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About Windspeed

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Four Letter Airport Code For Weather Obs (Such as KDCA)
KTRI
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Male
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Location:
Tri-Cities, TN/VA
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Geography, Climate and Geoarchaeology.
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The Mexican shoreline is getting raked by Simon. However, Simon's small core is a frog's hair distance offshore to avoid weakening versus strengthening any further. It's a delicate balance that's preventing Category 5 intensity but not yet detrimental enough to induce weakening. Still, the abrupt change in elevation near the coast and such influence on inflow will still disrupt Simon and should begin to weaken it if the core parallels the coast any closer. Granted, that means very little with respect to flash flooding that is underway with moist low-level southerly fetch within the eastern circulation feeder bands and orgographic lift.
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It seems like we always have to beat it into people's skulls during landfalls. It's the maximum sustained winds possible as an estimate over water for a reason. It's a marine storm before it is a land storm, and advisories have to account for what is occurring in real time over the ocean surface for any poor ships/souls that might find themselves in the worst scenario. But due to frictional convergence / drag, you will almost never see those sustained winds over land unless you have a super intense eyewall with embedded multiple mesos rotating around that overcome frictional forces with insane ground level velocities. As a general rule, the highest wind reports over land are always in gusts due to this process. You might get those highest sustained winds right on the immediate beach/shoreline perpendicular to the onshore motion of the inner edge of the eyewall, but the equipment would need to be in the right place at the right time and that is exceedingly difficult placement and timing to pull off. Interestingly, and as no surprise, the instrument anemometers that have been positioned in the right place and at the right time during past landfalls that recorded sustained winds near maximum have generally failed during that event. I also need to add that the reason most immediate advisory packages don't rapidly ramp down maximum sustained winds after landfall is twofold: 1) part of the eyewall or outer eyewall may still be over water, 2) any large estuaries even after landfall may still experience maximum winds. Once the entire circulation is inland, subsequent advisory packages tend to ramp down quickly.
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Simon appears to be doing what most EPAC hurricanes have done this year. It's undergoing rapid intensification. A pinhole eye has formed in the direct center of the tiny CDO. This is a microcane for now and on it's way to becoming a major hurricane today. It will most likely grow in size over the weekend. It's tiny core will expand, and the pinehole eye should give way to a larger eye eventually.
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4:00 AM CDT Fri Oct 09 Location: 26.4°N 88.0°W Moving: NNE at 15 mph Min pressure: 963 mb Max sustained: 110 mph
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Satellite continues to improve, and we have a warming clear eye now. Category 3 is looking much more likely. If they don't pull the trigger in the 4AM CDT package, they probably will later with an intermediate advisory.
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Best structure Isaias has had in its lifecycle so far. Perhaps a window here for some brief intensification prior to increasing shear today.
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I am starting to lean into a major being a real possibility, but I still anticipate it getting hammered in the mid-levels prior to landfall. Wouldn't even be surprised if it got decapitated. 30+ kts of shear is still going to win the battle, regardless of the vector of motion and all other favorable factors. Keep in mind that some of the 500 hPa barbs of flow may be in excess of 50 kts by landfall. I would still be cautious of early onset RI being a sure thing as well. It may thread the needle, but you can clearly see assymmetry already in the cloud pattern, and the coldest tops are NE of the surface circulation. It may be slower to moderate intensification instead if it gets hampered by westerly flow. You can easily see this flow on satellite moving in quickly from Mexico. Again, RI is a possibility, but absolutely not certain.
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Looks like we're going to have quite a battle of timing and walking thin ice with that shear axis. Might be a back and forth between 6 hr runs on the TC model suites today until they get a better feel for track motion, and if/when the mid-level shear begins encroaching. For example, the 18z HAFS suites kept intensity in check, preventing a major. The 00z suites kept the core on the edge and bombed Isaias into a strong major. The recent 06z runs are back to allowing encroachment in the mid-levels again, though it may still be reaching Category 3 / 960s prior to weakening. We'll have to see if the 12z suite swing back to flirting with the 940s and a more significant major.
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Best track is now 35 kts and upgraded to TS Isaias for the next advisory package.
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00z HAFS suites are significantly stronger versus 18z. Intensification is faster, with a major hurricane down into the 940s passing east of the mouth of the Mississippi River. Both still show disruption from increasing shear by landfall, but obviously, this would be troubling for surge impacts along the Mississippi, Alabama, and western Panhandle coastline.
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Intense bursting of convection now over the NHC's 10PM CDT advisory position:
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https://isotherm.rsmas.miami.edu/heat/weba/atlantic.php for updated TCHP maps. Sadly, many of the old NCEP and CPC sites are MIA these days for oceanic and atmospheric data.
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The first runs of the HAFS suites since classification are not impressive, to say the least. The TC gets walloped around 70'ish hours out and becomes very assymetric with advected dry air doing its thing. Something to keep in mind. Is the window there for a strong hurricane? Sure. But the TC needs to come together rapidly over the next 48 hours.
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Right now is the slowest motion we will see. The westerly steering flow in interaction with the mid-to-upper trough will push the TC towards the east and then begin to turn it poleward. At that point, it should be gaining forward motion into landfall.
