Sctvman
Member
Environmental agencies are going to want to claim some of these new river beds. River flow has changed. In many cases you won’t be able to rebuild your home or rebuild a road. If you sailed over on the Mayflower and sent out an expedition into WNC to find a place to build a town, would you choose one of these places if the landscape looked the way it did right now? We saw a thousand years worth of landscape alteration in a couple hoursIs there anyway to even rebuild some of these roads or towns? Like chimney rock, where do you build when on both sides are steep eroded slopes and what was once buildable collapsed into the river
it will be months, if not years. suffice to say there will be plenty of studies on this storm that will leave no stone unturned regarding synoptics, intensification, mountain meteorology, ull interaction, quantifying how much climate change juiced this, communication/messaging, etc. it's the kind of event my old synoptic professor would assign as a capstone event to analyze. but for now i think it would be in bad taste for the nhc or anyone affiliated to be spitballing about what went wrong with the eastward tug. one disconnect is that the core became decoupled from the actual LLC center as it trudged inland, so the forecast may have "technically" been alright but tell that to people in spartanburg.Did nhc ever come out and explain why they went against modeling and made such a bad forecast the day before the storm?
i'm also interested in this. growing up when my fam went to the mountains we would take 74 the entire way from wilmington to dillsboro and stay at the best western on the river. fond memories of waking up and screwing around on the bank and waving to the rafters. growing up i was also a big train guy and we would take the train from dillsboro that traced along the tuckasegee (forget the terminus). i really love that area, doing random "gem mining", driving along that highway with all the waterfalls around franklin. my first guess is that they had bad but not unprecedented flooding based on where the core of helene wound up.@ Met1985, How did the area from Cullowhee back up to Highlands/Cashiers then down to Dillsboro fare? The Tuskegee River. I saw that area river flood with mini icebergs post 1993 Superstorm. Can't imagine it did any better from this. Rural area back up to Highlands/Cashiers from Cullowhee
don't want to wade too far into this arena but I've read that the air traffic in the mountains is substantial, someone compared it jokingly to Newark. i know the private hellis are well meaning but this is probably a precaution so the airspace isn't so clogged upHelli's being turned away, no reason giving. Glenn covers this subject about private Helli's being shewed away and unfortunately all those here-says are true. Dont understand why, Hellis are your ambulance service next several months at minimum.
Looking at the sat imagery its clear that geologically speaking this level of flooding has not happened in a very very long time, definitely thousands if not 10's of thousands of years. There will be no rebuilding in many of these locations, they will have to literally start new versions of these towns where they can find suitable land which typically is found in valleys alongside streams and rivers etc...
It completely changed river channels, essentially the river now runs through what was the main strip in Chimney Rock, saw other examples on this when looking at Sat comparisons from a couple weeks ago, so it’s not an isolated case. And the velocity needed to love those boulders is just nuts, I have a chart laying around somewhere on water velocities required to move different objects, basically everything from sediment particles up through VW but sized boulders, if I can find it I’ll post it.
That’s all fine. But this wasn’t an unexplainable or unexpected miss… the llc tracked exactly where the model consensus showed it going the day before.it will be months, if not years. suffice to say there will be plenty of studies on this storm that will leave no stone unturned regarding synoptics, intensification, mountain meteorology, ull interaction, quantifying how much climate change juiced this, communication/messaging, etc. it's the kind of event my old synoptic professor would assign as a capstone event to analyze. but for now i think it would be in bad taste for the nhc or anyone affiliated to be spitballing about what went wrong with the eastward tug. one disconnect is that the core became decoupled from the actual LLC center as it trudged inland, so the forecast may have "technically" been alright but tell that to people in spartanburg.
i'm also interested in this. growing up when my fam went to the mountains we would take 74 the entire way from wilmington to dillsboro and stay at the best western on the river. fond memories of waking up and screwing around on the bank and waving to the rafters. growing up i was also a big train guy and we would take the train from dillsboro that traced along the tuckasegee (forget the terminus). i really love that area, doing random "gem mining", driving along that highway with all the waterfalls around franklin. my first guess is that they had bad but not unprecedented flooding based on where the core of helene wound up.
don't want to wade too far into this arena but I've read that the air traffic in the mountains is substantial, someone compared it jokingly to Newark. i know the private hellis are well meaning but this is probably a precaution so the airspace isn't so clogged up
Tree removal underway over at my in laws View attachment 152544
I don't have velocity numbers but I know the discharge on rivers across the regions were incredible. For example the South Toe's discharge hit 18,400 cubic ft/sec before the sensor went down. It could have easily peaked in the 20-30k range. For those who aren't familiar with discharge, it's the volume of water flowing through a river at a given time. To put this in perspective, the Potomac at DC averages ~11,000 cfs, and the Hudson at NYC is ~20,000 cfs. I can't find any sensors near Chimney Rock but at a glance the South Toe and Broad look similar in size. You basically had the equivalent of the Hudson River flowing through that tight valley which is mind-boggling.It completely changed river channels, essentially the river now runs through what was the main strip in Chimney Rock, saw other examples on this when looking at Sat comparisons from a couple weeks ago, so it’s not an isolated case. And the velocity needed to love those boulders is just nuts, I have a chart laying around somewhere on water velocities required to move different objects, basically everything from sediment particles up through VW but sized boulders, if I can find it I’ll post it.
It’s not good down here in South GA. Pine forest wiped, orchards wiped out, and chicken houses wiped out. A lot of lively hoods have been lost and communities that already weren’t the wealthiest. Most of these communities in South GA weren’t prepared for what they got because they expected the track to stay west. It’s a disaster from Florida to North Carolina that’ll take years to recover from.I have seen anything yet, but I’m guessing there will be something in the storm case study when it’s released. Let me say that as critical as I have been about the NHC forecast of the storm track, I don’t believe it made a big difference in the amount of rainfall and flooding experienced in WNC. I do think that it was a big deal for people in the Augusta area and NE GA and SC Upstate… those areas experienced a direct hit from what was left of the storm’s eyewall, something that by the NHC tracks should have happened a good 100+ miles west
I don't have velocity numbers but I know the discharge on rivers across the regions were incredible. For example the South Toe's discharge hit 18,400 cubic ft/sec before the sensor went down. It could have easily peaked in the 20-30k range. For those who aren't familiar with discharge, it's the volume of water flowing through a river at a given time. To put this in perspective, the Potomac at DC averages ~11,000 cfs, and the Hudson at NYC is ~20,000 cfs. I can't find any sensors near Chimney Rock but at a glance the South Toe and Broad look similar in size. You basically had the equivalent of the Hudson River flowing through that tight valley which is mind-boggling.
South Toe River Near Celo, NC
Monitoring location 03463300 is associated with a Stream in Yancey County, North Carolina. Current conditions of Discharge, Gage height, and Stream water level elevation above NAVD 1988 are available. Water data back to 1957 are available online.waterdata.usgs.gov