The Water Cycle 3D print model

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Evaporation transforms water from its liquid state to a gas state in the atmosphere, often driven by temperature and humidity changes. Transpiration propels moisture upwards from plants, contributing significantly to Earth's evapotranspirational losses. Condensation sparks formation of droplets within clouds when water vapor meets cooler air, setting the stage for precipitation. Precipitation manifests as falling particles or forms other water cycles in an effort to maintain atmospheric equilibrium. Groundwater runoff results when excess rain and melting snow seep downward into underlying soil layers and feed streams via subsurface aquifers. Surfacewater runoff occurs as precipitation directly flows across land, moving along various slopes until it meets the ultimate fate of drainage.