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Çѱ¹¼öÀÚ¿øÇÐȸ / v.37, no.2, 2004³â, pp.109-119
Áö±¸ ¿Â³­È­¿¡ µû¸¥ ¹° ¼ö¼Û º¯È­
( The Change of Water Vapor Transport due to Global Warming )
¿ÀÇöÅÃ;±èÁ¤¿ì;½ÅÈ£Á¤;ÃÖ¿µÁø; ±â»ó¿¬±¸¼Ò ±âÈÄ¿¬±¸½Ç;¿¬¼¼´ë ´ë±â°úÇаú;¿¬¼¼´ë Áö±¸È¯°æ¿¬±¸¼Ò;±â»ó¿¬±¸¼Ò ¿¹º¸¿¬±¸½Ç;
 
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ÀÌ ³í¹®¿¡¼­ ¿ì¸®´Â ´ë±â ´ë¼øÈ¯ ¸ðÇüÀ» »ç¿ëÇÏ¿© Áö±¸ ¿Â³­È­¿¡ µû¸¦ À°Áö ´ë±â·ÎÀÇ ¹° ¼ö¼Û º¯È­¸¦ Æò°¡Çß´Ù. ÇØ¾çÀ¸·ÎºÎÅÍ À°Áö·ÎÀÇ ¹° ¼ö¼Û º¯È­·®Àº Áö±¸¿Â³­È­¿¡ µû¶ó °ÅÀÇ ¿¬Áß Áõ°¡ÇÑ´Ù. À¯¶ó½Ã¾Æ´ë·úÀÇ ¹° ¼ö¼Û·®Àº ¿¬Áß 170¡­350${ imes}$106 Mt/day ¼öÁØÀÇ Áõ°¡¸¦ º¸ÀδÙ. ¾ÆÇÁ¸®Ä«·ÎÀÇ ¼ö¼ÛÀº 11¿ùÀ» Á¦¿ÜÇÑ ¸ðµç ´Þ¿¡ °¨¼Ò¸¦ º¸ÀÌ°í Æ¯È÷ 8¿ù°ú 9¿ù¿¡ -350${ imes}$106 Mt/dayÀÇ ÃÖ´ë °¨¼Ò¸¦ ³ªÅ¸³½´Ù. À¯¶ó½Ã¾Æ¿Í ¾ÆÇÁ¸®Ä«¸¦ Á¦¿ÜÇÑ ´Ù¸¥ ´ë·úµé¿¡ÀÇ ¼ö¼ÛÀº $pm$80${ imes}$106 Mt/day ¹Ì¸¸ÀÇ Áõ°¡¿Í °¨¼Ò¸¦ ´Þ¿¡ µû¶ó ´Ù¸£°Ô, ±×¸®°í ºÒ±ÔÄ¢ÇÏ°Ô º¸ÀδÙ. Áö±¸¿Â³­È­·Î À¯¶ó½Ã¾Æ ´ë·ú¿¡·ÎÀÇ ¹° ¼ö¼ÛÀÌ ÀüüÀûÀ¸·Î Áõ°¡ÇÏÁö¸¸, ÀÌ ´ë·ú ¾È¿¡ À§Ä¡ÇÑ »ç¸·Áö¿ªÀÇ ¹° ¼ö¼ÛÀº °¨¼ÒÇÑ´Ù. ±×·¯¹Ç·Î, »ç¸·À» Á¦¿ÜÇÑ ºÎºÐ, ƯÈ÷ ¸ó¼ø Áö¿ª¿¡ Áõ°¡ ºÐÀÌ ÁýÁßµÉ °ÍÀ̰í, ÀÌ·¯ÇÑ µ¿¾Æ½Ã¾Æ ¸ó¼ø°­È­ÀÇ °á°ú·Î ¸ó¼øÁö¿ª¿¡ »ó´çÇÑ °¡¿ë¼öÀÇ Áõ°¡°¡ ±â´ëµÈ´Ù.
This research is an analysis of the water vapor transport change Into the continent due to the global warming effect with the general circulation models. Water vapor transport change from ocean to land increases through the year due to CO2 doubling effect. In Eurasia, it indicates an increase about 170¡­350${ imes}$06 Mt/day the whole year. In Africa, it shows an decrease every month except November, especially there is the maximum decrease about -350${ imes}$106 Mt/day during August-September. In other continents, excluding Eurasia and Africa, the change of water vapor transport vary with the month below $pm$8.0${ imes}$106 Mt/day with the unsystematic patterns. In Eurasia, the change of water vapor transport increases as a whole, but it decrease in desert areas which occupy a high area-ratio. Therefore, except desert areas, the amount of the growth in water vapor transport change concentrate on Asian monsoon area. As a result of monsoon strengthening, available water will grow considerably at the asian monsoon areas.
 
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Áö±¸¿Â³­È­;°¡¿ë¼ö ¼ö¼Û;¹° ¼ö¼Û;¿¡³ÊÁö ¼ö¼Û;global warming;abailable water transport;water vapor transport;energy flux transport;
 
Çѱ¹¼öÀÚ¿øÇÐȸ³í¹®Áý / v.37, no.2, 2004³â, pp.109-119
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1226-6280
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO200411922294602)
¾ð¾î : Çѱ¹¾î
³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø
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