Ever seen the jet stream? Not on a weather map, or talked about on a weather show, but overhead in the sky?
Most of the time the jet stream, being air, is invisible. If you see clear sky looking up, or an overcast, you really can’t tell the jet stream’s up there. That’s one of the reasons it took so long to discover it was there. There were hints, starting with the way the ash from Krakatoa spread. Planes prior to WWII generally didn’t fly high enough to encounter it, though a few planes during WWII went high enough to find
their air speed and their ground speed were vastly different. Today the jet stream can make a difference of 100 mph or more in how fast a jet travels, and company meteorologists generally try to route planes away from a headwind in the jet stream.
Jet streams form where there is a large horizontal difference in temperature, and are very likely over fronts near the
surface. They also generally have a high-speed core with lower speeds to the sides, and this wind shear tends to drag out tendrils of cloud so they form lines parallel to the jet stream. If you look up and see long streaks of filmy cloud, all in the same direction from horizon to horizon, chances are good you are seeing the jet stream.
We don’t see that very often here in Alaska, because the jet stream is generally south of us, over the Pacific Ocean. But large waves do form in the jet stream, and last Wednesday a wave formed that put the jet stream moving from south to north over our heads. The warm air it brought aloft was reflected in a lovely warm day (77°F) at the ground, and the cirrus streaks were conspicuous. Thanks to perspective, they fanned out from the northern and southern horizons, and looked horizontal when you gazed east or west. All of the photos were taken at the Farmers Market, around 1 pm ADT.
In the lower 48, jet streams are more likely to blow roughly from west to east. Look for them!










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[…] 7/5/12 How Long is your Night? 7/7/12 Colorado Storm 8/2/12 Could Jarn have Made Glass? 8/11/12 Seeing the Jet Stream 8/18/12 Share this:FacebookEmailStumbleUponTwitterLike this:LikeBe the first to like this. […]
[…] Jet stream cirrus is by no means the only kind of cirrus cloud. Cirrus clouds come in many different forms. The thing they have in common is that they are all made of ice crystals, and thus they are all in cold parts of the atmosphere – generally below -20°C, or -4°F. At these temperatures, the ice nuclei that turn supercooled water droplets into ice are generally common enough that at least a few droplets freeze. Since ice can grow by direct sublimation of water vapor at humidities where supercooled water would evaporate, the ice particles grow rapidly at the expense of the water droplets. […]