Weather Post by Dr. Ryan Maue
The title is a bit facetious since Cindy is a marginal tropical storm (~35 knots) and will not last more than a day as a tropical entity. So, including tropical storms Arlene and Bret, we now have a total of 3-named systems for the 2011 record books.
Back at Climate Audit in 2009, Steve McIntyre, myself, and others had a long running conversation about the potential issue of recent “overcounting” tropical storms due to improved detection techniques, e.g. satellites which weren’t around a half-century ago. We coined these “fish” tropical storms that are short-lived and relatively weak as “Baby Whirls” or “Tiny Tims“. In recent research published in a couple journals, this improved detection has been found to exist. However, it is useful to look back the debate a couple years ago when the narrative revolved around the notion that Atlantic storm frequency had increased drastically due to global warming.
Here is the literature that seemed “to pass muster”:
Landsea,C.W., G.A. Vecchi, L. Bengtsson, and T. R. Knutson, 2010: Impact of Duration Thresholds on Atlantic Tropical Cyclone Counts. Journal of Climate, Vol.23, 15 May 2010, pp.2508-2519 — Paper Link
Abstract:

Villarini, G., G.A. Vecchi, T.R. Knutson and J. A. Smith (2011): Is the Recorded Increase in Short Duration North Atlantic Tropical Storms Spurious?. J .Geophys. Res. doi:10.1029/2010JD015493. Paper Link
Abstract:

Thus, as the North Atlantic sea-surface temperatures warm and the summer rolls into fall, one has to wonder what sort of tropical storms will develop. More of these weak, short-lived variety or some long-lasting monster Cape Verdes?
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Remember everyone, DON’T PRAY FOR RAIN.
http://www.treelobsters.com/2011/02/232-pray-tell.html
“Wade says:
July 20, 2011 at 6:36 pm
It has been my opinion that NOAA rushes to name storms to make it seem like there are more tropical cyclones due to global warming”
There has been a big change in storm warnings in recent decades. It’s not a conspiracy. Better observation, tracking, and prediction allow us to issue much more informative severe weather alerts to protect people and commerce. I don’t think it’s and ebil plot to take over the world. It’s probably a good thing.
Just a totally amateurish insight, but didn’t Brett develop at or near a stationary front (not a tropical wave) and Cindy is on that same line…Seems like the low pressure system associated with the front became our tropical hurricanes. I have also noted a tendancy in the last few years of double lows developing into storms. Mostly the second(easterly storm) tends to draw down the power of the first (westerly storm), with the second storm being very short lived. Now this is just an observation and does not constitute a model…LOL
In addition to small, short lived storms, other storms probably under-counted in the past include category fives:
http://ams.confex.com/ams/91Annual/webprogram/Paper181447.html
Fish Spinner – A storm that goes out to sea, and never makes landfall.
http://flhurricane.com/wiki/General_Hurricane_Info
A good read on Hurricane Hazel (1954).
Forgot to link, sorry.
http://www.ec.gc.ca/ouragans-hurricanes/default.asp?lang=En&n=5C4829A9-1
Let’s try this one…
http://www.ec.gc.ca/ouragans-hurricanes/default.asp?lang=En&n=5C4829A9-1#Storm%20Information
Sigh…
http://www.ec.gc.ca/ouragans-hurricanes/default.asp?lang=En&n=4343267B-1
http://www.ec.gc.ca/ouragans-hurricanes/default.asp?lang=En&n=9209D4D3-1
Joe Bastardi says:
July 21, 2011 at 4:22 am
While I like “fish storm,” I’ve never like “recurve.” Most storms that recurve have the steering wheel turned right for their entire existence. So, when does the original curve end and the recurve begin? When the storm is heading due North? What happens if we simply sto pusing the term?
savethesharks says:
July 20, 2011 at 10:05 pm
I dislike “excessive” as much ore more than “recurve.” Excessive implies to me there’s something we can do to fix it, e.g. excessive play in the steering wheel.
Sounds like the heat is getting to you. 🙂
zerored78 says:
July 21, 2011 at 5:59 am
I recall some old post mortems from Bill Gray that muttered a bit about storms getting named that hadn’t been before. I tried to find a reference to that without digging too deeply, but came up with http://www.nationalcenter.org/NPA565.html which is a decent but biased look at the issue and the busted forecast of 2007.
One thing it said is The criteria for naming storms has also changed – most recently, in 2002, when subtropical storms started to be named along with tropical storms and hurricanes. I knew there was some noise about subtropical storms, but I had been under the impression they had been named before, it was just that there were several one year.
Digging a bit more (e.g. changing hurricane to subtropical)…
http://www.chron.com/disp/story.mpl/front/5337583.html says in part:
I’ve seen no suggestions that the NHC is naming storms early to strengthen a link between global warming and tropical storms, and I’m sure Chris Landsea would certainly quash any effort the NHC might muster in that regard. Landsea might change the historical counts of storms, but the project to work through old Atlantic ST records has been quite open. Note that several records are indirect, e.g. swells from a tropical storm far away, so the intensity data is not as a the storm counts are.
35kt? I’ve motorcycled in worse. By gum, I’ve bicycled in worse. Drunk.
(Don’t you give me no lip, child: drunk cycling is a tradition bordering on religion West of th’ Appalachians.)
I’ve been observing and forecasting weather professionally for about 60 years. One of my duties has been to monitor the development and movement of Tropical cyclones in the Atlantic Basin. There is no doubt in my mind that the larger number of named storms in the past decade is the result of better observational techniques which include satellite information and reconnaissance aircraft. But that’s not the whole story. Neither of these techniques was available in 1933 when 21 storms equivalent to named storms today were reported. One requirement for achieving a high number in those pre 1950 years was that the storms move through the western third of the Atlantic where there were more land areas and ships of opportunity to provide observations. In fact, there were more ships reporting major hurricanes in those days than there are today. The simple reason for that counterintuitive fact is that with so little warning of the development and movement of storms in the Tropical Atlantic, many ships wound up being caught in their circulation than is the case today. Take a look at the synoptic ship reports today while a TS or HU is in progress and you’ll see a wide void in the vicinity of, and downstream from, the active storm systems. [You can see a similar absence of aircraft in a region where a cluster of severe thunderstorms are in in progress. These are fascinating to watch in real-time at an ATC tracking center]. So, there are some years when there really are many more storms than normal. NHC’s chart of TS Climate history shows a regimal pattern of annual TC frequency in which there may be about a decade of low numbers preceded and followed by decades of high numbers.
http://www.nhc.noaa.gov/climo/images/atlhist_lowres_sm.gif
In recent years there seems to be a tendency to name almost anything that exhibits a cyclonic circulation. So far this season we have had three named storms, none of which in the past would have been characterized as being as intense and these were designated to be. Looking at the criteria used for naming these systems, one sees a notable absence of genuine ground (or sea-surface) truth.
TS Arlene was named at 7PM CDT June 28th in the Southern Bay of Campeche with estimated winds of 35kts. The storm moved westward into Mexico 2 days later with sustained winds purported to be 55kts with the forecasted possibility of it becoming an HU before moving inland. It didn’t. The highest winds I saw reported at ground stations near the path were about 40kts.
TS Bret was named at 11pm EDT on July 17th north of the NE Bahamas with highest winds of 35kts based on recon FL winds of 43-45kts and a few SFMR surface winds analyzed as being about 36-37kts. Bret drifted slowly southward some convection around the E semicircle but with evidence of northerly shear starting to develop. Winds were estimated at 45kts with a SLP of 1001mbs. By 5pm EDT on the 18th, with northeasterly wind shear pushing most of the convection into the SW quadrant leaving the surface circulation exposed to the NNE, recon and dropsondes data and “believable” SFMR winds of 50+kts and a SLP of 996mbs, prompted NHC to increase the intensity to 55kts. Forecasters opined that the storm had a chance to make HU strength if it got its act together before increasing NE shear took it apart. Unfortunately, the subsequent recon pass and the accompanying satellite pix showed less organization with the central pressure rising to 998mbs by 11PM EDT and Bret’s intensity was reduced to 50kts. Further weakening occurred during the next 24 hours as the storm completed a tight cyclonic loop and headed NNEWD. The strength was maintained at 45kts through the morning hours of the 20th and then dropped to 40kts in the evening and 35kts at 11PM. This minimal TS strength of 35kts was retained through the 21st thanks to NHC supplying life support to a system that consisted of a naked, broad low-level circulation devoid of any significant convection. They finally pulled the plug earlier this evening dropping the peak winds to 30kts. Now the reason for highlighting the quote “believable” is to provide some evidence that SFMR winds cannot be uncritically relied upon without further examination of the surface conditions at the points they were sampled. The algorithms which solve for the wind speeds are based on the thermal characteristics of wind-driven spray just above the ocean surface. Were a particular sample to be taken in, say, a heavy rain burst, the resulting estimates could be much too high. As sophisticated as this measurement system is, there is a significant amount of subjectivity and expertise involved in the resolution of this data. It makes one think of how some analysts can derive temperatures from ancient tree-rings.
TS Cindy developed along or just ahead a quasi-stationary front north of Bermuda and well east of the Mid-Atlantic Coast and was picked up by NHC Wednesday afternoon, June 20th. There was some question as to whether it was a sub-Tropical low or a Tropical low since it had characteristics of both types. I had little doubt which way they would go, and sure enough they opted for a TC. In the absence of nearby surface data, NHC relied on several of the advanced techniques for determining surface wind speeds using methodology developed at CIRA at Colorado State and TAFB at NHC which incorporated data from the AMSU satellite and possibly the SSM/I data. They found enough of an array of winds to determine that there was probably a 35kt wind somewhere near the center and at 5PM EDT the system was named TS Cindy located at 35.2°N and 53.8°W. (Technically, the Tropical Atlantic is usually designated as beginning at 35.0°N and extending southward, but compared to other determinations, that’s probably just nit-picking). The system was in an area of strong west-southwesterly wind shear of 25-35kts and increasing, and the SST in the area was about 28°C. These parameters would suggest that it might have been more properly designated as a Sub-Tropical system, especially in the absence of a well-formed eye. During Wed night and into midday Thu the 21st, NHC increased the intensity to 50kts although the satellite (Dvorak) analyses had the strength ranging from 35-40kts. Late this past evening, warming cloud tops signaled a weakening of convection mostly due to the rapidly declining SSTs along the storm track. Since it is now showing a warm core, it will probably dissipate as a “Post-Tropical” system rather than convert to an extra-Tropical one.
Now in the case of these three storms, in none of them has there been a report from a reliable land-based, shipboard or buoy platform that has reported a wind in excess of 43kts (that for Arlene on the Mexican Coast) or 33kts for either Bret or Cindy. I doubt whether Bret ever had a sustained 35kt surface wind. Cindy could certainly have exceeded 35kts due to a strong baroclinic zone in the SE quadrant on Thursday. What nags at me is that thanks to these three duds, we have already burned 3 of the names on this year’s TS list from storms that might never have been reported in the pre-satellite era. To some that might be merely an academic distinction. However, corrupts the climatological data base. There is a strong and rarely disputed motivation to produce high numbers, possibly to satisfy a coterie of “climate scientists” who have theorized that warming marine conditions due to climate change will lead to larger numbers of Tropical storms and hurricanes. This is not to say that this hyping of the numbers implies anything sinister; it may be nothing more than rooting for the home team.
Speaking of counting things . . . . How about water spouts . . . do ‘we’ (somebody) detect them, count them, and figure them in the “big picture” of ‘weather’ . . . . I know my little brain does . . . as it looks to me like all that water gets to become a cloud and then rain . . . . eventually . . .
But then again, maybe it is just another troll question . . . or maybe worth a discussion! I dun no!