Discussion: Modifying the Saffir Simpson Scale

Posted by: leftlink, 11:38 PM GMT on August 31, 2012 +0
This blog will be used to share ideas on changing the Saffir Simpson scale so that it will more accurately warn the public about storms with a large area and duration (such as Ike or Issac). The first entry will be updated frequently and will contain the latest ideas for changing the scale.

Background:

Here are the existing categories of the scale, and observations people have made about the limitations of it:



1) The current scale, based completely on highest surface wind speed, says little about surge potential or duration. A 30-minute burst of convection could generate swings in wind speeds that just be temporary, or conversely a steady intensification can occur without any wind speed increase, as we saw with Isaac. A better system would take into account a growing wind field and also any large central pressure dips that occur just prior to public updates.

2) The current scale has an added flaw: a storm at 35kts and a storm at 63kts are given the same classification, requiring added effort by the public to tell whether a system is dangerous.

3) The "step-ups" from one hurricane category to another in the current scale are uneven. This leads to a lower number of "cat 2" storms than if the steps were equal.

4) [added 9/2] A storm that intensifying rapidly in terms of central pressure, but already has dispersed its energy to cover a large area, will not have its strongest winds near the center. In the case of Isaac, the strongest winds were 100-130 miles from the center for a couple of days. In such a storm there is lots of room for intensification in the center without affecting wind speed. IF winds near the core are just 45-50 due to poor organization of the eyewall, pressure can drop 10 or even 15mb without the storm getting its designation bumped up by Saffir Simpson.

5) [added 9/4] The current wind scale does not differentiate between a storm moving at 30mph and a storm moving at 5mph, with the latter likely to cause more damage.

The IKE (Integrated Kinetic Energy) scale addresses several of these flaws, however I don't think it was designed as a complete replacement for Saffir-Simpson. By focusing on surge, the IKE number if reported alone might underestimate the wind damage from small, compact storms. The IKE calculation requires observations from all four quadrants of a storm. This may not always be available on a timely fashion. Finally, the calculations needed will be a bit beyond what general members of the public can easily peform -- which is not exactly the best way to engage the public.


[Update on 9/4]
Here are some newly revised charts to describe an alternative to Saffir Simpson that attempts to correct current deficiencies, when it comes to warning the public:

Saffir Simpson Alternative Scale

Here is an initial list of proposed "intensity upgrades":

Mandatory Adjustments

The idea for a "flight level wind" adjustment needs more review; the "size and wind field power factor" is a number that is larger for large-area storms, and it is defined as the radius of TS winds plus the radius of hurricane-force winds, multiplied by the top surface wind speed of the storm.

Size and Wind Field Power Factor

This is like the current scale except that a "strong tropical storm" category is added (suggested by Aussieweather), a category 6 is added, the categories are more uniformly spaced for wind, and most importantly, UNUSUAL SIZE OR STRENGTH can result in the storm's classification getting "bumped up" to a higher level even without a qualifying surface wind speed.
Updated: 10:42 PM GMT on September 04, 2012   Permalink | A A A

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About leftlink
Rich C., Based in Lowell, MA. A bit of a lurker here but have always been interested in winter storms and hurricanes since growing up near Cape Cod.

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