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A collage of imagery from Typhoon Champi's ultimate peak yesterday around ~18z — an absolutely beautiful cyclone with a stunning pinwheel eye & rotund CDO.
AI models have become pretty aggressive with TC development chances in the CPAC ~10-15 days from now. The large-scale environment is certainly supportive, with several overlapping equatorial waves driving a corridor of anomalous low level westerlies late next week:
Subsurface waters off the Indonesia have cooled substantially as of late, with low level easterlies firmly entrenched in the region thanks to el niño's background state. +IOD should strengthen significantly with trades to remain brisk, good signal for a mature +ENSO phase
(1) Arnab's swift strengthening over the past day has culminated this morning with a gorgeous satellite appearance. Troughing to the NW has opened up a large poleward outflow channel, which along with very hot waters, likely bolstered intensification overnight in spite of..
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#Infa flew a little too close to the sun early this morning, with stronger westerly flow aloft from the +PV streamer to its north. If the inner core structure remains intact, a secondary bout of RI is possible after 06z as the TUTT cell splits, considerably lightening shear
Since this post was made untimely, convection quickly rotated upshear & now In-Fa is on approach to major typhoon status. The system is enjoying a maximum of poleward divergence in a saddle point, where 10-15kts of outflow shear can be easily managed.
#In-Fa's current structure indicates the presence of moderate vertical shear, with repeated updrafts that initiate downshear struggling to rotate into the right of the shear vector. A nearby upper trough is driving moderate westerlies aloft.
Really struggling to understand why 98B isn't being classified as a tropical cyclone by the JTWC/IMD right now? One look at satellite imagery shows rotating convection over a tightly-wound LLCC, corroborated by a recent microwave pass revealing a formative mid-level core.
This is caused partially by 98B pivoting around a disturbance embedded within the monsoon trough (99A). This doesn't entirely negate the potential impacts for the region, however. As a result of this interaction, the TC slows down significantly near landfall, which is driving...
Gradual intensification can still be expected as SSTs are very warm: 29-30C, which is reflected in the convective intensity. Upper flow will flip to easterly through late Monday into the following afternoon as upper troughing fractures & ridging aloft takes hold.
The North Pacific jet is likely to extend significantly through early November given a couple factors. A large cold shot over east Asia will drive an +EAMT (east asian mountain torque) occurring in tandem with anomalous convective forcing over the Central Pacific



































