#160 Postby chaser1 » Sun Jun 14, 2015 6:13 pm
Essentially, this is better organized than an open trough yet lacking the required co-located convection which would aid in furthering surface convergence as well as a continued lowering of surface pressures by means of the creation of an upper anticyclone to evacuate the rising air and thus create & increase a cycle of organization and strengthening. The low level winds causing 91L to move off to the NW will prevent itself from "sitting around" long enough for any convection (or Mid level low) that is presently well to the east, from catching up and suddenly organize. This is what upper wind shear does. Only if and when the upper level winds become conducive enough for thunderstorms to develop and maintain themselves close to or over the LLC, will 91L have a chance to organize enough to permit it to be classified as a Depression (and then potentially a Tropical Storm). 91L is "on the clock", and has perhaps 36-48 hours for upper level conditions to Iimprove. How much it may deepen in how short a period of time? That's a separate qu3stion but a legitimate one.... unless it doesn't reach the coast prior to organizing further.
Last edited by
chaser1 on Sun Jun 14, 2015 6:18 pm, edited 1 time in total.
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Andy D
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