¶óÆæÆ®¦¢Ä«Æä¦¢ºí·Î±×¦¢´õº¸±â
¾ÆÄ«µ¥¹Ì Ȩ ¸í»çƯ°­ ´ëÇבּ¸½Ç޹æ Á¶°æ½Ç¹« µ¿¿µ»ó°­ÀÇ Çѱ¹ÀÇ ÀüÅëÁ¤¿ø ÇÐȸº° ³í¹®
ÇÐȸº° ³í¹®

Çѱ¹°Ç¼³°ü¸®ÇÐȸ
Çѱ¹°ÇÃà½Ã°øÇÐȸ
Çѱ¹µµ·ÎÇÐȸ
Çѱ¹»ý¹°È¯°æÁ¶ÀýÇÐȸ
Çѱ¹»ýÅÂÇÐȸ
Çѱ¹¼öÀÚ¿øÇÐȸ
Çѱ¹½Ä¹°ÇÐȸ
Çѱ¹½Ç³»µðÀÚÀÎÇÐȸ
Çѱ¹ÀÚ¿ø½Ä¹°ÇÐȸ
Çѱ¹ÀܵðÇÐȸ
Çѱ¹Á¶°æÇÐȸ
Çѱ¹Áö¹Ý°øÇÐȸ
Çѱ¹ÇÏõȣ¼öÇÐȸ
Çѱ¹È¯°æ»ý¹°ÇÐȸ
Çѱ¹È¯°æ»ýÅÂÇÐȸ

Çѱ¹¼öÀÚ¿øÇÐȸ / v.14, no.4, 1981³â, pp.35-52
Çѱ¹ ¸éÀû °­¿ì·® »êÁ¤¿¡ °üÇÑ ¿¬±¸<¿ùº°, °èÀýº° ¹× ¿¬°£¿ì·® Áß½ÉÀ¸·Î>
( A Study on the Evaluation of Areal Precipitation in Korea. )
Á¤¹®±³;½ÉÀç¼³; ¿¬¼¼´ëÇб³ ´ëÇпø;¿¬¼¼´ëÇб³ ´ëÇпø, °æ±â´ëÇÐ Á¶±³¼ö, °æ±â´ëÇÐ;
 
ÃÊ ·Ï
º» ¿¬±¸´Â Àü±¹ ÁÖ¿ä ÁöÁ¡¿¡ ´ëÇÑ ¿ùº°, °èÀýº° ¹× ¿¬¿ì·®À» ±âº»ÀÚ·áÁý´ÜÀ¸·Î ÇÏ¿© ÁöÁ¡ ¹× Áö¿ª ºóµµ ÇØ¼®À» ½Ç½ÃÇÔÀ¸·Î½á ¸éÀû °­¿ì·®À» »êÁ¤ÇÑ ³»¿ëÀÌ´Ù. ±âº»ÀÚ·áÁý´ÜÀº Àü¹Ý±â(1916³â¡­1944³â; 29³â°£)¿Í ÈĹݱâ(1960³â¡­1979³â; 20³â°£)·Î ¾çºÐÇÏ¿© ó¸®ÇÏ°í ºñ±³ °ËÅäÇÏ¿´´Ù. ÁöÁ¡ ºóµµÇؼ®¿¡ À־ ÀûÁ¤ ºÐÆ÷ÇüÀº º¯¼öº¯È¯¹ýÀ» Àû¿ëÇϰí, $$-test ¹ýÀ» ÀÌ¿ëÇÏ¿© Á¤±Ô¼º °ËÁ¤À¸·Î ¼³Á¤ÇÏ¿´À¸¸ç, Áö¿ª ºóµµ ÇØ¼®Àº ÁöÇüÀÎÀÚ¿Í ¼ö¹®±â»óÇÐÀû ÀÎÀÚ¸¦ °í·ÁÇÏ¿© Àü±¹À» 5°³±Ç¿ªÀ¸·Î ±¸ºÐÇϰí Thiessen ¹æ¹ý°ú µî¿ì¼±¹ý(Isohyetal Method)À» Àû¿ëÇÏ¿© ºñ±³ °ËÅäÇÏ¿´´Ù. º» ¿¬±¸¸¦ ÅëÇÏ¿© ¾ò¾îÁø ¼º°ú´Â ¾Æ·¡¿Í °°´Ù. 1) Àü¹Ý±â ÀÚ·áÁý´Ü¿¡ ÀÇÇÑ Àü±¹ÀÇ ¸éÀû °­¿ì·®Ä¡´Â ÈĹݱâ ÀÚ·áÁý´Ü¿¡ ÀÇÇÑ ÇØ¼® °á°úÄ¡º¸´Ù 70¡­80mm ÀÛÀº °ªÀ» ³ªÅ¸³»°í ÀÖÀ¸¹Ç·Î º¸¾Æ ÇöÀç±îÁöÀÇ 1,150mm¸¦ 1,180mm Á¤µµ¸¦ »óÇâÁ¶Á¤ÇÔÀÌ ¹Ù¶÷Á÷ÇÏ´Ù°í »ý°¢ÇÑ´Ù. 2) Àü±¹À» 5°³ ±Ç¿ªÀ¸·Î ±¸ºÐÇÏ¿© ¿¬Æò±Õ ¸éÀû °­¿ì·®À» »êÁ¤ÇÑ ¹Ù, Ãá°èÀÇ ¸éÀû °­¼ö·®ÀÌ Å¸°èÀý¿¡ ºñÇÏ¿©(¾à 5½Å) Å©°Ô Áõ°¡Çϰí ÀÖÀ½Àº ¼öÀÚ¿ø Àû±â È®º¸ ¹æ¾È ¼ö¸³¿¡ Ư±âÇÒ Á¡À̶ó ÇϰڴÙ. 3) ¸éÀû °­¼ö·® ÇØ¼®Àº ±Ç¿ªº°·Î ±¸ºÐÇÏ¿© µî¿ì¼±µµ¹ýÀ¸·Î ÇØ¼®ÇÔÀÌ ÇÕ¸®Àû ¹æ¹ýÀ̶ó°í »ý°¢µÈ´Ù.
This study is to evaluate the areal precipitation from the basic data groups of monthly, seasonal, and annual rainfalls over all ma in stations in Korea. The evaluating pocesses are performed through the point and regional frequency analysis from the basic data. The basic data groups are divided into two periods-the first(1916-1944) and the second (1960-1979)-which are compared with each other. In the point frequecny analysis, the variable transformation method is applied to the best fitting distribution, and the normal fittings are established by using the Chisquare test method. In the regional frequency analysis, the geomorphologic factors and hydrometeorological factors are taken into consideration when dividing into five zones and Thiessen method and the Isohyetal method are applied. The results of this study are as follows: 1)The areal precipitation values of the first period are about 70-80mm less than that of the second period for the whole of Korea. Therefore, a new precipitation value of 1180mm is considered more suitable than the value of 1159mm, which has been up till now. 2)As the annual areal precipitiation values areevaluated over the five divide zones, it tis noticed that the difference between the values of the first period and the second is the largest in spring (to the extent of 5 times that in the other seasonas). Thereform it is considered that this result is necessary for the establishment of a timely insurance plan for the water resources. 3)The application of the Isohyetal method through the division of Korea into five zones is considered to be a reasonable procedure in the analysis of areal precipitation.
 
Ű¿öµå
 
Çѱ¹¼öÀÚ¿øÇÐȸÁö / v.14, no.4, 1981³â, pp.35-52
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1738-9488
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO198111920090265)
¾ð¾î : Çѱ¹¾î
³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø
¸ñ·Ïº¸±â
ȸ»ç¼Ò°³ ±¤°í¾È³» ÀÌ¿ë¾à°ü °³ÀÎÁ¤º¸Ãë±Þ¹æÄ§ Ã¥ÀÓÀÇ ÇѰè¿Í ¹ýÀû°íÁö À̸ÞÀÏÁÖ¼Ò ¹«´Ü¼öÁý °ÅºÎ °í°´¼¾ÅÍ
   

ÇÏÀ§¹è³ÊÀ̵¿