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Çѱ¹¼öÀÚ¿øÇÐȸ / v.36, no.1, 2003³â, pp.13-21
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·¹ÀÌ´õ ¹Ý»ç°µµ¿Í °¿ì°µµÀÇ Z-R °ü°è½Ä »êÁ¤
( Estimation of Z-R Relationships between Radar Reflectivity and Rainfall rate ) |
| ¾È»óÁø;±èÁø±Ø; ÃæºÏ´ëÇб³ Åä¸ñ°øÇаú;ÃæºÏ´ëÇб³ ´ëÇпø Åä¸ñ°øÇаú;
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| º» ¿¬±¸´Â ¸ñÀûÀº ·¹ÀÌ´õ ÀÚ·áÀÇ È°¿ëÀ» À§ÇØ ·¹ÀÌ´õ ¹Ý»ç°µµ¿Í °¿ì°µµ »çÀÌÀÇ ·¹ÀÌ´õ °ü°è½ÄÀ» »êÁ¤ÇÏ´Â °ÍÀÌ´Ù. Z-R °ü°è½Ä¸¦ »êÁ¤Çϱâ À§ÇØ ÃæÁÖ´ï À¯¿ªÀÇ ¼öÀ§Ç¥ÁöÁ¡Áß ¿µÃá ¼öÀ§Ç¥ ÁöÁ¡ÀÇ À¯Ãâ·®ÀÌ 1,000~8.519§©/secÀÎ °¿ì»ç»óÀ» ¼±Á¤ÇÏ¿© Z-R ¹æÁ¤½ÄÀ» »êÁ¤ÇÏ¿´´Ù. 32°³ÀÇ °¿ì·® °üÃø¼Ò¿¡¼ A: 26.4~37.4, $eta$=0.97~l.56.ÀÇ ¹üÀ§³»¿¡ ºÐÆ÷ÇÔÀ» ¾Ë ¼ö ÀÖ¾ú´Ù. »êÁ¤µÈ Z-R ¹æÁ¤½ÄÀÇ »ó°ü°è¼ö´Â 0.63~0.748¹üÀ§À̸ç, Z=200Rl.6½ÄÀÇ »ó°ü°è¼ö´Â 0.63·Î ÁöÁ¡º° Z-R ¹æÁ¤½ÄÀÇ »ó°ü°è¼öº¸´Ù ³·Àº »ó°ü¼ºÀ» º¸À̰í ÀÖ´Ù. |
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| The purpose of this study is to estimate Z-R relationships of between radar reflectivity and rainfall rate. The Z-R relationships estimated that rainfall events are selected at Yeongchun water level station where the discharge recorded from 1,000cms to 8,519cms in chungju dam basin. The result of Z-R relationship distributed at thirty two raingage sites, the constant values of A and $eta$ are distributed between 26.4 and 7.4, 0.9 and 1.56 respectively. The correlation coefficients of standard Z-R relationships(Z=200Rl.6)shows that 0.63 lower than each other raingage sites(0.65~0.748). |
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| ·¹ÀÌ´õ;·¹ÀÌ´õ ¹æÁ¤½Ä(Z-R);Radar;Z-R relationship; |
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Çѱ¹¼öÀÚ¿øÇÐȸ³í¹®Áý / v.36, no.1, 2003³â, pp.13-21
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1226-6280
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO200311921555605)
¾ð¾î : Çѱ¹¾î |
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| ³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø |
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