Abstract
A hydrologic cycle model is developed in order to evaluate water budget and the mechanism of the cycle of water movement within a forested watershed. This model is built by four basic processes, rainfall interception, transpiration, soil moisture and runoff, taking account of SPAC (Soil-Plant-Atmosphere Continuum).This model is applied to a small forested watershed in Tokushima Prefecture. It is concluded that this model can explain the diurnal and long-term hydrologic trends of soil moisture whose behavior is related to rainfall interception, transpiration and rainfall-runoff.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
