I went to a talk by Kerry Emanuel today. Kerry is a professor at MIT, where he does all sorts of number crunching on hurricane data, and high-falutin' theorizing on the genesis, growth, and decay of tropical cyclones. I realized as I walked into the room that in my seven years at MIT as a grad student and post-doc in the same building as Kerry, I had never seen him, even though I had several friends who were students of his.
Kerry is firmly in the camp that believes the increases in storm strength are due to climate change - specifically from the warming of the sea surface. But he's interested in more than simply that - he wants to know how the energy budget of the ocean-atmosphere system works today, and how it worked in the distant past.
Some points from the presentation Kerry Emanuel made here at NSF:
- Early April is a global minimum for hurricanes
- 10% of the global total occur in the North Atlantic, but they get 90% of the press coverage
- Hurricanes do not form within a few degrees of the Equator because they need Coriolis forces - they also need warm sea water (Quizlet alert...)
- There are generally no cyclones in the South Atlantic because the water is just slightly too cold except in a narrow strip off Brazil. The first recorded hurricane there, Catarina, only just classified as a hurricane before it went onshore
- Hurricanes are basically Carnot heat engines - they are driven by the difference between sea surface temperature and the atmospheric temperature, and are therefore directly related to the greenhouse effect
- Insurance losses vary roughly as the cube of maximum wind speed (that is why this number is predicted)
- Over 50% of all damage in the US was caused by the 5 great storms prior to Katrina (I researched these numbers, they are not Kerry?s):
- Andrew, 1992 ($20.3 billion, 2006 dollars: $28.9 billion*)
- Charley, 2004 ($6.7 billion, 2006 dollars: $7.1 billion)
- Hugo, 1989 ($6.2 billion, 2006 dollars: $6.6 billion)
- Ivan, 2004 ($6 billion, 2006 dollars: $6.4 billion)
- Frances, 2004 ($4.4 billion, 2006 dollars: $4.7 billion)
- Andrew, 1992 ($20.3 billion, 2006 dollars: $28.9 billion*)
- Katrina itself is equal to all those together, with insured losses estimated at $40-60 billion, and total losses at over $200 billion
- The next five in the list are:
- Georges, 1998 ($3.27 billion, 2006 dollars: $4.0 billion)
- Jeanne, 2004 ($3.24 billion, 2006 dollars: $3.43 billion)
- Opal, 1995 ($2.5 billion, 2006 dollars: $3.3 billion)
- Iniki, 1992 ($2.09 billion, 2006 dollars: $2.98 billion)
- Floyd, 1999 ($2.1 billion, 2006 dollars: $2.52 billion)
- Georges, 1998 ($3.27 billion, 2006 dollars: $4.0 billion)
- This list does not include damages outside the US, or from the other known Category 5 hurricanes:
- Labor Day storm, 1935
- un-named storm, 1947
- Dog, 1950
- Camille, 1969
- David, 1979
- Gilbert, 1988
- Mitch, 1998
- Isabel, 2003
- Labor Day storm, 1935
- [I note as an aside that insurance losses are not a good index for increases in storm strength, even after correction for inflation. They do not account for increases in population in vulnerable areas.]
- Over 90% of the damage has been caused by category 3 storms or greater (and there have been only 30 of these since 1870, causing statistical problems for insurance)
- We can get a good count for the North Atlantic back to the 1870s because the ship traffic was so dense
- The annual global total of cyclones has been 90+/-10 since 1970 (when we first had continuous global coverage) -- for statistical purposes, this frequency is constant, and we have no evidence that the number of storms is increasing
- The argument about a trend (and from there, about natural cycles in hurricanes) is based on an extremely limited dataset that is not statistically significant
- The resulting pattern of storm numbers has no recognizable trend, but it is a very good match to sea surface temperature, which is also well known over that period
- There will be no quiet decades (hurricane-wise) in our lifetimes (but there will be quiet years from ENSO or volcanic activity)
- "Global warming" means different things over the oceans ? heating in the high and medium latitudes, but cooling in the tropics. If sea surface temperature increases, this makes for a stronger Carnot cycle.
- The argument about solar variability is still constrained mostly by measurement problems
- 50 million years ago, during the Eocene, the tropics were a few degrees warmer, and the higher latitudes were about 15C warmer. Climate models cannot replicate this temperature distribution without hurricanes to transport the required heat
The take-home is that while the frequency of storms has not increased noticeably, the number of strong storms has. This has great implications for coastal development and insurance.
*: Constant dollar values calculated with the Bureau of Labor Statistic?s handy Inflation Calculator. Base figures are from the Insurance Information Institute.
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