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Çѱ¹¼öÀÚ¿øÇÐȸ / v.18, no.3, 1985³â, pp.243-251
Áõ¹ß·®ÀÇ ½Ã°øÀû º¯È­
( Seasonal Variations of the Evaporation in Korea )
À̱¤È£;±è¹®ÀÏ; ÀüºÏ´ëÇб³ »ç´ë ÁöÇб³À°Çаú : College of Education, Jeonbuk National University;±â»ó¿¬±¸¼Ò ±â»ó±âÁ¤ : Applied Meteorological Laboratory, Meteorological Research Institute;
 
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¿ì¸®³ª¶ó¿¡¼­ Áõ¹ß·®ÀÇ ½Ã°£Àû °ø°£Àû ºÐÆ÷¸¦ 4´ë°­ À¯¿ª°ú ¿µµ¿Áö¹æÀ¸·Î ³ª´©¾î ±âÈÄÀڷḦ ÀÌ¿ëÇÏ¿© ºÐ¼®Çϰí, È£¼ö¸é Áõ¹ß·®°ú Áõ¹ß»êÀ§·®À» °è»êÇÏ¿© ´Ù¸¥ Áõ¹ß·® ¹× °­¼ö·®°ú ºñ±³ÇÔÀ¸·Î¼­ Áö¿ªº° ¹°¼öÁö¿ä¼ÒÀÇ º¯È­¸¦ Á¶»çÇÏ¿´´Ù. ¶ÇÇÑ Áõ¹ß¿¡ ¿µÇâÀ» ¹ÌÄ¡´Â ±â»ó¿ä¼Ò¿ÍÀÇ °ü°è¸¦ ºÐ¼®ÇÔÀ¸·Î¼­ ±âÈİüÃø¿ä¼Ò »óÈ£°£ÀÇ °ü°è¸¦ ±Ô¸íÇÏ¿´´Ù. ¼ÒÇüÁõ¹ß°è¿¡ °¡Àå Å« ¿µÇâÀ» ¹ÌÄ¡´Â ±â»ó¿ä¼Ò´Â Àϻ緮À̸ç, ´ÙÀ½Àº ±â¿ÂÀ̳ª dz¼Ó ¹× »ó´ë½Àµµ µîÀº ±× ¿ùº°°ªÀ» ³ªÅ¸³¾ ¶§ °ÅÀÇ ±â¿©µµ°¡ ¾ø¾ú´Ù. ¼ÒÇüÁõ¹ß·®°ú ´ëÇüÁõ¹ß·® ¹× È£¼ö¸éÁõ¹ß·®Àº ¼­·Î ±× ¿ùº°°ªÀÇ »ó°üÀÌ 0.90À» »óȸÇÔÀ¸·Î ¾î´À ÇÑ Áõ¹ß·®À¸·ÎºÎÅÍ À¯ÃßÇÒ ¼ö ÀÖ°í, ³â ¼ÒÇüÁõ¹ß°è¿¡ ´ëÇÑ ´ëÇüÁõ¹ß·® ¹× È£¼ö¸é Áõ¹ß·®ÀÇ ºñ´Â °¢°¢ 73% ¹× 55%Á¤µµÀ̳ª, »êÁö¿¡¼­´Â ±×º¸´Ù ¾à 10% Á¤µµ°¡ ³·¾Ò´Ù. Áõ¹ß»êÀ§·®Àº ÀÛ¹°»ýÀ°±â¿¡ ¼ÒÇüÁõ¹ß·®ÀÇ ¾à 80%¿¡ ´ÞÇϳª ³â Æò±ÕÄ¡´Â ¾à 70% Á¤µµÀ̸ç, °­¼ö·®ÀÇ 40¡­60%¿¡ ´ÞÇÑ´Ù.
The distributions of the copper plated(small) pan evaporation in both space and time are analysed with the data observed, and the lake and the potential evaportranspiration are estimated from the climatological data. These value are compared with each other and to the precipitation for deducing the seasonal amounts and variations of water budgets in the selected basins and regions. The meteorological factor which is closely associated with the small pan evaporation are hardly recognizable when they are used as the monthly values. The relationships among the small pan, the Class A pan and the lake evaporation are well correlated with each other with correlation coefficient of above 0.90, so it may be possible to derve other evaporations from knowing one evaporation. The ratio of the Class A pan and the lake evaporation to the small pan evaportion in annual are about 73% and 55%, repectively, except the mountaineous area where the values are about 10% less than those. The evapotranspiration reach about 40¡­60% of the annumal precipitation, but in May and October two values are nearly same. The frequencies of the monthly evaportion in class intervals in the regions are also provided.
 
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Çѱ¹¼öÀÚ¿øÇÐȸÁö / v.18, no.3, 1985³â, pp.243-251
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1738-9488
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO198511920091350)
¾ð¾î : Çѱ¹¾î
³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø
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