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Net Radiation and Soil Heat Fluxes Measured on Coastal Wetland Covered with Reeds

갈대 서식 연안습지에서의 순복사와 토양열 플럭스

  • Kim, Hee-Jong (Department of Astronomy and Atmospheric Sciences, Kyungpook National University) ;
  • Kim, Dong-Su (Department of Environmental Atmospheric Science, Pukyong National University) ;
  • Yoon, Ill-Hee (Department of Earth Science Education, Kyungpook National University) ;
  • Lee, Dong-In (Department of Environmental Atmospheric Science, Pukyong National University) ;
  • Kwon, Byung-Hyuk (Department of Environmental Atmospheric Science, Pukyong National University)
  • 김희종 (경북대학교 천문대기과학과) ;
  • 김동수 (부경대학교 환경대기과학과) ;
  • 윤일희 (경북대학교 지구과학교육과) ;
  • 이동인 (부경대학교 환경대기과학과) ;
  • 권병혁 (부경대학교 환경대기과학과)
  • Published : 2007.02.28

Abstract

In the coastal wetland the mud is consist of fine particles, which means that it is characterized by small gap, and heat transfer is obstructed since moisture is found between the gaps. The relationship between net radiation ($R_N$) and soil heat flux($H_G$) shows a counterclockwise hysteresis cycle, which refer to a time lag behind in the maximal soil heat fluxes. The albedo is independent of seasonal variation of the vegetation canopy which plays very important roles to store and control the heat in the atmospheric surface layer.

Keywords

References

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