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Çѱ¹¼öÀÚ¿øÇÐȸ / v.35, no.5, 2002³â, pp.31-43

( ANALYSIS OF FLOW RESPONSE CHANCE ON A DAM CATCHMENT DUE TO GLOBAL WARMING )
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º» ¿¬±¸¿¡¼­´Â ¿Â³­È­¿¡ ÀÇÇÑ ÇÏõÀ¯¿ªÀÇ ¼ö¹®ÀÀ´ä(°­¿ìÀ¯Ãâ, ƯÈ÷ ÀÏ´ÜÀ§ÀÇ À¯È²)ÀÇ º¯È­¾ç»óÀ» ¼öÄ¡½ÇÇèÀ» ÅëÇØ Á¤·®ÀûÀ¸·Î Æò°¡ÇÏ¿´´Ù. ÀÌ»êȭź¼Ò ³óµµÀÇ Áõ°¡¿¡ µû¸¥ ¿Â³­È­ÀÇ ÁøÇàÀ¸·Î ¾ß±âµÇ´Â ¼ö¹®ÇÐÀû Æò°¡´Â ¸¹Àº °üÃøÀڷḦ ÇÊ¿ä·Î Çϸç À̸¦ Á¤·®ÀûÀ¸·Î Æò°¡ÇÑ´Ù´Â °ÍÀº ´ë´ÜÈ÷ ¾î·Á¿î ÀÏÀÌ´Ù. µû¶ó¼­ Àå·¡ÀÇ ±âÈĸ¦ ¿¹ÃøÇÏ´Â ¼ö´ÜÀ¸·Î¼­ ÀûÁ¤ÇÑ ½Ã³ª¸®¿À¸¦ »óÁ¤ÇÏ¿© ÆòÇÏ´Â ¹æ¹ýÀ» »ý°¢ÇÒ ¼ö ÀÖ´Ù. º» ¿¬±¸¿¡¼­´Â ¿©·¯ °¡Áö »óÁ¤ÇÒ ¼ö ÀÖ´Â ½Ã³ª¸®¿À Áß ±â¿ÂÀº $0^{circ}C$¿¡¼­ $4.0^{circ}C$±îÁö º¯È­ÇÏ¸ç °­¼ö·®Àº 15%±îÁö Áõ°¨ÇÒ ¼ö ÀÖ´Ù´Â ½Ã³ª¸®¿À¸¦ »óÁ¤ÇÏ¿© ºÒÈ®½Ç¼ºÀÌ Å« Áö±¸¿Â³­È­ÀÇ ¹®Á¦¿¡ ´ëÇÏ¿© °£´ÜÇϸ鼭 ¸íÈ®ÇÑ °¡Á¤À» µµÀÔÇÏ¿´´Ù. µû¶ó¼­, ´ë»óÀ¯¿ªÀÎ ¾Èµ¿´ï À¯¿ª¿¡ ´ëÇÑ Àå·¡ÀÇ ÇÏõÀ¯·®Àº ±âÈĺ¯È­ ½Ã³ª¸®¿À¿¡¼­ ¾ß±âµÇ´Â °­¼ö·®À» ¹ß»ý½ÃÄÑ ÅÊÅ©¸ðÇü¿¡ ÀÇÇÏ¿© ÀÏ À¯·®À» ¸ðÀÇ ¹ß»ýÇÏ°Ô µÈ´Ù. º» ¿¬±¸¿¡¼­´Â 2030³âÀ» ÀÌ»êȭź¼Ò ³óµµ°¡ ¹èÁõµÇ´Â ½ÃÁ¡ ($2{ imes}CO2$), 2010³â, 2020³â ¹× 2050³âÀ» °¢°¢ ($1.5{ imes}CO2$),($1.75{ imes}CO2$) ¹× ($2.5{ imes}CO2$)·Î ¼³Á¤ÇÏ¿´À¸¸ç, ÀÌ ½Ã±â¿¡ ´ëÇÑ ÇÏõ À¯È²ÀÇ ÇØ¼® ¹× ¿Â³­È­°¡ ¹ß»ýµÇÁö ¾Ê¾ÒÀ» ¶§¿ÍÀÇ ºñ±³ °ËÅ並 ½Ç½ÃÇÏ¿´´Ù.
This study describes results of numerical simulations on river flow response due to global warming. Forecasts of changes in climatic conditions are required to estimate the hydrologic effects of increasing trace gas concentratrions in the atmosphere. However, reliable forecasts of regional climate change are unavailable. In there absense various approaches to the development of scenarios of furture climatic conditions are used. The approach in this study is to prescribe climatic changes for a river basin in a simplified manner. As a rule, such scenarios apecify air temperature increases from $0^{circ}C$ to $4.0^{circ}C$ and precipitation change (increase or decrease) in the range of 0% to 15%. On the basis of acceptable supposition of warming scenarios, furute daily stream flow is simulated using rainfall-runoff model in the Andong Dam basin. The numerical experiments have quantitatively revealed the change of discharge at 2010, 2020, 2030 and 1050 for each warming scenarios and compared it with the results for a non-worming scenario.
 
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Çѱ¹¼öÀÚ¿øÇÐȸÁö / v.35, no.5, 2002³â, pp.31-43
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1738-9488
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO200211922046552)
¾ð¾î : ¿µ¾î
³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø
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