An Integrative Theory Of Dew Ecology: Reconstructing Its Origins Across Diverse Natural Landscapes

This study aims to reconstruct the theoretical framework of dew formation in natural ecosystems by classifying its origins into three ecological pathways: atmospheric, plant-based, and subterranean, rather than attributing it solely to atmospheric condensation. The method employed is systematic observation and theoretical reconstruction through analysis of physical and chemical processes at three interfaces: atmosphere, biosphere, and geosphere, supported by field validation using plastic barriers to capture vapor rising from the soil. The results identify three types of dew: atmospheric dew formed by nocturnal temperature differences, transpiration (biological) dew resulting from interactions between plant-emitted water vapor and CO₂, and telluric (ground) dew driven by continuous geothermal evaporation that later condenses at the surface. These findings show that dew is not a singular phenomenon but the result of synchronized interactions among air, plants, and soil. The novelty of this study lies in its tri-origin framework of dew formation, integrating atmospheric, biological, and geothermal processes, offering a new perspective in eco-hydrology and water resource management.