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Çѱ¹¼öÀÚ¿øÇÐȸ / v.14, no.3, 1981³â, pp.47-54
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Çѱ¹ÁÖ¿äÁöÁ¡¿¡ ´ëÇÑ È®·ü°¿ì·®°ú °üÃøÃÖ´ë°¿ì·®ÀÇ È®·üºÐ¼®
( Probability Characteristics of Probable Rainfall and Recorded Maximum Rainfall in Korea. ) |
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| ¿ì¸®³ª¶óÀÇ ÁÖ¿ä µµ½Ã ¼¿ï, ºÎ»ê, ´ë±¸, ±¤ÁÖÀÇ ÁöÁ¡°¿ì·®¿¡ ´ëÇÏ¿© È®·üÀûÀÎ ¹æ¹ý°ú M³â ÃÖ´ëÄ¡¹ý¿¡ ÀÇÇÏ¿© ±× Ư¼ºÀÌ ÇØ¼®µÇ¾úÀ¸¸ç ÀϺ»ÀÇ ÇØ¼®°á°ú¿Íµµ ºñ±³µÇ¾ú´Ù. º» ¿¬±¸¿¡¼ ¾ò¾îÁø °á°ú´Â ´ÙÀ½°ú °°´Ù. T³âÈ®·ü°¿ì°¡ N³â µ¿¾È¿¡ ¹ß»ýÇÏÁö ¾ÊÀº È®·üÀº °üÃøÄ¡·ÎºÎÅÍ ºÐ¼®µÈ °ª°ú ºñ±³ÇÏ¿© º¼ ¶§ ÀÌ·ÐÄ¡º¸´Ù ÀÛ¾ÒÀ¸¸ç ÀϺ»ÀÇ °á°úº¸´Ù´Â ÄÇ´Ù. M³â 10ºÐ ÃÖ´ëÄ¡°¡ N³â µ¿¾È¿¡ ¹ß»ýÇÏÁö ¾ÊÀº È®·üÀÇ Æò±ÕÄ¡´Â ÀÌ·ÐÄ¡º¸´Ù ÄÇÀ¸¸ç M³â 1½Ã°£ ÃÖ´ëÄ¡´Â ÀÌ·ÐÄ¡º¸´Ù ÀÛ¾Ò°í M³â 1ÀÏ ÃÖ´ëÄ¡´Â ÀÌ·ÐÄ¡¿Í °ÅÀÇ ÀÏÄ¡ÇßÀ¸¸ç ÀϺ»ÀÇ °æ¿ì´Â ÀÌ·ÐÄ¡º¸´Ù ÀÛ¾Ò´Ù. »ó±â °á°ú¿¡ ÀÇÇÏ¿© È®·üÀûÀÎ ¸é¿¡¼ º»´Ù¸é M³â Ãִ밿츦 ¼³°è·®À¸·Î ÅÃÇÏ´Â °ÍÀÌ T³â È®·ü°¿ìº¸´Ù ¾ÈÀüÃøÀ̶ó°í »ý°¢µÈ´Ù. |
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| The characteristics of point rainfall for three different durations in Seoul Pusan Taegu and Gwangju have been analysed by the probabilistic ainfall method and the M-year maximum rainfall method. The probabilities that the T-year probabilistic rainfall did not occur during the observation period, compared with the values obtained from the observed data. were smaller than the theoretical values. The averages of the probabilities that the M-year maximum-ten-minute rainfall did not occur in the consequent N-years were larger than the theoretical values, the M-year maximumone hour rainfall were smaller than the theoretical ones, and the M-year maximum daily rainfall nearly agreed with them, and while those of Japan were smaller than the theoretical values. It is recommended from the results that the recorded maximum value should be used as a design value rather than the probabilistic rainfall. |
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Çѱ¹¼öÀÚ¿øÇÐȸÁö / v.14, no.3, 1981³â, pp.47-54
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1738-9488
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO198111920090177)
¾ð¾î : Çѱ¹¾î |
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| ³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø |
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