Windspeed

Considering the numerous videos floating around on SM showing direct hits or close calls by flying debris unleashed by extreme winds on pedestrians, motorists and especially motorcyclists, I am left to wonder at how little these populaces disregard official warnings (or the lack thereof) to protect life and property. For all of the flak Americans get for riding out TCs, at least most of us heed warnings and stay sheltered. Another thought that crosses my mind is even more sobering. The struggle to keep a job for basic survival forces folks to risk life and limb. People can bitch and moan at the disruption a TC will bring to a region, but I am very relieved and proud that we have the societal structure and system of government in place to not only protect our citizens, but help them manage the survival part so they aren't forced by some shitty corporation to either bleed or starve.

Yagi continues to re-intensify and is now a Category 4 equivalent as explosive convection with HTs wrap the eye. Dire situation unfolding. Densely populated region at or below 2.5 meters (8 feet) -- essentially infrastructure built upon a river delta. The shallow gulf combined with shape of the coastline within the northern half of the circulation may funnel surge into these low-lying urban areas.

Yagi may be the big bad TC of 2024. That's not to downplay Shanshan's flooding impacts to Japan. Yagi has already caused severe flooding in the Philippines, smacked a densely populated city (Haikou) at Category 3+ intensity, and appears to have reintensified now prior to densely populated port cities in northern Vietnam. I can not recall a typhoon ever this strong impacting the Haiphong and Ha Long metropolitan regions in the satellite era. I am worried about potential storm surge up the estuaries there. Yagi may have been moving just slow enough to regain fetch in the Gulf of Tonkin.

Klotzbach weighs in again.

Fair enough. I think we're all just a bit stressed trying to resolve what is going on versus the 20-25% failure mode. What factors are essentially countering other overwhelming favorable data points. Additionally, all hell could break loose in two weeks. We get complacency. Peak merely got delayed until mid-to-late September this year when all these countering factors subside.

If I put you on the spot, well, you just made a post inquiring pros and cons about stepping away from the pack. So without empirical datum, you just played devils advocate and went with average numbers knowing if a 20-25% failure rate of climate precursors resolves, you are sailing to victory and looking quite brilliant and bold. lol... I appreciate the honesty versus jumping on the WAM strength/OS Index/Tonga (*barf*)/+NAO etc., etc... things we are trying to resolve in situ. I should also point out that you can still have a hyperactive season and only have 13 named storms based on metrics being ACE. Granted, that means the insanity of nearly all TCs being long-lived hurricanes or powerful majors. At any rate, I digress. I am pretty sure we know what you meant by hyperactive.

Better yet, what was your reasoning in only going with 13 named storms in the face of overwhelming model and climate parameter support for a hyperactive season? I mean, you're sharing your numbers while knowing full well the majority of the best TC climatologists on the planet are scrambling for answers. 13 named storms is barely average.

Welp...

The MDR wave from last week's big AEW is gaining a robust convective envelope tonight. It's worth watching just to see if it pulls off some quick development through late week. There is an upper trough that is modeled to amplify north of the Lesser Antilles in 3-4 days that will likely impede the system with strong shear regardless. But in the meantime, perhaps it can grab a name and end the drought.

Yeah, if deeper convection remains absent, dominant vorticity or an amplified wave remains nothing more than a feature of interest until environmental conditions improve.

Despite the anemic appearance, the MDR disturbance east of the Lesser Antilles actually looks better organized this Sunday morning. The axis of the resultant wave that's developed out of the ITCZ breakdown is quickly folding around dominate 850-700 hPa vorticity. Shallow convection has aided this process. Granted, we need deep convection to take over now to allow this vorticity to ramp up at the surface to spawn TCG. But the stage has now been set. We do not have competing vorticies along the boundary of the old MT but more of a stand-alone easterly wave structure. If deeper convection begins to fire and wrap into fold, the wave will likely get labeled an official invest. Without competing centers of vorticity, it may not take long for development to initiate TCG in the ECARIB. We may even see this all go down on radar out of Barbados.

Essentially, the ITCZ is a boundary of convergence at the surface between equatorial and subtropical latitudes. A trough is, by definition, a region of covergence due to lower pressures. So you may interpret the ITCZ as an elongated monsoonal trough that stretches loosely with longitude around the globe. However, in normal meteo/climo applications, we usually stay off classifying a monsoonal trough unless there is a large or very broad region of cyclonic windflow anchored to the ITCZ with many multiple competing surface vorticities. The reasons should be obvious here. We may see the ITCZ stretch over long distances, but a large embedded surface trough will bend the boundary cyclonically into it. It can also significantly enhance larger clusters of convection spreading airmass dilffluently into jet channels above 700 hPa level. Depending on size, strength, and latitudinal placement, MTs can be a nebula for spawning TCs or a deterrent. In the case of our current central MDR disturbance, that MT is breaking down into a region of tighter vorticity within the ITCZ. Modeling is currently evolving that surface vorticity into a TC. So, in this case, the MT would be a harbinger of TC development. Whereas the large MT over the African Sahel the past month had been a deterrent for TC development due to bending the ITCZ further north in latitude and kicking AEWs into NW Africa. Hope this helps.

@WxWatcher007 The last few OP runs are trying to close off tighter vorticity out of the decaying trough remnant between 24 and 48 hrs. Deep convection begins consolidating by Saturday. In other words, if the ECMWF (and GFS a bit later into the 72 hr range) were going to verify, we shouldn't have long to wait to see signs both convectively and cyclonically in the next few days. 594 dm heights positon to the north of this potential system, therefore, as soon as vorticity ramps up with the hypothetical TC, it immediately gets kicked into the easterly steering layer on both the 12 and 18z runs and becomes a Caribbean Cruiser until late in the midrange. Eventually, the ridge breaks down, allowing a northerly turn. Furthermore, an ULAC builds over much of the Caribbean on timing with a TC moving through the region. I have to admit. The OPs are simulating one hell of a potential setup for a powerful Caribbean hurricane. All big grains of salt though until we see actually start to see when and where vorticity ramps up.

Though the western MDR looks pretty meh as far as the surface trough breakdown, both ensemble suites seem to like something to organize out of that feature. If something were to develop and move WNW, that wouldn't be ideal as both the ECMWF and GFS have a ULAC pivoting with the general upper flow to over the Bahamas by 96-120 hours. Barring land interaction with the GA, a hypothetical TC would have excellent upper support.

This same AEW is now SSE of the Cabo Verdes and remains quite convectively active. No surprise that global ensemble suites are now picking it up. Regardless if we get development out of the western MDR from monsoonal trough breakdown, it does appear this new wave in the eastern MDR may have enough organization to develop. Future track may lead into the central Atlantic however. As of current time, the 7-day outlook from the NHC has yet to mention it. But if the wave continues to remain convectively active, it wouldn't surprise me to see it show up on the 2AM. As mentioned before, this AEW appears to have an embedded low at the surface. There is also a beefy 700 hPa easterly jet incoming from interior Africa, but the AEW may be able to stay out in front of this feature with a mid-level trough digging to the NNE. I like this system and I do think we will get TCG sometime over the weekend as environmental conditions should remain condusive.

Yes, instead of one negative factor versus another (700-500 hPa shear versus downslopping), or slow motion and upwelling, it's more a combination of all factors weakening the typhoon too much convectively to sustain the higher-end TC modeling outputs from previous days. Interestingly, Shanshan did maintain a stable peak and large eye while in what was essentially a 24-to-36-hour stall in the Amami islands. It was not much of a surprise since that region of sea had a much deeper 26°C isotherm of over 100 meters.

Dr. Jeff Masters and Bob Henson break down the much-discussed quiet August period of the 2024 Atlantic hurricane season: Where are the hurricanes? The Atlantic’s late-August nap may lead into a stormy September

I'm not convinced that westerly shear is the culprit for weakening here. I think the problem a TC experiences in its current location is downsloping off of Kyushu's mountainous terrain. About 12 hours ago, there was a pass that showed significant deformation in the eyewall and a replacement cycle in progress. Then, the entire western band disintegrated as the northern circulation moved over the greater Kyushu landmass. If you watch satellite and radar animation through the same timeframe, it's rather neat to see the landmass of Kyushu having effects on Shanshan's structure. I agree we're looking at a Cat 1-2 in windspeeds, most likely. But in hindsight, this is a massive typhoon and large circulation. A dangerous situation is unfolding if it continues to crawl at a slow pace through landfall and progresses slowly over the Kagoshima prefecture. Precipitation amounts may lead to a historical event, unfortunately.

Shanshan is now a Category 4 typhoon. The storm is crawling, but its large symmetrical eye is maintaining a very stable and steady state. It is churning up deeper water, but not feeling its own effects of upwelling due to the 26°C isotherm being over 100 meters deep currently in that part of the NW Pacific. High TCHP is critical for slow-moving large TCs to maintain such intensity for long durations.

A vigorous AEW should be exiting south of the Cabo Verdes by Wednesday. This disturbance is at a lower latitude and has intensified over the past 24 hours. The cyclonic spin is quite noticeable beyond a typical mesoscale feature and may already have an organized low. Based on its look and latitude, it has my attention. Note that the image was sourced from Meteosat and not GOES to get a better perspective of the wave at 5°W to avoid distortion.

Shanshan completed an ERC and now has a larger diameter eye. For now, it looks like the Kagoshima Prefecture will take the brunt of landfall. There is also potential for a stall inland over Kyushu before moving back out over open water. Modeling has not performed the greatest with Shanshan up to this point, however, not handling the steering layer well around large features such as the typhoon's interaction with the mid-to-upper cutoff and weak steering flow with a potential block to the north.

Excellent thread by Kaylan Patel covering the quiet August stretch. He includes the abnormally strong monsoonal trough latitudinally displacing WAM/ITCZ like we have also discussed and also mentions a stable upper troposphere over the MDR. He mentions the +NAO and SPH placement tapping SAL. But I do like his play-by-play of the resulting pattern here: He also alludes to the EPS and GEFS showing the monsoonal trough weakening. These are all topics we've covered above but a nice succinct thread here. Just to show a lot of discussion ongoing across SM by the pros and further implications that the quiet period may be closing.

Yes. lol, interestingly enough, the sudden drop in the meridional and equatorial Atlantic doesn't seem to have weakened the WAM at all in July. In fact, WAM did the opposite and dominated. Perhaps one of the strongest in decades, influencing above normal precip across Sub-Saharan, Sahel. But it must be noted that precipitation has been above normal from the Arabian Peninsula to Morocco. So it's not just West African. Something else is going on, but it does look as if WAM is finally weakening or backing off into a more supportive state for lower latitudinal AEWs. Edit: I should also clarify that if you want MDR TCs during ASO, you actually want there to be an active WAM in June and July but does not go completely away. If you have no WAM, AEWs are significantly limited in frequency and organization to limit MDR TC production. However, as we have seen this past month, an overly aggressive or potent WAM allows AEWs to gain too much latitude. SPH placement still pulls SAL into that region North of the CVs, not to mention cooler SSTs for thermal support.

That is referring to the equatorial and meridional Atlantic Niño/Niña SSTa oscillation. Generally, AN SSTs enhance the WAM and ITCZ. BN tends to weaken them. There is a paper on this if you're interested. An Atlantic Niño can enhance the MDR where as a Atlantic Niña can limit the spawn of AEWs. But it's not as impactful versus ENSO's influence and other factors. You can still get an active MDR if meridional SSTs are BN. Atlantic Niño can enhance in combination with -ENSO, but certainly won't counter a moderate +ENSO. https://cpaess.ucar.edu/meetings/2021/pirata-24/abstracts/atlantic-ni%C3%B1oni%C3%B1a-influences-atlantic-tropical-cyclone-activity I should also add that the article you posted above isn't also referring to the SSTs across the North Atlantic basin. They are still very much above normal.

Shanshan has positioned itself in a more favorable environment now for rapid intensification. The features that were holding it in check are now aiding in ventilation. Over the past few hours, intense convection has wrapped the core of the typhoon. Hopefully, the TC doesn't go too crazy and become a super typhoon prior to landfall.