Statement I: Evapotranspiration helps in classifying the climatic types.

Evapotranspiration is the process by which water is transferred from the land to the atmosphere through evaporation from the soil and transpiration from plants. It plays a crucial role in the water cycle and the overall climate system. Evapotranspiration is influenced by various climatic factors such as temperature, humidity, wind speed, and solar radiation.

The statement that evapotranspiration helps in classifying the climatic types is generally true. Different climatic types have different levels of evapotranspiration due to variations in temperature, humidity, and other climatic factors. For example, arid or dry climates have low evapotranspiration rates due to high temperatures and low humidity, while humid climates have high evapotranspiration rates due to lower temperatures and higher humidity. Therefore, evapotranspiration can be used as an indicator to classify climatic types.

Statement II: Only temperature affects evapotranspiration, hence it can be used for classifying the climatic types.

This statement is false. While temperature is a significant factor influencing evapotranspiration, it is not the only factor. Evapotranspiration is also influenced by humidity, wind speed, solar radiation, and other environmental