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31 de ago. de 2010 · [4] This analysis presents daily values of canopy rainfall interception on a global 0.25° latitude-longitude resolution grid. It is based on the revised version of Gash's analytical model [Valente et al., 1997] driven by satellite remotely sensed data of precipitation, lightning frequency and canopy fraction.
As a consequence, the methodology distinguishes only three sources of evapo-ration based on the land surface type: (1) bare soil, (2) short vegetation, and (3) vegetation with a tall canopy. The snow and ice sublimation is estimated for the pixels covered in snow through a separate routine.
31 de ago. de 2010 · The Climate Prediction Center morphing technique (CMORPH) precipitation product is used as driving data and is applied to Gash's analytical model to derive daily interception rates at global scale. Results compare well with field observations of rainfall interception ( R = 0.86, n = 42).
31 de ago. de 2010 · According to our findings, interception loss is responsible for the evaporation of approximately 13% of the total incoming rainfall over broadleaf evergreen forests, 19% in broadleaf deciduous...
Together they form a unique fingerprint. Canopy Earth and Planetary Sciences. Satellite Observation Earth and Planetary Sciences. Rainfall Earth and Planetary Sciences. Forests Agricultural and Biological Sciences. Satellites Agricultural and Biological Sciences. Canopy Interception Agricultural and Biological Sciences.
1 de may. de 2024 · Forest canopy rainfall interception (FRCI) is an essential hydrological process that governs water and biogeochemical cycles in forest ecosystems. Identifying patterns and relationships of FCRI using a systematic review is key to improving our knowledge supporting new experiment research, modeling, and application.
27 de ago. de 2010 · This article presents a comprehensive study of canopy interception in six rainforests in Australia's Wet Tropics for periods ranging between 2 and 3·5 years. Measurements of rainfall, throughfall, …
