¶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.33, no.3, 2000³â, pp.375-382
ÇѰæÀ¯¿ª¿¡¼­ÀÇ °Ç±â¿Í ¿ì±âÀÇ º¯À̱Ⱓ ºÐ¼®
( An Analysis of the Transition Time between Dry and Wet Period in the Han River Basin )
ÀÌÀç¼ö; ÀüÁÖ´ëÇб³ Åä¸ñȯ°æ°øÇаú;
 
ÃÊ ·Ï
´ëÀ¯¿ªÀÇ ÁöÇ¥¸é ¼ö¹®Çö»óÀº Ãß°èÇÐÀû º¯µ¿¿¡ ÀÇÇØ ¾ß±âµÇ´Â ¾ÈÁ¤µÈ »óÅÂÀÇ º¯ÀÌ¿Í ÇÔ²² ¸î °³ÀÇ ¹ß»ýºóµµ°¡ ³ôÀº ¾ÈÁ¤µÈ »óÅÂÀÇ ¿µÇâÀ» ¹Þ±â°¡ ½¬¿îµ¥ ±× ÀÌÀ¯´Â ÁöÇ¥¸é°ú ´ë±â »óÈ£°ü°èÀÇ ¹ÐÁ¢ÇÑ Á¶ÇÕ°úµµ °ü°è°¡ ÀÖ´Ù. µû¶ó¼­ °¢ ¾ÈÁ¤»óÅ¿¡¼­ÀÇ Ã¼·ù±â°£ Áï, °¡¹³±â³ª È«¼ö±âÀÇ Áö¼Ó±â°£ÀÌ Áß¿äÇÑ ¿¬±¸ °úÁ¦¶ó ÇÒ ¼ö ÀÖÀ¸¸ç º» ¿¬±¸¿¡¼­´Â ÇѰ­À¯¿ª¿¡ ´ëÇÏ¿© ¾ÈÁ¤»óÅÂÀÇ Æò±Õ º¯À̱ⰣÀ» ºÐ¼®ÇÏ¿´´Ù. ºñ¼±Çü ¹°¼öÁö¸ðÇüÀ» ÇѰ­ À¯¿ª¿¡ ´ëÇÏ¿© °ú°ÅÀÇ ÀڷḦ ¹ÙÅÁÀ¸·Î °ËÁ¤ÇÏ¿´°í ¸ðÇüÀ» ÅëÇÑ ¹°¸®°úÁ¤ÀÇ Ãß°èÇÐÀû Ç¥Çö°ú »êÁ¤µÈ ¸ðÇüº¯¼öµé·ÎºÎÅÍ ¾ÈÁ¤»óÅ»çÀÌÀÇ Æò±Õ º¯À̱ⰣÀÌ °è»êµÇ¾ú´Ù. º» ¿¬±¸´Â ¾ÈÁ¤»óÅ »çÀÌÀÇ º¯À̱Ⱓ ȤÀº °ÅÁֱⰣ, Áï ½Ã½ºÅÛÀÌ ÁÖ¾îÁø ¾ÈÁ¤»óÅ¿¡ ¸Ó¹«´Â ±â°£(°¡¹³À̳ª È«¼ö»óÅÂÀÇ Áö¼Ó±â°£)ÀÇ ¿¹Ãø°ú ¹ÐÁ¢ÇÑ °ü°è°¡ ÀÖ´Ù.
The surface hydrology of large watershed is susceptible to several preferred stable states with transitions between stable states induced by stochastic fluctuations. This comes about due to the close coupling of land surface and atmospheric interaction. An interesting and important issue is the duration of residence in each mode. In this study, mean transition tunes between the stable modes are analyzed for the Han River Basin. On the basis of historical data, the nonlinear water balance model is calibrated for the Han River Basin. The transition times between the stable modes in the model are studied based on the stochastic representation of the physical processes and on the calibrated model parameters. This study has implications for prediction of the transition time between stable modes or residence times, that is, the time the system spends in a given stable modes, since this would be equivalent to predicting the duration of drought or wet conditions.
 
Ű¿öµå
º¯À̱Ⱓ;ÁöÇ¥-´ë±â»óÈ£°ü°è;ºñ¼±Çü¹°¼öÁö¸ðÇü;ÇÔ¼öºñ;±³Â÷ ÀÌ·Ð;transition time;land sueface-atmospheric interaction;non-linear water balance model;soil moisture content;crossing theory;
 
Çѱ¹¼öÀÚ¿øÇÐȸ³í¹®Áý / v.33, no.3, 2000³â, pp.375-382
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1226-6280
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO200011920063747)
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¿