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Çѱ¹¼öÀÚ¿øÇÐȸ / v.33, no.4, 2000³â, pp.471-482
Landsat TM ÀڷḦ ÀÌ¿ëÇÑ ±¤¿ª Áõ¹ß»ê·® ÃßÁ¤
( An Assessment of Areal Evaportranspiration Using Landsat TM Data )
äȿ¼®;¼Û¿µ¼ö;¹ÚÀ翵; Çѱ¹¼öÀÚ¿ø°ø»ç ¼öÀÚ¿ø¿¬±¸¼Ò;ÀüºÏ´ëÇб³ °ø°ú´ëÇÐ ÀÚ¿ø°øÇаú;Çѱ¹¼öÀÚ¿ø°ø»ç ¿¬¼ö¿ø;
 
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º» ¿¬±¸¿¡¼­´Â Landsat TM ÀÚ·á¿Í GIS ±â¹ýÀ» ÀÌ¿ëÇÏ¿© ÁöÇ¥¸é ¿¡³ÊÁö ¼öÁö ¿ä¼Ò¸¦ °ø°£ÀûÀ¸·Î ÃßÃâÇϰí, ÃßÃâµÈ ¿¡³ÊÁö ¼öÁö ¿ä¼ÒÀÇ Àû¿ë¼ºÀ» °ËÅäÇϱâ À§Çؼ­ ±¤¿ª Áõ¹ß»ê·®À» ÃßÁ¤ÇÏ¿´´Ù. ÃßÁ¤°á°ú¿¡ ´ëÇÑ Á¤È®µµ ¹× ¿­¼öÁö ¿ä¼Ò°¡ Áõ¹ß»ê·®¿¡ ¹ÌÄ¡´Â ¿µÇâÀ» ºÐ¼®Çϱâ À§Çؼ­ ¹Î°¨µµºÐ¼®°ú ¿ÀÂ÷ºÐ¼®À» ½Ç½ÃÇÏ¿´´Ù. ¿¬±¸ ´ë»óÁö¿ªÀº ±Ý°­ »ó·ùÀÇ º¸Á¤ÃµÀ̸ç, 1995³âµµ 1¿ù 11ÀÏ, 4¿ù 1ÀÏ, 5¿ù 3ÀÏ, 10¿ù 10ÀÏ ¹× 11¿ù 27ÀÏ¿¡ ȹµæµÈ 5°³ÀÇ Landsat TMÀڷḦ ÀÌ¿ëÇÏ¿´´Ù. ¿¬±¸°á°ú ÁöÇ¥¸éÀÇ °æ»ç ¹æÇâ°ú ÅäÁöÇǺ¹ ÇüÅ¿¡ µû¶ó Áõ¹ß»ê·®ÀÇ º¯È­°¡ Å©°Ô ³ªÅ¸³µÀ¸¸ç, °æ»ç ¹æÇâÀÌ ºÏµ¿À̳ª ³²µ¿¹æÇâÀÏ °æ¿ì ½Ä»ýÁö¼ö(NDVI; Normalized Difference Vegetation Index) °ªÀÌ Áõ°¡ÇÔÀ¸·Î½á ÁöÁß¿­ Àüµµ·®ÀÌ Áõ°¡ÇÏ°Ô µÇ¾î »ó´ëÀûÀ¸·Î Áõ¹ß»ê·ªÀÌ °¨¼ÒÇÏ´Â °ÍÀ¸·Î ³ªÅ¸³µ´Ù. ¹Î°¨µµ ¹× ¿ÀÂ÷ºÐ¼® °á°ú, ¼ø¹æ»ç·®ÀÌ 12.5% ³»Áö 23.6%ÀÇ ¹Î°¨µµ·Î¼­ ÁöÇ¥¸é ¿Âµµ¿Í ´ë±â¿Âµµ ¹× dz¼Ó µîµµ ´Ù¸¥ ÀÎÀÚ¿¡ ºñÇØ °¡Àå Å« ¿µÇâÀ» ¹ÌÄ¡´Â °ÍÀ» ¾Ë ¼ö ÀÖ¾ú´Ù.
Surface energy balance components were evaluated by Landsat TM data and GIS with meteorological data. Calibration and validation for the applicability of this methodology were made through the estimating of the large-scale evapotranspiration (ET). In addition, sensitivity and error analysis was conducted to see the effects of the surface energy balance components on ET and the accuracy of each components. Bochong-chon located on the upper part of Guem River basin was selected as the case study area. Spatial distribution map of ET were produced for five dates: Jan. 1, Apr. 3, May. 10, and Nov. 27, 1995. The study results showed tat ET was greatly varied with the aspect and theland use type on the surface. In the case of having northeast and southeast in the aspect, ET was linearly increased depending on growing net radiation. While surface temperature has a high value, NDVI(Normalized Difference Vegetation Index) has a low value in the vegetated area. Therefore, ground heat flux was increased but ET was relatively decreased. The results of sensitivity and error analysis showed that net radiation is most sensitive and effective, ranging from 12.5% to 23.6% of sensitivity. Furthermore, the surface temperature, air temperature, and wind speed have the significant effects on ET estimation using remotely sensed data.
 
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Áõ¹ß»ê;¿¡³ÊÁö ¼öÁö;Evapotranspiration;Landsat TM;energy balance;GIS;
 
Çѱ¹¼öÀÚ¿øÇÐȸ³í¹®Áý / v.33, no.4, 2000³â, pp.471-482
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1226-6280
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO200011920063846)
¾ð¾î : Çѱ¹¾î
³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø
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