Continuing with our Answering Viewer Questions series, Susie asks why it seems like the wind is stronger during the day than at night. Outside of the influence of storms, our winds are typically a bit stronger during the day compared to at night. This is because stronger winds found just above the surface can be mixed down to the ground a little easier during the day.

This can be visualized using an atmospheric sounding, or a vertical profile of a column of air above one single point. The red line plotted below is the temperature, while the green line is a dew point. The bottom of the plot the surface, while the top of the chart is typically miles up in the sky.
A typical daytime sounding has strong "lapse rates" in the lower levels. Simply put, the air cools quicker over short distances. This steeper slope allows the air above to easier mix down toward the ground unimpeded. And often stronger winds -- commonly referred to as the "low-level jet" -- are found just above the ground. These winds are also mixed down to the ground, producing stronger winds during the day.

Compare this to a nighttime example. The only change from the last sounding to this one is the temperature in the lower levels near the surface. Since we cool off quickly at night with the loss of solar radiation, the temperature at the surface becomes cooler than that above. This is called an "inversion" where there is no longer cooling with height. This layer of relatively warmer air prevents that mixing mentioned above, which typically results in lower wind speeds at night compared to the day.

To summarize: stronger winds during the day are a result of deeper mixing, where air above the surface is easier transported down to the ground. While the loss of daytime heating prevents that mixing effect.



















