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Çѱ¹¼öÀÚ¿øÇÐȸ / v.43, no.8, 2010³â, pp.757-767
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È®·ü°¿ì·®ÀÇ °ø°£ºÐÆ÷ ÃßÁ¤À» À§ÇÑ KED ±â¹ýÀÇ Àû¿ë
( Application of KED Method for Estimation of Spatial Distribution of Probability Rainfall ) |
| ¼¿µ¹Î;¿©¿î±â;À̽ÂÀ±;ÁöÈ«±â; ¿µ³²´ëÇб³ °Ç¼³½Ã½ºÅÛ°øÇаú;¿µ³²´ëÇб³ °Ç¼³½Ã½ºÅÛ°øÇаú;Çѱ¹¼öÀÚ¿ø°ø»ç, K-water ¼öÀÚ¿ø¿¬±¸¿ø;¿µ³²´ëÇб³ °Ç¼³½Ã½ºÅÛ°øÇаú;
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| º» ¿¬±¸´Â È®·ü°¿ì·®¿¡ ´ëÇÑ °ø°£ºÐÆ÷ ÃßÁ¤½Ã ½Å·Úµµ¸¦ Çâ»ó½Ã۴µ¥ ÀÖ¾î¼ ¿ÜºÎº¯¼ö »ç¿ëÀÇ À¯È¿¼ºÀ» Æò°¡Çϱâ À§ÇÏ¿© È®·ü°¿ì·®°ú ´ÜÀÏ º¸Á¶º¯¼ö·Î¼ ÁöÇüƯ¼ºÀÎÀÚµé°úÀÇ »ó°ü°ü°è¸¦ °í·ÁÇÑ KED ±â¹ýÀ» Àû¿ëÇÏ¿´À¸¸ç, ±× °á°ú °¿ì°ø°£ºÐÆ÷ ¹× À¯¿ªÆò±Õ°¿ì·®ÀÇ ÃßÁ¤¿¡ ÀÖ¾î¼ È®Á¤·ÐÀû °ø°£º¸°£±â¹ý ¹× Å©¸®Â¡ ±â¹ý°ú ´ëü·Î ºñ½ÁÇÑ °á°ú¸¦ ³ªÅ¸³»´Â °ÍÀ¸·Î ºÐ¼®µÇ¾úÀ¸¸ç, KED ¹× Å©¸®Â¡ ±â¹ý¿¡ ´ëÇÑ ±³Â÷°ËÁõ °á°ú º¸Á¶º¯¼ö·Î¼ Ç¥°í¸¦ »ç¿ëÇÑ KED ±â¹ýÀÌ °¡Àå ÁÁÀº °á°ú¸¦ ³ªÅ¸³»°í´Â ÀÖÀ¸³ª ´Ù¸¥ ±â¹ýµé°ú ºñ±³ÇßÀ» ¶§ Å« Â÷À̸¦ º¸ÀÌÁö ¾Ê´Â °ÍÀ¸·Î ºÐ¼®µÇ¾ú´Ù. |
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| This study employs the KED method using the correlations between probability rainfall and topographical factors as single auxiliary variable for assessing the effectiveness of external variables to improve the reliability in the estimation of spatial distribution of probability rainfall. As a result, the KED method gives similar results compared with deterministic spatial interpolation methods and kriging methods in the estimation of rainfall spatial distribution and mean areal rainfall, and as a result of the cross-validations of KED and kriging methods, the KED method using terrain elevation as auxiliary variable gives the best results, which are not significantly different in comparisons with other methods. |
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| Ű¿öµå |
| È®·ü°¿ì·®;°ø°£ºÐÆ÷;ÁöÇüƯ¼ºÀÎÀÚ;Å©¸®±ë;probability rainfall;spatial distribution;topographic factor;KED;kriging; |
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Çѱ¹¼öÀÚ¿øÇÐȸ³í¹®Áý / v.43, no.8, 2010³â, pp.757-767
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1226-6280
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO201025240675837)
¾ð¾î : Çѱ¹¾î |
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| ³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø |
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