What occurs to the ELR during the day as temperature increases post-sunrise?

As the day progresses after sunrise, solar heating causes the ground and the lower layers of the atmosphere to warm up. This increase in temperature leads to the phenomenon known as a steepening of the environmental lapse rate (ELR). The ELR represents how temperature changes with height in the atmosphere. As the surface warms, the air close to the ground becomes less dense compared to the cooler air above it. This creates a situation where the temperature decreases more sharply with height, resulting in a steepening of the ELR.

When the ELR steepens, it contributes to atmospheric instability. In unstable conditions, rising air can continue to ascend freely, leading to the development of convective clouds and possibly thunderstorms as warm air rises and cools. This is a critical aspect of meteorology, as it helps forecasters predict weather patterns associated with instability, such as the formation of cumulonimbus clouds.

In contrast, other scenarios where the ELR either decreases or remains constant would typically signify stable atmospheric conditions, where vertical movement of air is suppressed, and stability prevails. Therefore, the correct understanding of the relationship between surface heating and the ELR is vital for predicting weather phenomena and is captured accurately in this answer.