Which statement is true regarding the relationship between temperature and dew point?

The relationship between temperature and dew point is characterized by the principle that air can hold a certain amount of moisture at different temperatures. The dew point refers to the temperature at which air becomes saturated with moisture and water vapor begins to condense into liquid water.

In this context, temperature will always be greater than or equal to the dew point. When the air temperature is equal to the dew point, it indicates that the air is saturated, leading to conditions such as fog or high humidity. Conversely, when the temperature exceeds the dew point, it signifies that the air is not fully saturated, and moisture will not condense unless cooling occurs or humidity increases.

This understanding clarifies why the assertion that temperature is always below the dew point or always equal to it cannot be accurate; it is the other way around. Additionally, noting that temperature and dew point are independent of each other overlooks the intrinsic connection between these two measures of atmospheric conditions. Temperature significantly influences the dew point, as warmer air can retain more moisture, aligning perfectly with the concept of temperature being greater than or equal to the dew point.