caribsue wrote:tolakram wrote:It's only a matter of time before a "non tropical" tropical storm does significant enough damage that someone has to go back and review the rules. While I understand the need to be scientifically pure, there are humans involved down there on those Islands, and many won't react until it gets the designation.
This disturbance is tropical in nature, so the point is rather moot. In my opinion.

Well said, from a human in one of those islands..... these systems can tear villages apart, cause flooding and landslides. I have heard people say its not a depression or a storm .... then bish bash bosh devastation.
The problem is that the LLC is defined in a surface-relative sense, and not in a storm-relative sense. This means that a fast moving but relatively poorly-defined circulation may have strong winds of even TS strength, but no closed circulation relative to the surface. However, in these sorts of cases, in a moving reference frame following the storm motion, the circulation would likely be closed and better defined. In my opinion, this should be how they determine whether the system has "closed off" a circulation enough to be considered a tropical cyclone. This would make those borderline cases of tropical disturbances with TS winds on the north side of the circulation which are screaming westward at 20+ kts into true tropical storms, and help alleviate the problem of perception you mention. Obviously there are some ambiguities involved in how one defines the storm motion vector to begin with, but, as in many other cases in meteorology and science in general, definitions and classifications will always have some level of arbitrariness attached to them.
EDIT: I should point out that I still think that the storm's intensity should be classified with respect to the ground-relative wind speed (since that is what we humans who live on the ground and aren't usually moving very fast relative to it care about

), and not the storm relative. I just think that the *presence or absence* of a circulation center should be considered relative to the storm motion.