noun The process by which water is transferred from the land to the atmosphere through evaporation from the soil and transpiration from plants.
Evapotranspiration is a significant factor in ecosystem water balance and energy exchange.
Evapotranspiration is a key component of the water cycle, representing the combined processes of evaporation from the Earth's surface and transpiration from plants.
Evapotranspiration is important for determining water needs of crops and irrigation scheduling.
Evapotranspiration plays a crucial role in the movement of water through the atmosphere and the Earth's surface.
Evapotranspiration is a critical variable in climate models and understanding regional climate patterns.
Evapotranspiration may be mentioned in articles or essays about climate change, agriculture, or environmental science.
Meteorologists use evapotranspiration data to understand water cycles and weather patterns.
Agricultural scientists study evapotranspiration to optimize irrigation strategies and crop productivity.
Evapotranspiration is a key factor in environmental engineering projects related to water management and ecosystem health.
Geographers may analyze evapotranspiration rates to study regional climate patterns and land use changes.
Hydrologists use evapotranspiration data to model water budgets and predict water availability in different regions.
Botanists consider evapotranspiration in their research on plant physiology and ecosystem dynamics.
Civil engineers incorporate evapotranspiration data into infrastructure projects such as irrigation systems and urban planning.
Ecologists study evapotranspiration as part of their research on ecosystem dynamics and biodiversity conservation.