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Çѱ¹¼öÀÚ¿øÇÐȸ / v.33, no.5, 2000³â, pp.623-634
±âÈĺ¯È­ ½Ã³ª¸®¿À¿¡ ÀÇÇÑ ÇÏõ À¯È²ÀÇ ÇØ¼®
( Analysis of River Flow Change Based on Some Scenarios of Global Warming )
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¿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¿© Æò°¡ÇÏ´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¸¦ °¡Á¤ÇÏ¿© ºÒÈ®½Ç¼ºÀÌ Å« Áö±¸¿Â³­È­ÀÇ ¹®Á¦¿¡ ´ëÇÏ¿© °£´ÜÇϸ鼭 ¸íÈ®ÇÑ °¡Á¤À» µµÀÔÇÏ¿´´Ù. µû¶ó¼­, ´ë»ó À¯¿ªÀÎ ¾Èµ¿´ï À¯¿ª¿¡ ´ëÇÑ Àå·¡ÀÇ ÇÏõ À¯·®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¡($2{ imes}CO_2$), 2010³â, 2050³âÀ» °¢°¢ $(1.5{ imes}CO_2),;(1.75{ imes}CO_2),;(2.5{ imes}CO_2)$·Î ¼³Á¤ÇÏ¿´À¸¸ç, ÀÌ ½Ã±â¿¡ ´ëÇÑ ÇÏõÀ¯È­ÀÇ 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 concentrations in the atmosphere. However, reliable forecasts of regional climate change are unavailable. In there absence, various approaches to the development of scenarios of future 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 specify 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. future daily streamflow 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 2050 for each warming scenarios and compared it with the results for a non-warmmg scenano.cenano.
 
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¿Â³­È­;¿Â³­È­½Ã³ª¸®¿À;ÇÏõÀ¯È²;¾Èµ¿´ï À¯¿ª;global wanning;wanning scenario;river flow;Andong Dam basin;
 
Çѱ¹¼öÀÚ¿øÇÐȸ³í¹®Áý / v.33, no.5, 2000³â, pp.623-634
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1226-6280
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO200011920730571)
¾ð¾î : Çѱ¹¾î
³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø
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