|
|
Çѱ¹¼öÀÚ¿øÇÐȸ / v.44, no.8, 2011³â, pp.683-694
|
±âÈĺ¯È¿¡ µû¸¥ ¿ì¸®³ª¶ó °¼öÈ¿À² ¹× À¯Ãâ·®ÀÇ º¯ÈƯ¼º ºÐ¼®
( The Impact of Climate Change on the Trends of Precipitation Effectiveness Ratio and Runoff Data in South Korea ) |
±èÁ¾ÇÊ;±è±¤¼·; °æºÏ´ëÇб³ °ø°ú´ëÇÐ °ÇÃàÅä¸ñ°øÇкÎ;°æºÏ´ëÇб³ °ø°ú´ëÇÐ °ÇÃàÅä¸ñ°øÇкÎ;
|
|
|
 |
|
|
ÃÊ ·Ï |
±âÈĺ¯È¿¡ µû¸¥ Áö¿ªÀû ¿µÇâÀÎ ±â¿Â »ó½Â°ú °¼ö·® º¯È·Î ÀÎÇÑ ¼öÀÚ¿ø º¯È Ư¼ºÀ» ÆÄ¾ÇÇϱâ À§ÇÏ¿© ±â»óû(KMA)À¸·ÎºÎÅÍ Àü±¹ 59°³ °üÃøÁöÁ¡¿¡ ´ëÇØ¼ 1973³âºÎÅÍ 2009³â±îÁö °¼ö·® ¹× ±â¿ÂÀڷḦ ÀÌ¿ëÇÏ¿© »êÁ¤ÇÑ °¼öÈ¿À²ÀÚ·á¿Í ±¹°¡¼öÀÚ¿ø°ü¸®Á¾ÇսýºÅÛ(WAMIS)À¸·ÎºÎÅÍ 1966³âºÎÅÍ 2007³â±îÁö PRMS ¸ðÀÇ À¯Ãâ·® ÀڷḦ ¼öÁý, ºÐ¼®ÇÏ¿´´Ù. ºÐ¼®°á°ú, Àü¹ÝÀûÀ¸·Î °¼öÈ¿À²ÀÇ °Åµ¿Àº °¼ö·®ÀÇ º¯È Ư¼ºÀ» µû¸£³ª Áö¿ªÀûÀ¸·Î °¼ö·®ÀÌ Áõ°¡ÇÔ¿¡µµ ºÒ±¸ÇÏ°í ±â¿Â »ó½Â¿¡ µû¶ó °¼öÈ¿À²ÀÌ °¨¼ÒÇÏ´Â °Åµ¿À» º¸¿´À¸¸ç, ÀÌ´Â À¯Ãâ·®ÀÇ º¯È Ư¼º°ú À¯»çÇÏ¿´´Ù. ¶ÇÇÑ À¯Ãâ·®ÀÇ Æò±Õ´ëºñ º¯ÈÀ²Àº °¼ö·® º¯Èº¸´Ù »ó´çÈ÷ Å©°Ô ³ªÅ¸³ª, ±âÈĺ¯ÈÀÇ ¿µÇâ¿¡ ¹Î°¨ÇÑ °ÍÀ¸·Î ³ªÅ¸³µ´Ù. °¼ö·®ÀÌ Áõ°¡ÇÏ´Â 5¿ù~9¿ùÀ» Á¦¿ÜÇÑ Àüü ±â°£¿¡ ´ëÇÏ¿© °¼öÈ¿À²Àº °¼ö·®º¸´Ù ´õ À¯ÀÇÇÑ °¨¼Ò °æÇâÀ» ³ªÅ¸³»°í ÀÖ¾î ÇØ´ç±â°£ÀÇ °¡¿ë ¼öÀÚ¿ø·®ÀÌ ÁÙ¾îµé °ÍÀ¸·Î ÆÇ´ÜµÇ¸ç, ÀÌ·¯ÇÑ Æ¯¼ºÀº º½, °¡À» ¹× °Ü¿ïö ¼öÀÚ¿ø °ü¸®¿¡ ¹Ý¿µµÇ¾î¾ß ÇÒ °ÍÀÌ´Ù. |
|
To analyze the regional impact of air temperature increase and precipitation variation on water resources, the variability of precipitation-effectiveness (P-E) ratio which is estimated using precipitation and air temperature data of 59 weather stations operated by the Korean Meteorological Administration (KMA) during 1973~2009 was analyzed. Also runoff data resulting from the Precipitation-Runoff Modelling System (PRMS) modelling were analyzed during 1966~2007. The overall spatio-temporal variability of P-E ratio and runoff data in South Korea is corresponding to the variability of precipitation amount. However some region shows that the P-E ratio decreases even though the trend of precipitation amount increases which may be caused by the air temperature increase. Runoff trend is similar to that of P-E ratio. Precipitation and P-E ratio have decreased all seasons except summer season and it means the reduction of available water resources during those seasons. These variability should be reflected in the spring, fall, and winter water supply strategy. |
|
Ű¿öµå |
±âÈĺ¯È;°¼öÈ¿À²;À¯Ãâ;Ãß¼¼ºÐ¼®;Climate Change;Precipitation Effectiveness Ratio;PRMS;Runoff;Trend Analysis; |
|
|
|
 |
|
Çѱ¹¼öÀÚ¿øÇÐȸ³í¹®Áý / v.44, no.8, 2011³â, pp.683-694
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1226-6280
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO201126235932371)
¾ð¾î : Çѱ¹¾î |
|
³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø |
|
|
|
|
|