¶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.39, no.8, 2006³â, pp.645-658
SWSI °¡¹³Áö¼ö¸¦ º¸¿ÏÇÑ ÁØºÐÆ÷Çü ¼ö¹®ÇÐÀû °¡¹³Æò°¡ ¿¬±¸
( A Study on Semi-distributed Hydrologic Drought Assessment Modifying SWSI )
±ÇÇüÁß;¹ÚÇöÁø;È«´ëÀÇ;±è¼ºÁØ; °Ç±¹´ëÇб³ ´ëÇпø Áö¿ª°Ç¼³È¯°æ°øÇаú;Çѱ¹¼öÀÚ¿ø°ø»ç Á¶»ç¼³°èÆÀ;Çѱ¹¼öÀÚ¿ø°ø»ç Á¶»ç¼³°èÆÀ;°Ç±¹´ëÇб³ »çȸȯ°æ½Ã½ºÅÛ°øÇаú;
 
ÃÊ ·Ï
¼ö¹®ÇÐÀûÀÎ °¡¹³Æò°¡¸¦ À§ÇÏ¿© SWSI °¡¹³Áö¼ö¸¦ º¸¿ÏÇÑ MSWSI °³¹ßÇÏ¿´´Ù. MSWSIÀÇ Àû¿ëÀ» À§ÇÏ¿© °¡¹³¿¡ ¿µÇâÀ» ¹ÌÄ¡´Â ¼ö¹®ÀÎÀÚ°¡ µ¿ÁúÇÑ Áö¿ª Áï, ´ï, ÇÏõ, ÁöÇϼö, °­¼ö Áö¿ªÀ¸·Î Àü±¹À» 32°³ÀÇ Áö¿ªÀ¸·Î ºÐÇÒÇÏ¿´´Ù. °¢°¢ÀÇ Áö¿ª¿¡ MSWSI¸¦ Àû¿ëÇÏ¿© °ø°£ÀûÀ¸·Î ÁØºÐÆ÷ÇüÀÇ ¼ö¹®ÇÐÀû °¡¹³ Á¤º¸¸¦ ȹµæÇÏ¿´À¸¸ç, ½Ã°£ÀûÀ¸·Î 1974³âºÎÅÍ 2001³â±îÁöÀÇ ÇÑ´Þ °£°ÝÀ¸·Î Æò°¡ÇÏ¿´´Ù. °ú°Å °¡¹³ »ç»ó ³âµµ¿¡ ´ëÇÏ¿© ±â»óÇÐÀû °¡¹³Áö¼öÀÎ PDSI¿ÍÀÇ ºñ±³, ºÐ¼®À» ÅëÇÏ¿© ¼ö¹®ÇÐÀûÀÎ °¡¹³ Æò°¡ °á°ú¿¡ ´ëÇÏ¿© °ËÁõÇÏ¿´´Ù.
A hydrological drought index, MSWSI (Modified Surface Water Supply Index) was suggested based on SWSI. South Korea was divided into 32 regions considering the distribution of available gauge station of precipitation, dam storage, stream water level and natural groundwater level. The indices estimated in the regions represent a spatially distribution of drought. Monthly MSWSI was evaluated for the period of 1974 and 2001. The result was compared with PDSI and checked the applicability of the suggested index in our hydrologic drought situation.
 
Ű¿öµå
¼ö¹®ÇÐÀû °¡¹³;MSWSI;hydrological drought;PDSI;
 
Çѱ¹¼öÀÚ¿øÇÐȸ³í¹®Áý / v.39, no.8, 2006³â, pp.645-658
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1226-6280
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO200634741444580)
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¿