kayman Posted 11 hours ago Share Posted 11 hours ago I do wonder if the low-level circulation is reforming further south near the mid-level circulation in Bertha. Link to comment Share on other sites More sharing options...
Chinook Posted 7 hours ago Share Posted 7 hours ago what a weird tropical storm surface low by Louisiana convective storm far south 1 Link to comment Share on other sites More sharing options...
vortex95 Posted 1 hour ago Share Posted 1 hour ago 6 hours ago, Chinook said: what a weird tropical storm surface low by Louisiana convective storm far south You can see the mid-level center spin on radar near CRP currently. Talk about a tilted vortex sfc to mid-levels! This one of the most "disconnected" TCs I think I have ever seen. Great case study. The ECWMF handled this evolution very well. Compare its 925 mb RH/streamlines to its 500 mb RH streamlines, and the disconnect was fcst very well. This is about as far as you can get from a classic TC structure, but they exist on a *spectrum*. You can't use textbook examples all the time for what actually occurs in the real world. So both Arthur and Bertha were odd ducks, and even for sheared TC, more atypical for this variant of a TC. It also shows how the models still struggle w/ initial TC genesis for systems like this. Pre-Bertha was a non-tropical low that appeared it would remain broad and cold core, and strong shear was factor. Not that the models can't handle non-tropical to tropical transition, but the overall environment was not favorable, so that likely influenced the models. Yet the system still managed to form a large, solid LLCC in the mid 990s. 1 Link to comment Share on other sites More sharing options...
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