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Çѱ¹¼öÀÚ¿øÇÐȸ / v.23, no.4, 1990³â, pp.459-466
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¾óÀ½°ñÀÇ ÇÏ°è °áºùÇö»ó¿¡ °üÇÑ ¼ö¹®ÇÐÀû ¿¬±¸
( Hydrological Study of the Freezing in Summer Season at the Ice Valley, Korea ) |
| ¹è»ó±Ù; °è¸í´ëÇб³ °ø°ú´ëÇÐ Åä¸ñ°øÇаú;
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| Çϰ迡´Â ¾óÀ½ÀÌ ¾î³ª µ¿°è¿¡´Â ¾óÁö ¾Ê´Â ¾óÀ½°ñÀÇ ¿Âµµ ¿ªÀüÇö»óÀ» ±Ô¸íÇϱâ À§ÇÏ¿© ¿ÀÌ·ù¿Í ¿Àüµµ¸¦ °í·ÁÇÑ ÁöÇϼö¿Â Çü¼º¿¡ °üÇÑ À̷нÄÀ¸·Î ºÎÅÍ ¼öÄ¡½ÇÇèÀ» ÇàÇÏ¿´´Ù. ±× °á°ú ¾óÀ½°ñÁö¿ªÀÇ ÀÌ»ó¼ö¿ÂÇö»óÀº ÁöÇϼö¿ÂÀÇ Áöü¿¡ ÀÇÇÑ °ÍÀÓÀÌ ÆÇ¸íµÇ¾úÀ¸¸ç ±×¿¡ ´ë ÇÑ ¿øÀεµ ÃßÁ¤µÇ¾ú´Ù. |
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| In the Ice Valley, it freeze in summer season. However, there is no ice during winter. In order to clarify the phenomenon of unusual temperature, numerical experiments were conducted using the coupled equations of fluid flow and heat transfer. The results demonstrated that temperature inversion in the Ice Valley is primarily due to delay of the groundwater temperature. Also, the results of the simulation suggest that major factors affecting the delay are the topographical configuration, geological factors and groundwater flow system, combined with groundwater recharge and discharge systems. |
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Çѱ¹¼öÀÚ¿øÇÐȸÁö / v.23, no.4, 1990³â, pp.459-466
Çѱ¹¼öÀÚ¿øÇÐȸ
ISSN : 1738-9488
UCI : G100:I100-KOI(KISTI1.1003/JNL.JAKO199011920093351)
¾ð¾î : Çѱ¹¾î |
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| ³í¹® Á¦°ø : KISTI Çѱ¹°úÇбâ¼úÁ¤º¸¿¬±¸¿ø |
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