themselves are invisible – we can’t see the air. However, we can see what affect inversions have on the atmosphere. That’s becauseinversions act as a lid and trap whatever is emitted between them and the ground.
This is particularly evident with pollution and most apparent during the winter months when inversions are
typically the strongest. In the animated image to the left, a strong morning inversion developed over Maryland
on Wednesday, January 6, 2016. Downtown Baltimore can be seen in the center left of the image. The image spans
from 9am to 5pm local time. Without sunlight, inversions strengthen. As the sun had only risen briefly by 9am,
the inversion on January 6th was near its lowest height (strongest intensity) of the day as often occurs near
sunrise. Trapped pollution is evident as a “brownish” color due to elevated concentrations of nitrogen dioxide
very near to the ground which is emitted from cars and other combustion sources. At the beginning of the animation,
the brown area is very near the ground (lower black line) while up above a very blue, clean sky is visible, evidence
of clean air. Over the course of the next few hours, the inversion “lifts”, that is, the pollution of the city (the brownish area) rises to a higher height (upper black line noted on the image). This increase in height of the inversion decreases pollution concentrations near the surface and is why in winter time, the most polluted part of the day is often in the early morning hours.
*The white plume seen in the center of the image is steam. It illustrates changing wind direction during the day due to heating differences between the water and land.