The US has seen three Once-In-A-Thousand-Years rain storms in the last 7 or 8 days.
Three of 'em.
I wonder if anybody's keeping track of how many of these we've see in recent years, and whether or not we can get a reasonable guess as to what we can expect - other than the usual "this is going to get worse".
So can we expect Republicans to get on board now? Or will they try to kick it around one more time- hoping to continue their political "success" by sitting on their asses bitchin' about wind mills and the price of electric cars, and taking every opportunity to block the actions that would help? The actions which btw, they've been actively sabotaging for 30 years - which, had they not been sabotaging every attempt, would be in place now making things just a tiny bit better.
It was pointed out years ago that Climate Change could be the perfect driver that causes such global upheaval that a situation is created to facilitate the movement towards authoritarianism.
Seems like we're watching that shit happen in real time right now.
WaPo: (pay wall)
If it seems like a barrage of extreme rain events has been wreaking havoc across the country over the past week, you’re not imagining things. The latest resulted from an overnight deluge in central and southeastern Illinois, with some areas registering 8 to 12 inches of rain in less than 12 hours.
It’s the third 1-in-1,000-year rain event in the Lower 48 states in about a week.
The National Weather Service office in Lincoln, Ill., has received about 20 reports of flooding, mostly due to water inundating roads and intersections. Television affiliate WAND in Decatur, which is about 35 miles east of Springfield, reported cars submerged in high water with emergency crews involved in rescues. Minor flooding of several rivers has also occurred.
Flash-flood warnings have affected a large swath of central and southern Illinois from around Springfield to southeast of Effingham. That’s where months’ worth of rain has fallen because of a parade of thunderstorms. Many of them were “training” or repeatedly moving over the same neighborhoods.
Even after the overnight downpours, storms appeared once again around sunrise Tuesday morning, drifting back over hard-hit areas that bore the brunt of the nocturnal drenching. It continued raining in the region through midday, with flash-flood warnings extending into the afternoon. It’s probable some areas will see rainfall totals surpass a foot.
“We’re still kind of waiting to hear on reports from some of the heaviest-hit areas, but based on radar estimates, we are seeing amounts of 8 to 12 inches across Jasper County, Ill.,” said Alex Erwin, a meteorologist at the Weather Service in Lincoln. “Late last night, before midnight, we received a seven-inch report from West Liberty in Jasper County, as well as a 5.5-inch report near Dundas in Richland County.”
Erwin said rainfall rates reached at least 2 inches per hour at times.
A dangerous combination of ingredients
The stalled front responsible for the torrent in southern Illinois on Monday night into Tuesday is the same one that produced flooding in St. Louis and eastern Kentucky last week. The former saw its wettest day on record a week ago; the latter faced disastrous flooding Wednesday night; at least 37 people were killed.
Ahead of Monday night’s storms in Illinois, forecasts called for damaging winds, hail and the chance of an isolated tornado in the Midwest and Ohio Valley. At least one tornado did touch down from the same string of storms to the east near the West Virginia-Pennsylvania border.
Beneficial rainfall was mentioned ahead of the deluge by the Weather Service office in Lincoln, but a flood threat was not highlighted in its afternoon forecast discussion. “It could be a nice rainmaker for us in central Illinois, with [total precipitation] values ranging from a few tenths, while localized values could exceed an inch,” the office wrote.
However, stalled fronts can prove notoriously tricky for forecasters, the clashing air masses and convergence, or gathering of air, serving as a focal mechanism for storminess. To the south of the boundary, atmospheric moisture was pooling; a measure of that — known as precipitable water — climbing to around 2 inches.
It’s worth noting that precipitable water isn’t a limit to how much rain can fall, especially in situations where the moisture is continually being replenished by the wind flow. It’s akin to wringing a waterlogged washcloth into a bucket. Even though the washcloth can only carry a finite amount of water, if you keep wringing it out and then getting it wet again, eventually that bucket can overflow.
The moisture collected on the stalled front, which sat atop a heat dome sprawled over the southern United States. It was pumped northward into the area by a zone of high pressure offshore the Southeast United States.
Monday night’s event fits into a pattern of ultrarare high-end rain events that have struck the United States in the past week. What happened in St. Louis and Kentucky both fall under the umbrella of 1,000-year rain events, meaning the amount of rain that fell during such a short window would have only a 0.1 percent chance of happening any year.
Similarly, Weather Service precipitation frequency charts for the zone southeast of Springfield, Ill., indicate that the foot of rain that fell in less than 12 hours from this event constitutes another 1,000-year event.
Human-caused climate change is likely playing a role in amplifying the severity and frequency of heavy rainfall events. For every degree Fahrenheit the air temperature increases, the atmosphere can hold about 4 percent more water. That disproportionately tilts the scales toward more exceptional events, and episodes like which have occurred in the past seven days will become more routine.
While there have been numerous reports of flooding in Illinois, it has not been as severe as in St. Louis and eastern Kentucky. In St. Louis, the large amount of paved surfaces meant the water had few places to go and overwhelmed drainage systems, while the steep terrain of eastern Kentucky diverted vast amounts of water into vulnerable valleys. In southeast Illinois, the terrain is relatively flat and unpaved, and thus able to absorb more water.
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