The smoke was cruising by in the middle levels of the atmosphere many thousands of feet above the ground. While far too high to smell, it caused spectacularly hued sunsets from New York to D.C. to Missouri.
Red sky at night
Lasting for about a week from Sept. 12 to Sept. 19, the smoke could be seen in satellite images as wisps and patches of light gray and was especially apparent over the darkly contrasting water of the Atlantic.
Soot particles are much larger than air molecules and are more adept at scattering the yellow, orange and red wavelengths of sunlight. The enhanced oranges, pinks and reds during sunset occur when the Sun’s rays have to travel through more smoke. That happens when the Sun is very low near the horizon rather than when it is directly overhead, hence the fiery sunsets.
Riding the jet stream
The smoke on the East Coast is coming from the horrifically large and persistent wildfires in the Western states. Smoke from those fires is showing up not only on the Eastern Seaboard, but even across the Atlantic in Europe.
How has all that smoke migrated so far? Blame this on the vagaries of the jet stream.
The jet stream is a high-altitude belt of fast wind that sails from west to east around the hemisphere in the middle latitudes. The jet stream is always present, but its wind speeds and exact path around the globe vary daily.
A connected world
Smoke isn’t the only aerosol that can sail around the Earth on wind currents. Pollution from China regularly travels to the U.S., where it’s been detected along the East Coast. Fine dusts lofted from the Sahara Desert in Africa can be swept westward to the Southeastern U.S., as happened just a few months ago.
After a week of hazy skies, a large air mass from Canada blew into the East Coast bringing in smoke-free air. But the Western U.S. fire season continues, and if the jet stream dips south again, the East could experience additional blasts of smoke-laden air. The globe may be vast, but wind currents connect us all.