of Radar-Derived Rainfall (I) Optimal Radar Rainfall Estimation )
¹è´öÈ¿;±èÁøÈÆ;À±¼º½É; ¼¼Á¾´ëÇб³ ¹°ÀÚ¿ø¿¬±¸¼Ò Åä¸ñȯ°æ°øÇаú;¼¼Á¾´ëÇб³ Åä¸ñȯ°æ°øÇаú;¼¼Á¾´ëÇб³ Åä¸ñȯ°æ°øÇаú;
 
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º» ¿¬±¸ÀÇ ¸ñÀûÀº ±â»ó ·¹ÀÌ´õÀÇ ¼ö¹®ÇÐÀû Ȱ¿ë¼ºÀ» ³ôÀ̰íÀÚ ÃÖÀûÀÇ ·¹ÀÌ´õ °­¿ì¸¦ ÃßÁ¤Çϱâ À§ÇØ °ü¾Ç»ê ·¹ÀÌ´õ ÀڷḦ ´ë»óÀ¸·Î POD ºÐ¼®±â¹ýÀ» Ȱ¿ëÇÏ¿© ÁöÇüŬ·¯ÅÍ ¹× ºö Â÷Æó¿µ¿ª µîÀ» Á¦°ÅÇϰí Marshall-PalmerÀÇ Z-R °ü°è½ÄÀ¸·Î ·¹ÀÌ´õ °­¿ì¸¦ ÃßÁ¤ÇÑ °á°ú °­¿ì°è °üÃø°­¿ì¿Í ºñ±³ÇÏ¿© ½Ã$cdot$°ø°£ÀûÀ¸·Î °ú¼Ò ¸ðÀÇÇÏ´Â °ÍÀ¸·Î ³ªÅ¸³µ´Ù. ÀÌ·¯ÇÑ °á°ú¸¦ ¹ÙÅÁÀ¸·Î °­¿ì°è °üÃø°­¿ì¿ÍÀÇ ½Ç½Ã°£ º¸Á¤±â¹ýÀ» ¼Ò¾ç°­ À¯¿ªÀ» ´ë»óÀ¸·Î Àû¿ëÇÑ °á°ú Æò±Õ G/R °ªÀº $0.95~1.32$·Î ÀûÁ¤ºÐÆ÷¸¦ º¸ÀÌ°í Æò±ÕÆíÂ÷´Â $9~28%$ ¹üÀ§·Î °¨¼ÒµÇ¾î ºÒÈ®½Ç¼º ¶ÇÇÑ °¨¼ÒÇÏ´Â °ÍÀ¸·Î ³ªÅ¸³µ´Ù. ÇÑÆí, ÆíÂ÷°¡ º¸Á¤µÈ ÃÖÀû ·¹ÀÌ´õ ÃßÁ¤°­¿ì·Î ¼Ò¾ç°­ À¯¿ªÆò±Õ °­¿ì·®À» »êÁ¤ÇÑ °á°ú °üÃø°­¿ì¿Í ºñ±³ÇÏ¿© ¸Å¿ì Àß ÀÏÄ¡ÇÏ´Â °ÍÀ¸·Î ³ªÅ¸³µ´Ù. µû¶ó¼­ ½Ç½Ã°£ ÆíÂ÷º¸Á¤ ±â¹ýÀº ¼ö¹®ÇÐÀû À¯¿ªÆò±Õ °­¿ì·® »êÁ¤½Ã ´Ù¼Ò °ú¼ÒÃßÁ¤µÇ´Â ·¹ÀÌ´õ °­¿ìÁ¤º¸¸¦ Á¤È®ÇÏ°Ô º¸Á¤ÇÒ ¼ö ÀÖ´Ù´Â Ãø¸é¿¡¼­ ±× Àû¿ë¼ºÀÌ ¿ì¼öÇÑ °ÍÀ¸·Î ÆÇ´ÜµÈ´Ù.
The objective of this study is to produce optimal radar-derived rainfall for hydrologic utilization. The ground clutter and beam blockage effects from Mt. Kwanak station (E.L 608m) are removed from radar reflectivities by POD analysis. The reflectivities are used to produce radar rainfall data in the form of rain rates (mm/h) by the application of the Marshall-Palmer reflectivity versus rainfall relationship. However, these radar-derived rainfall are underestimated in temporal and spatial scale compared with observed one, so it is necessary to hire a correction scheme based on the gauge-to-radar (G/R) statistical adjustment technique. The selected watershed for studying the real-time correction of radar-rainfall estimation is the Soyang dam site, which is located approximately 100km east of Kwanak radar station. The results indicate that adjusted radar rainfall with the gauge measurement have reasonal G/R ratio ranged on 0.95-1.32 and less uncertainty with that mean standard deviation of G/R ratio are decreased by $9-28%$. Mean areal precipitation from adjusted radar rainfall are well agreed to the observed one on the Soyang River watershed. It is concluded that the real-time bias adjustment scheme is useful to estimate accurate basin-based radar rainfall for hydrologic application.
 
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·¹ÀÌ´õ °­¿ì;POD ºÐ¼®;Z-R °ü°è½Ä;ÆíÂ÷º¸Á¤;°ü¾Ç»ê ·¹ÀÌ´õ;radar rainfall;POD analysis;Z-R relationship;bias adjustment;Mt. Kwanak radar;
 
Çѱ¹¼öÀÚ¿øÇÐȸ³í¹®Áý / v.38, no.12, 2005³â, pp.1039-1049
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1226-6280
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO200508824142533)
¾ð¾î : Çѱ¹¾î
³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø
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