The Woolwich Observer
The convergence of Texas, Rossby waves, and wave-7
Texas puts out more carbon dioxide than any other U.S. state, so there was some innocent amusement to be had from the indignation of Texans unable to boil their drinking water during the Big Freeze because the power was still out. Things like that are not supposed to happen in a modern, developed country like the US of A. How dare they?
Others, aware that Texas has cut every corner in the public services that it’s possible to cut, were unsurprised by the fiveday mini-disaster that struck the country’s second-biggest state (30 million people). One blogger wrote philosophically: “Occasionally, something will happen in Texas to remind the people who live here that we live in a failed state.”
A winter temperature 25°C colder than usual for the time of year is rare, but this is not the first time it has snowed in Texas. The electricity failed, triggering a cascade of other disasters, mainly because of a longstanding refusal to connect the state electricity grid with the two main national grids. (This was done to avoid federal supervision on prices and standards).
Other people have cold snaps too. Germany, Russia, Canada, even northern China get much colder than Texas, but they don’t end up freezing in the dark because they are prepared for it. Texas could have been prepared for it, too, but somebody in power would have had to read the science journals. Since they almost all got elected with donations from fossil fuel producers, that was never very likely.
The ‘explainers’ on the media talk about a rogue
‘Arctic vortex,’ but what’s really happening is much simpler than that. It’s just what global heating has done to the northern hemisphere’s ‘jet stream.’
The northern jet stream is a high-speed, high-altitude atmospheric ‘river’ that flows from west to east all the way around the planet. It marks the boundary between the polar air mass, sometimes called the ‘Polar Vortex’, and the warmer air masses of the mid-latitudes. (Eastbound airliners crossing the North Atlantic and the North Pacific often hitch a ride on the jet stream, saving up to an hour compared to the westbound journey.)
The energy that drives the jet stream comes from the temperature difference between the two air masses it divides. However, the Arctic is warming much faster than the rest of the world, so that difference is shrinking – and with less energy, the jet stream is slowing down.
It used to blast straight east all the way around the planet, but even then it occasionally developed long S-shaped kinks called Rossby waves: big loops extending far north and south of its usual track. As it has slowed down (the average speed is now 150-225 kph), the Rossby waves have grown both more frequent and bigger.
They are often now great loops deviating far north and south from the straight track, and those loops bring with them cold polar air rarely seen so far south, or warm air not seen previously so far north. That’s what happened to Texas last week: one of those Rossby waves brought cold Arctic air all the way south – and then stuck for a while.
The jet stream itself didn’t stop. It just flowed all the way