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() and soil heat flux() 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.

• 권병혁(부경대학교 환경대기과학과) | Byung Hyuk Kwon Corresponding Author
• 이동인(부경대학교 환경대기과학과) | Dong In Lee
• 윤일희(경북대학교 지구과학교육과) | Ill Hee Yoon
• 김동수(부경대학교 환경대기과학과) | Dong Su Kim
• 김희종(경북대학교 천문대기과학과) | Hee Jong Kim