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West Pacific Tropical Action 2011


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There's some northerly shear... weak to moderate maybe, but maybe just the kind that makes cyclones slowly intensify, or plateau when around major status... high end 4 or 5 requires almost perfect conditions.

OTOH, if the upper ridge providing the shear moves little, then Ma-on would encounter less shear down the road.

Agreed, the asymmetry of the convection in the earlier microwave passes, not only in the eyewall but in the inner/outer band regions, have the classic northerly-shear look. It's been enough to slow intensification, but it appears that the shear has begun to abate.

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Surprised Joint Typhoon Warning Center is still forecasting Ma-on to intensify considering it is now crossing over lower SST's and has never overcome the presence of dry air to the north.

28C SSTs aren't exactly cool and if the stupid shear ever abates, everything else is still all systems go for intensification. They're surely basing it on the dynamical models showing further strengthening over the next 24-36 hours.

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Well, that ERC basically put an end to any serious intensification. It is totally blown out now.

I'm more concerned about the outflow on the Western side. Starting to look pinched, and I also suspect it won't get too much further West.

Its going to be kind of like New England or North Carolina, if it can just make it due North the coast comes out to meet it.

The Euro hasn't varied much in about a week.

msl_uv850_z500!Wind%20850%20and%20mslp!48!Asia!pop!od!oper!public_plots!2011071700!!chart.gif

post-138-0-73434500-1310908579.jpg

post-138-0-60292700-1310908590.jpg

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If only we could forecast when eyewall replacement cycles are going to go bad.

Adam, has there been any published literature about susceptibility of a TC during a EWRC to close proximity dry air? I don't have computer access currently (on my phone) Could that be a primary reason why some EWRC end poorly for the storm in the absence of significant shear. I have noticed EWRC tend to be much more successful (completion results in intensification) for storms in the Caribbean as opposed to the Atlantic, although SSTs could also be a factor here.

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Adam, has there been any published literature about susceptibility of a TC during a EWRC to close proximity dry air? I don't have computer access currently (on my phone) Could that be a primary reason why some EWRC end poorly for the storm in the absence of significant shear. I have noticed EWRC tend to be much more successful (completion results in intensification) for storms in the Caribbean as opposed to the Atlantic, although SSTs could also be a factor here.

None to my knowledge. When I was in Tuscon last summer, I tried to go to all of the ERC talks, but there just wasn't a lot there with the internal dynamics. Shear tends to cause the ERCs to take longer to complete, but beyond that, I don't know of any literature on them. Sounds like a good Google Scholar project today, if I get time.

I think your SST/dry air theory makes sense, though. The more thermodynamic instability available, the stronger the updrafts can become in the secondary wind max/rainband, and therefore the more quickly inflow can get cutoff to the inner eyewall.

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None to my knowledge. When I was in Tuscon last summer, I tried to go to all of the ERC talks, but there just wasn't a lot there with the internal dynamics. Shear tends to cause the ERCs to take longer to complete, but beyond that, I don't know of any literature on them. Sounds like a good Google Scholar project today, if I get time.

I think your SST/dry air theory makes sense, though. The more thermodynamic instability available, the stronger the updrafts can become in the secondary wind max/rainband, and therefore the more quickly inflow can get cutoff to the inner eyewall.

Cool. If there is in fact no study, I've still got a masters thesis that hasn't been decided yet :P

My hunch is that the size increase that occurs during EWRC may also help to ingest dry air that was previously outside of the of the dynamic environment that influenced the storm when it was a smaller radius.

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Folks on the W side of the cyclone will need to apply sunblock (SPF >15) if they venture out during the storm.

Gusting to 61 kts (10-min) at Miyazaki. I mean, it's not Cat 5, but that wind is higher than I was expecting from the IR presentation.

http://weather.uwyo.edu/cgi-bin/wyowx.fcgi?TYPE=sflist&DATE=current&HOUR=current&UNITS=A&STATION=RJFM

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