• Hello, please take a minute to check out our awesome content, contributed by the wonderful members of our community. We hope you'll add your own thoughts and opinions by making a free account!

Tropical Major Hurricane Michael

Curious to see what the 12z global models look like today but this right here is a tight cluster...

AL14_2018100912.png
 
Yeah agreed think strong likelihood this makes into a solid cat 3 over next 24 hours and still has a shot if atmosphere behaves of getting to a 4
 
Eric, what are your thoughts on the transition and interaction of Michael as it moves across NC? I'm noticing some models are enhancing the west side, possibly due to some baroclinic influences as it is transitioning to extratropical? Euro wind gusts are pretty concerning for coastal NC with gusts over hurricane force... realistic or is the Euro out to lunch here?

The Euro wind gusts are likely overdone to some extent as was the case w/ Florence but they could be enough to bring down trees and power lines. The enhancement of precipitation on the west side of Michael is a classic, left of track case with a positively tilted trough approaching from the northwest, interacting additively with the cyclone to enhance rainfall due to large-scale quasi-geostrophic ascent, frontogenesis, upper level divergence to the north of the cyclone, and isentropic lift w/ warm tropical air gliding up isentropes into the relatively cooler air aloft to the N and NW of the incoming cyclone. The easterly wind north of the cyclone also helps triggers a geostrophic adjustment process whereby some cold air damming is favored, which only acts to increase lift and precipitation. Contrary to popular misconceptions, you don't necessarily need to have a strong high to the north in New England or SE Canada every single time to get a CAD event. Even near or slightly below normal MSLP north of very low MSLP to the south via a hurricane for example still generates the same large-scale pressure gradient fore and easterly wind needed to produce cold air damming. Buoyancy is obviously way different in the warm season however and the amount of time the easterly wind will be present north of Michael is limited by its rapid forward movement so it'll only play a very minor role in this case but it's non-zero and can't be entirely ignored. Orographic lift will also contribute to precipitation amounts especially over the western piedmont, foothills, and mountains of NC particularly if Michael tracks over or west of central NC.
 
Back
Top