tolakram wrote:Blown Away wrote:CrazyC83 wrote:A farther west track means that Delta would avoid the cold pool south of the mouth of the Mississippi as well. The water is a bit warmer farther west.
May also encounter more shear?
I think that's the big unknown. Upper level winds from the SW favor intensification as they vent the system, but as an amateur I need someone else to interpret if this will be a benefit the the system or a hindrance, and does moving further west increase or decrease that?
For the most part the specific setup hasn't changed much because the whole pattern has shifted westward, including the upper level anticyclone. The GFS still has the storm riding the western edge of the upper ridge, but further west overall. The ULL in the Caribbean is also further west so the environment is very similar. What will be vital in knowing just how much of an affect that shear will have on the storm is how strong the core is, how long the storm moves over cooler waters, and whether or not dry air gets entrained.

The GFS seems to keep dry air out of the core of the storm, however I imagine the further west the storm gets the more likely that gets entrained, even with the setup shifted west. If the dry air is able to disrupt the core we're probably looking at a strong cat-1 landfall, if the core stays intact, the storm likely won't weaken as quickly. Dry air and shear may also play a part in tornadoes in feeder bands as well, so there could potentially be more significant impacts outside the core of the storm compared to some of the other storms not named Isaias.

It should be noted that weakening will likely happen just before landfall and even if the storm is hitting as a Cat-1 hurricane, it will likely still be packing a Cat-3like surge as it takes prolonged weakening for the surge to drastically reduce.
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