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NTIS 바로가기한국습지학회지 = Journal of wetlands research, v.19 no.1, 2017년, pp.16 - 29
송성욱 (고려대학교 건축사회환경공학과) , 이진욱 (고려대학교 건축사회환경공학과) , 조은샘 (고려대학교 건축사회환경공학과) , 유철상 (고려대학교 건축사회환경공학과)
It is known that large-scale deforestation has occurred in North Korea due to economic failures since the 1990s, and this is expected to greatly change the characteristics of the hydrological cycle. In this study, hydrological cycle simulation was carried out for the period of about 30 years from 19...
핵심어 | 질문 | 논문에서 추출한 답변 |
---|---|---|
VIC 모형은 어디에 많이 활용되는가? | VIC 모형은 1994년 미국 University of Washington의 Dennis Lettenmaier 박사 연구팀에 의해 개발된 모형으로 중규모 이상의 유역에 대한 적용성이 검증된 지표 수문해석모형이다. VIC 모형을 대륙 또는 전지구 단위의 수문순환을 모의하는데 많이 활용하고 있다. 예를 들어, Xie et al. | |
VIC 모형이란 무엇인가? | 1994)을 이용하였다. VIC 모형은 1994년 미국 University of Washington의 Dennis Lettenmaier 박사 연구팀에 의해 개발된 모형으로 중규모 이상의 유역에 대한 적용성이 검증된 지표 수문해석모형이다. VIC 모형을 대륙 또는 전지구 단위의 수문순환을 모의하는데 많이 활용하고 있다. | |
VIC 모형에서 구분되는 3개의 토층은 어떻게 나뉘는가? | 먼저, 차단층에서는 상록침엽수, 낙엽활엽수, 초지 등 11가지로 분류된 피복종류별 면적비를 고려하여 각 피복특성이 반영된 차단 및 증발(Ec)이 모의된다. 토층은 깊이에 따라 최상부토층(top thin layer), 상부토층(upper layer), 하부토층(lower layer)으로 나뉜다. 이 중 최상부토층은 침투(i)에 직접적인 영향을 받는 지역이며, 토양수분의 변화에 가장 민감하다. |
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