Incoming graduate student at the University of Arizona - Tucson, likes the tropics (a lot) UM ‘26 (meteorology, mathematics)

Joined September 2018
With significant external threats to NOAA, I figured it may be pertinent to discuss what TC forecasting looked like a mere half century ago. All images used in this thread come from the NHC — I will be focusing on 1974’s Hurricane Fifi, at 00z on September 19th.
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Deelan Jariwala retweeted
Argo float 4903516 has drifted very close to where #Polo stalled for an extended period at considerable strength. Although it has moved ~100 miles east in the past month, the difference in the subsurface is truly astounding -- from deep >30C waters to nothing warmer than 22C
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Deelan Jariwala retweeted
6.5 hours of #Champi's violent pinhole eyewall on visible imagery. Notice not only the continued core contraction, but also the particularly pronounced standing gravity wave in the southern CDO at close to peak intensity -- fascinating stuff
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Deelan Jariwala retweeted
Supertyphoon (cat-4-equivalent) #Champi’s track dipped to the south of Guam. While this makes the inner-core winds stay away from the island, peak winds over the terrain remain strong (>40 m/s) from the #PGUA radar velocity. Wind damage could still be a serious issue.
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Deelan Jariwala retweeted
Eye-tracked multi-tilt loop for the past few hours of Typhoon Champi from the PGUA radar showing all the eyewall mesovortices. Longer loop coming later!
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Deelan Jariwala retweeted
#Hurricane #Simon's track forecast today is exhibiting large uncertainty, related to it entering a COL in the steering flow or "saddle point". Here, small shifts in its initial position can result in very different track solutions. A visual helps explain things better👇
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Deelan Jariwala retweeted
New feature for cyclonicwx.com/interactive/: you now have total freedom with colormaps! Choose from the many pre-existing ones, create your own with a new colormap editor, or upload a CPT file and instantly import its colormap. Want to use one elsewhere? Export it to a CPT file or use the automatically generated Python snippet to use it for your own plots. Check it out by looking through the layers in the bottom right and clicking on the product you want to change
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Deelan Jariwala retweeted
I've had lot of conversations with other meteorologists I respect who feel strongly (with good arguments!) this wasn't a sting jet. There's a continuum here, though, and I'm not sure you'll ever fully satisfy the classic Browning definition of a sting jet with a transitioning TC.
Replying to @AriWeather
Our 12Z experimental HAFS forecast the day of landfall picked up on the structure pretty well, just showed it a little further offshore. It's not really a traditional "sting jet" at the base of the "comma head" because there wasn't one yet (hadn't really fully ET'd yet). But if you look, it seems like there was some really robust subsidence on the backside that likely brought strong winds down to the surface, similar to sting jet. Very interesting case that I want to dig into more.
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Deelan Jariwala retweeted
The 2026 eastern North Pacific #hurricane season (to 180°W) has now generated 319 ACE (Accumulated Cyclone Energy), breaking the old seasonal record of 318 set in 2018. #Simon
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Deelan Jariwala retweeted
Scene of 54 mph gusts in Hurricane #Isaias near Niceville, FL.
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I’m not really sure aircraft data today showed anything that resembles a warm front that close to Isaias’s center? Temperatures were reasonably axisymmetric in the vicinity of the core from what I can tell
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Deelan Jariwala retweeted
It's possible that the @NOAA_HurrHunter aircraft just measured the first solid evidence of vertical shear directly attacking the eyewall of Hurricane #Isaias. The last penetration measured an anomalous temperature spike at 750mb within the SW eyewall -—not within the eye—7C higher than the previously measured eye maximum. This might be evidence of a rapidly descending flow belt caused by shear laterally forcing external air into the eyewall region, leading to a massive subsidence inversion. This is often observed in high-resolution modeling (see HAFS sounding from this morning's 06Z run). The dewpoint also sharply decreased concurrent with the temperature spike measured by aircraft, supporting the possibility that this phenomenon was observed. This could foretell significant erosion of the southern eyewall in the near future, but time will tell. For now, Isaias remains as strong as ever according to the same aircraft data.
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#Isaias is trying its best to fend off the moderate vertical wind shear it is experiencing, with intense convection trying to push upshear over the last few hours. Of note is that the low-level windfield has symmetrized substantially, which may help it intensify tomorrow.
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Deelan Jariwala retweeted
#Isaias is getting itself together today. The newest recon finds a more coherent center, with some stronger winds close to the center and a 4mb drop in pressure from 2 hours ago. With the structure improving we'll likely see some intensification today. TDR will be interesting
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Deelan Jariwala retweeted
We are monitoring a tropical disturbance in the Bay of Campeche near the tail-end of a Gulf Coast cold front that could end up impacting Gulf states in a few days. While poorly organized right now, thunderstorm activity is increasing, and this system has a chance to develop into a tropical storm later this week. Environmental conditions won't be a slam dunk here. The cold front is associated with the upper-level jet stream, causing strong wind shear along the Gulf Coast that disfavors an organizing storm. However, the position of a series of shortwave troughs over Texas through ~Friday also facilitates strong upper-level divergence over the Gulf near a jet streak entrance region, which could help the disturbance fight off the wind shear a bit. Computer models are splitting into two broad camps: 1. Most AI-based models (see AIFS example) show the system moving northeast more quickly, prior to the Texas shortwave trough lifting out. This would place the storm in the most favorable position to intensify, and would bring it into the central or eastern Gulf Coast by the weekend. 2. Several physics-based models (see ECMWF example) are slower to lift the disturbance northward, allowing the Texas shortwave to exit and the favorable jet dynamics to subside, giving way to a more purely hostile environment for a potential tropical storm. The result is a weaker, messier storm that waits until next week to attempt a move toward the Gulf Coast, if ever. Significant uncertainty remains in this scenario, but this disturbance is one to watch this week. Even if a strong storm is avoided, heavy rains may stay in the forecast for portions of the Gulf Coast. Keep an eye on the forecast from the National Hurricane Center, which currently gives a 70% chance of a tropical cyclone forming.
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Deelan Jariwala retweeted
NHC has completed its post-analysis and Tropical Cyclone Report for Hurricane #Genevieve (July 24-August 2, 2026). The report can be accessed at nhc.noaa.gov/data/tcr/EP0720…
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Deelan Jariwala retweeted
New data has come in from Argo platform 3902386, located very close to where #Polo stalled as a powerful category 5 (15.35, -101.94). While SSTs have not changed much, the deep subsurface warmth (previously >30C extending to a depth of over 80 meters) has been exhausted.
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Neat example of eyewall mesovortices merging together during the intensification process in Hurricane #Nolo this evening. Can see the progression from a high wavenumber state to essentially a monopole over the last 6 hours or so.
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Deelan Jariwala retweeted
Had a good (final for me) flight into #Polo today. It was down a couple notches from its beast mode earlier last week, but still a powerful major hurricane. The eye even cleared out a bit again during our flight. It was especially fun to get to fly with a few UM/CIMAS/HRD people on their first flight!
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Deelan Jariwala retweeted
Now that the nor'easter completed its phase with a tropopause vortex and is decidedly non-tropical, let's look back at its structural evolution over the last day and a half, and why despite attempting to start the tropical transition process, it fell short of classification:
The much talked about nor'easter is now well underway, with a large cyclone producing widespread rain and significant coastal flooding slowly making its way north. Slightly technical thread discussing its structure and forecast: 🧵
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Fantastic example of an occluded low sitting off the NJ coastline. I have seen a lot of discourse about this feature requiring an NHC classification of some sort, and this image makes it very clear why that isn’t the case.
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This is an unusually long post on something relatively mundane, but I figured it would be worth putting my two cents out there as someone who worked @ the NHC reanalyzing historical hurricane seasons for a few years.
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Posts like this are conflating weakening due to lack of surface fluxes (this system has been over cold water for all of its life and has no deep convection anyway) with the typical weakening seen after occlusion when baroclinic processes wrap up.
This has had eye for 24 hours. There’s no precip left around it and it’s weakening as it should be weakening if it were a warm core system which it is. Why would it weaken? because it’s coming over a cooler water
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