¶óÆæÆ®¦¢Ä«Æä¦¢ºí·Î±×¦¢´õº¸±â
¾ÆÄ«µ¥¹Ì Ȩ ¸í»çƯ°­ ´ëÇבּ¸½Ç޹æ Á¶°æ½Ç¹« µ¿¿µ»ó°­ÀÇ Çѱ¹ÀÇ ÀüÅëÁ¤¿ø ÇÐȸº° ³í¹®
ÇÐȸº° ³í¹®

Çѱ¹°Ç¼³°ü¸®ÇÐȸ
Çѱ¹°ÇÃà½Ã°øÇÐȸ
Çѱ¹µµ·ÎÇÐȸ
Çѱ¹»ý¹°È¯°æÁ¶ÀýÇÐȸ
Çѱ¹»ýÅÂÇÐȸ
Çѱ¹¼öÀÚ¿øÇÐȸ
Çѱ¹½Ä¹°ÇÐȸ
Çѱ¹½Ç³»µðÀÚÀÎÇÐȸ
Çѱ¹ÀÚ¿ø½Ä¹°ÇÐȸ
Çѱ¹ÀܵðÇÐȸ
Çѱ¹Á¶°æÇÐȸ
Çѱ¹Áö¹Ý°øÇÐȸ
Çѱ¹ÇÏõȣ¼öÇÐȸ
Çѱ¹È¯°æ»ý¹°ÇÐȸ
Çѱ¹È¯°æ»ýÅÂÇÐȸ

Çѱ¹¼öÀÚ¿øÇÐȸ / v.23, no.1, 1990³â, pp.79-87
ÇÏõȫ¼ö·®ÀÇ Áö¿ªÈ­¸¦ À§ÇÑ ÀϹÝȭȸ±Í¸ðÇüÀÇ °³¹ß
( Development of Generalized Regression Model for Regionalization of River Floods )
Á¶±¹±¤;ÀÌÁøÇü; ¼ö¿øÀü¹®´ëÇÐ Åä¸ñ°ú;¼­¿ï´ëÇб³ ³ó°ú´ëÇÐ ³ó°øÇаú;
 
ÃÊ ·Ï
º» ¿¬±¸¿¡¼­´Â ȸ±Í¸ðÇüÀÇ ¿ÀÂ÷ºÐ¼®À» ¸ðÇü¿ÀÂ÷ºÐ¼®°ú Ç¥º»¿ÀÂ÷ºÐ»êÀ¸·Î ºÐ¸®ÇÏ¹Ç·Î½á ¿ÀÂ÷ºÐ»ê¿¡ ´ëÇÑ ÇÕ¸®ÀûÀÌ°íµµ ÆíÀǵÇÁö ¾ÊÀº ÃßÁ¤·®À» Á¦°øÇØ ÁÙ ¼ö ÀÖ´Â ÀϹÝÈ­ ÃÖ¼ÒÀڽ¹ýÀ» ÀÌ¿ëÇÏ¿© ÇѰ­ ¹× ³«µ¿°­À¯¿ªÀÇ À¯·®°üÃøÁ¡¿¡¼­ ¼öÁýµÈ ¿¬ÃÖ´ëÈ«¼ö·® ÀڷḦ À¯¿ªÆ¯¼º ¹× °­¿ì·® ÀÚ·á¿Í ¿¬°ü½ÃŰ´Â Áö¿ªÈ­È¸±Í¸ðÇüÀ» °³¹ßÇÏ¿´´Ù. º» ¸ðÇüÀº °èÃøÁöÁ¡À¸·ÎºÎÅÍ ¹Ì°èÃøÁöÁ¡À¸·Î ¼ö¹®Á¤º¸¸¦ Àü´ÞÇØÁÖ±â À§ÇÑ ¼ö´ÜÀ¸·Î »ç¿ëµÉ ¼ö ÀÖ´Ù.
In this study, a regression model, which relates annual flood peak flows collected at stramflow gaging stations in the Han river and Nakdong river basin to both basin characteristics and precipitation data, is developed by using the generalized least squares method which can provide reasonable and unbiased estimator of error variance by separating error variance of the regression model into that due to model error and due to sampling error. This model may be used as a mechanism for transferring hydrologic information from the gaged sites to ungaged sites.
 
Ű¿öµå
 
Çѱ¹¼öÀÚ¿øÇÐȸÁö / v.23, no.1, 1990³â, pp.79-87
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1738-9488
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO199011920093049)
¾ð¾î : Çѱ¹¾î
³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø
¸ñ·Ïº¸±â
ȸ»ç¼Ò°³ ±¤°í¾È³» ÀÌ¿ë¾à°ü °³ÀÎÁ¤º¸Ãë±Þ¹æÄ§ Ã¥ÀÓÀÇ ÇѰè¿Í ¹ýÀû°íÁö À̸ÞÀÏÁÖ¼Ò ¹«´Ü¼öÁý °ÅºÎ °í°´¼¾ÅÍ
   

ÇÏÀ§¹è³ÊÀ̵¿