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Hurricane Season 2012 Gets Started Early with Tropical Storm Alberto

Visible Imagery of Tropical Storm Alberto

Visible Imagery of Tropical Storm Alberto

Hello everyone, and welcome to the start of the 2012 Hurricane Season, being abruptly started by an early season tropical storm, Alberto. This will be a short update, as I am pressed for time, but I wanted to get this update out here today as soon as possible. Alberto’s genesis was relatively unexpected, with neither the GFS or ECMWF really picking up on the feature, even as of the 00z runs last night. The National Hurricane Center (NHC) in fact as late at this morning had the probability of genesis at 20%. However, starting last night, well defined spiral banding on radar reflectivity started to develop, which lead to increasing winds, and lowering pressures near the circulation center. When ASCAT confirmed the presence of tropical storm force winds confined close to the center and convection persisted from a 12-18 hour period, the storm met the full criteria of a tropical cyclone. Maximum sustained winds are at 45 mph, and the track is expected to drift southwest for the next 24 hours or so before a mid-latitude trough picks up the system in the later half of the forecast. However, any deviation to the west of the NHC forecast track could put the storm close to the coastline of SC/NC so tropical storm watches/warnings may be hoisted up as soon as tonight, so be on the lookout!


I’ll try to post a more detailed update tomorrow time permitting. Until next time!

Update: Pressure is down to 995 mb and the winds are up to 60 mph, mainly based upon a recent ship report near the center.

Irene Now A Hurricane… US Landfall Looming on the Horizon

Tropical Activity For August 22nd, 2011

We finally have the first hurricane of the 2011 season! Irene became a hurricane last night and is now traversing between Puerto Rico and Hispaniola with eyes eventually on the Southeast coastline. Harvey has finally dissipated, and 98L continues to be a non-threat for development. Thus, I’ll once again primarily focus on Irene for this discussion.


Hurricane Irene

Visible Loop of Hurricane Irene

Hurricane Irene has continued to move more rightward than expected, and it has now cleared Puerto Rico and is now currently in between Puerto Rico and Hispaniola. Over the last 24 hours, the presentation of the storm has improved, with an eye appearing on microwave imagery, radar imagery, and in recon observations. In addition, recon observations earlier showed that this system continued to track towards the west-northwest at around 290 degrees. More recently, radar observations show that this motion has persisted but slowed a little bit. While visible satellite imagery shows some evidence of dry air on the NW flank of the system, more recently a large blow up of convection near the circulation center shows evidence that this dry air is not being ingested into the core circulation of Irene. However, the close proximity of the circulation to Hispaniola will likely slow or prevent development for the next 18-24 hours. Beyond this time though, a well defined anticyclone continues to persist over Irene, and this along with ample Total Precipitable Water (TPW), and very warm sea surface temperatures exceeding 30 degrees Celsius in spots could lead to rapid development beyond Hispaniola. Beyond this time, the track still remains the big question.

72 hour 500mb heights and Sea Level Pressure From the ECWMF, GFS, GGEM, and UKMET

Plotted above is the 72 hour forecast plots for four of the most widely used global models for tropical cyclone tracking. The most interesting things to note in the early going is that the GFS seems to be the most progressive with the initial east coast trough which allows for a larger weakness initially. The ECWMF still has a bit of ridging that should keep on a slightly more westward track. The GGEM is strange, because it has the same weakness as the GFS, yet does not have as progressive of a trough. Once again I feel that the GGEM may not be handling all the global features correctly and is not considered a very likely solution. On the other side of the spectrum, the UKMET is by far the strongest with the ridging, and this solution is considered a leftward outlier at this time.

96 hour 500mb heights and sea level pressure for the ECWMF, GFS, GGEM, and UKMET

Moving on to day 4, we see that the similar model evolution. The GFS continues to be the most progressive with the first trough, but is also tries to develop a mid-level ridge back over Irene. The ECWMF is the least progressive with the trough, yet it also continues to have a little bit of ridging nosiness north of Irene, keeping it on a slightly west of north track. Its a little strange to see the GFS show more ridging yet have a further eastward track. The GGEM looks like its trying to pick up Irene somewhat from the first trough and this solution is still considered unlikely at this time due to GGEM’s lower verification scores with the weather pattern beyond day 3. UKMET continues to be a western outlier, but has a very similar ridge pattern in comparison to the GFS. My hunch is that while the UKMET is likely too far west, the GFS is also a little bit too far east with Irene.

120 hour 500mb heights and sea level pressure for the ECWMF, GFS, GGEM, and UKMET

Finally we reach the end of my forecast period at 120 hours, when the second trough, the system that expected to pick up Irene, arrives. Due to this late forecast period, the models are literally all over the place with regards to how intense this feature is, although the placement in most of the models doesn’t seem to be as bad. The first think you might note is that the GGEM is well to the NE with Irene from the rest of the global model guidance. This is partially due to the unlikely consequence of the first trough trying to pick up Irene but failing to do so. The solution is strange because the second trough is weaker on the GGEM than any other global model so I’d consider this solution highly suspicious. The GFS is the second furthest east, but this solution makes sense synoptically considering how strong the second trough is depicted in the modeling. Finally, we are left with the ECWMF and the UKMET which both show the system further southwest with a weaker second trough taking longer to pick up Irene.

So great, that’s a lot of analysis of a bunch of model plots, but which one is right. As you probably suspect from my rant above, the GGEM doesn’t seem like a logical solution looking at the upper level pattern in the model. So I’m throwing that model out right from the get go. Thus we are left with the ECWMF, GFS, and the UKMET.

Recently, a NOAA P-3 aircraft is conducting a Gulstream – IV Mission that will sample the atmospheric environment around Irene over the next few hours. The data obtained from this mission will be fed into the next model cycle (00z). However, the data is already available publically now, and we can already infer a few things about the dropsonde data. First of all, dropsonde obs indicate that the mid-level ridge is actually slightly stronger than the GFS model was suggesting at this time earlier today by around 10-20 meters. This might not seem like much, but every little height rise unaccounted for could mean a further west track trend in the modeling when this data is ingested. In addition, the dropsonde soundings closer to the storm show that the 500mb heights were actually a little lower in reality than in the model progs. This might help explain the more poleward motion of the storm than the model guidance was suggesting over the past 24 hours.

So what does this tell us? The lower heights closer to Irene might indicate it will continue on a more northerly path and miss most of Hispaniola. However, if the higher heights hand tough in the Bahamas, this might mean a slightly more westward track in this region. Obviously the atmosphere is very dynamic and we will likely see vast changes occur over the next 24 hours, but the data above suggests that a track closer to the west, perhaps slightly further west than the GFS is more likely. Looking at the overall track guidance, My forecast is that we see Irene take a path just slightly to the left of this envelop, between the EGRI and the TVCN guidance. Intensity wise things have actually become more clear. Now that it seems likely that Irene will miss Hispaniola, there is little to nothing impeding the future intensity of Irene. A significant portion of the model guidance takes Irene to major hurricane status between 60 and 72 hours, and I’d be inclined to agree.

Third Forecast Map For Tropical Storm Irene

EDIT: Irene is now a Category 2 hurricane with 100mph winds. This forced me to make a last minute edit about the first 48 hour forecast which is now significantly higher. Between 24 and 72 hours Irene will likely undergo rapid intensification under very favorable conditions. Beyond this period, sea surface temperatures drop slightly and the chances of an eyewall replacement cycle (EWRC) increase. Thus I have the winds slowly decreasing to 135mph by landfall. This is still a very formidable category 4 hurricane. The track is a blend of The ECWMF and UKMET with more emphasis on the ECWMF. Stay tuned to your local weather affiliate and this blog for updates, as this storms looks like it will be the real deal. I should have an update around this time tomorrow unless there are major changes beforehand.

Caribbean Disturbance Persists… Which Basin Will it Develop In?

Tropical Activity For July 14th, 2011

Hope everyone is having a good day! After the quick flare up that was Invest 97L, we are now down to one disturbance located within the monsoonal gyre. While the system is showing signs of organization, the question remains that if the system develops, what basin will it end up in, the Atlantic in the Southern Caribbean, or the East Pacific on the other side of Central America. The answer lies below.


Southern Caribbean Disturbance

Southern Caribbean Disturbance

The pesky disturbance that I mentioned yesterday in the Southern Caribbean has continued to fester, without really moving all that much. Visible imagery above shows that there is a decent amount of rotation, stretching from the Southern Caribbean across Central America into portions of the Eastern Pacific. All of this broad rotation is associated with the monsoonal low pressure that continues to create broad rotation around Central America. However, in order for a tropical cyclone to develop, this rotation will have to become more focused, either in the Atlantic Basin or the Eastern Pacific. Wind shear has decreased over this area in the last day to 5-10 knots. This drop in shear, along with ample warm water in the Caribbean and plenty of moisture, are favorable conditions that support development into a tropical cyclone. These conditions are also coupled by other favorable parameters such as enhanced upper level divergence provided by phase 1/2 of the MJO, and a propagating kelvin wave (highlighted by a horizontal black circle) that could enhance vorticity over the disturbance. Using all of these parameters together, it seems like there is a good chance that this disturbance will eventually develop into a tropical cyclone, and I’m placing the probabilities of development in the next 48 hours at 30%, with higher chances beyond this time range. This is higher than the current probabilities on from the National Hurricane Center (NHC). However, the broad nature of the disturbance makes it difficult to pinpoint where this system might develop.

Over time the low level ridge is expected to become stronger, forcing the monsoonal trough to move into the Eastern Pacific, taking our disturbance along with it as it organizes into a tropical cyclone.

One model seems to have an answer. The Global Forecast System (GFS) shows that over time, the low level anticyclone that dominates low level steering currents will increase in intensity, by increasing in heights over the Atlantic Basin during the next several days. This will force the lower heights, associated with the low level monsoonal circulation to push westward, taking our disturbance along with it. Thus, there will only be a small window where the disturbance will be over the Caribbean. Even despite these favorable conditions alluded to above, the limited time over the Caribbean Sea could prevent development into a tropical cyclone. However, once the circulation moves out over the waters of the East Pacific, development is much more likely. The first 36-48 hours will likely still have this system over the Atlantic side, where I’ve given the disturbance a 30% chance of development. However, based on the GFS and ECWMF (which is showing a similar if weaker solution) my expectations is that this will become a stronger and more formidable system in the Eastern Pacific basin and I’m much more confident in this system becoming a tropical cyclone in this basin. I don’t normally cover the East Pacific basin, but I’ll update my thoughts in future updates on the progress of this disturbance.


Elsewhere in the Tropics

Inferred imagery showing African waves exiting off the coastline.

Beyond our disturbance in the Caribbean, there are a couple of more minor features worth noting. First, there is a Central Atlantic tropical wave that does have a bit of low level vorticity associated with it. However, as it moves westward, it will run into upper level southerly flow that will prevent convective development over the vorticity. In addition to this tropical wave, there is also a strong wave that has recently emerged off the African coastline, as seen above. While these waves have favorable upper level conditions with low wind shear. However, this recent tropical wave is likely coupled with a Saharan air layer (SAL) outbreak that prevents convective development through dry mid level air, as evidence in a area of lower tropospheric preciptable water (TPW) near the African coast at 15 degrees north. Thus, my hopes aren’t too high that this wave will develop immediately, although down the road as it crosses across the Atlantic it might be able to regain deep convection in earnest as it approaches the lesser Antilles.

That is all I have today… until the next update!