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Çѱ¹¼öÀÚ¿øÇÐȸ / v.12, no.2, 1979³â, pp.56-62
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( A Determination of the Rainfall Durations of Various Recurrence Intervals )
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°­¿ìÀÚ·á·ÎºÎÅÍ ¼³°è È«¼ö·®À» ÃßÁ¤ÇÏ´Â ¸¹Àº ¹æ¹ýµéÀº ¼³°è°­¿ì·®ÀÇ Áö¼Ó±â°£ °áÁ¤¿¡ ¸Å¿ì º¹ÀâÇÑ ½ÃÇà Âø¿À¹ýÀ» »ç¿ëÇϰí ÀÖÀ¸³ª, º» ¿¬±¸¿¡¼­´Â ¼ø°£´ÜÀ§À¯·®µµ ÀÌ·ÐÀ» Àû¿ëÇÑ ÇØ¼®Àû ¹æ¹ý¿¡ ÀÇÇÏ¿© ±Ù»ç Áö¼Ó±â°£À» °áÁ¤ÇÏ´Â ¹æ¹ýÀ» ÀÌ·ÐÀûÀ¸·Î Àü°³ÇÏ¿´´Ù. ÀÌ·¸°Ô À¯µµµÈ ¹æ¹ýÀ» ¹«½Éõ ´ëÇ¥À¯¿ª¿¡ Àû¿ëÇÏ¿© ±³Á¡À¯·®ºñ°î¼±(hydrograph curve)°ú ÀçÇö±â°£º°·Î ¼³°è°­¿ì°î¼±(rainfall curve)À» °è»êÇϰí, ±× °á°ú¸¦ µ¿ÀÏ ÁÂÇ¥»ó¿¡ ±×·Á ±× ±³Á¡ÀÌ Ç¥½ÃÇÏ´Â À¯È¿¿ì·® Áö¼Ó±â°£À» °áÁ¤ÇÏ¿´´Ù.
Many methods of estimating design floods from rainfall data involve a trial and error procedure to determine the duration of the design rainfall, which is very complicated and time-consuming. In this study, an effort was given to derive an analytical expression for estimating the appropriate duration for use with a particular unit hydrograph. According to the so-derived analytical expression the coordinateds of hvdrograph curve and rainfall curve for the Musim Representative Basin were computed and then plotted on a same scal graph paper on which the critical durations of design rainfall excess of various recurrence intervals were determined by the point of intersection of the tow curves.
 
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Çѱ¹¼öÀÚ¿øÇÐȸÁö / v.12, no.2, 1979³â, pp.56-62
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1738-9488
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO197911920089580)
¾ð¾î : Çѱ¹¾î
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