CF  "The Hurricane-Climate Connection" 
<ftp://texmex.mit.edu/pub/emanuel/PAPERS/Haurwitz_2008.pdf> (PDF). *Bulletin 
of the American Meteorological Society 
<https://en.wikipedia.org/wiki/Bulletin_of_the_American_Meteorological_Society>*
. *89* (5): ES10–ES20

On Saturday, September 15, 2018 at 7:35:38 PM UTC-4, Russell Seitz wrote:
>
> Stephen, I'd direct your editors to Kerry Emmanuel's seminal paper on 
> hurricane track cooling, as the published basis for considering both 
> hurricane track cloud nucleation and sea surface albedo modulation to 
> moderate strorms
>
> On Saturday, September 15, 2018 at 4:19:10 AM UTC-4, Stephen Salter wrote:
>>
>> Hi All
>>
>> I was asked to write something about hurricanes for a well known popular 
>> news outlet but they thought that it was too technical. However it might 
>> still be useful.   I hope that the ETC group can comment.
>>
>> The formation of a hurricane depends on many factors including 
>> atmospheric water vapour, distance from the equator and the recent history 
>> of wind patterns.   But an essential requirement is a high sea surface 
>> temperature. To get from a tropical storm to the lowest category of 
>> hurricane requires a temperature of 26.5 C.  We can moderate hurricanes, 
>> or even prevent them, by reducing water temperature.
>>
>> A useful start to any engineering project is the estimation of all the 
>> energy flows. One cubic metre of air at a temperature of 30 C can hold 
>> about 30 grams of water vapour. The energy to evaporate this is about the 
>> same as in 13 grams of TNT, enough for a nasty anti-personnel mine.  A 
>> cubic kilometre of such air contains the same energy as the Hiroshima bomb.  
>> Hurricanes can be hundreds of kilometres in diameter and so contain tens 
>> of thousands of Hiroshimas.  If you have read this far you will know 
>> about the billions of lost dollars and thousands of deaths from this amount 
>> of energy.
>>
>> Most of the hurricanes that reach America (with the exception of Harvey), 
>> start on the African side of the Atlantic near Cape Verde and grow as they 
>> move west. We can use Google Earth to measure the hurricane breeding area. 
>>  The US National Weather Service gives a warm water depth of 45 metres. 
>> To cool this volume by 2 C in 200 days needs more than 600 times the mean 
>> US electricity power generation. If you want to moderate a hurricane 
>> tomorrow, today is much too late.  You should have started last 
>> November.  
>>
>> All this heat has come from the sun.  Some could be reflected back out 
>> to space by clouds. The reflectivity of clouds was studied by Sean Twomey.  
>> He flew over many clouds, scooped samples and measured the solar energy 
>> reflected from their tops.  He showed that reflectivity depends on the 
>> size distribution of drops.  Lots of small drops reflect more than the 
>> same amount of liquid water in fewer, larger ones.  In typical 
>> conditions, doubling the cloud drop number increases reflectivity by a bit 
>> over 0.05. 
>>
>> Making cloud drops needs a high humidity but also some kind of ‘seed’ 
>> called a condensation nucleus on which to start growth.  There are 
>> thousands of condensation nuclei per cubic centimetre of air over land but 
>> fewer in air over mid ocean, often less than 50. John Latham suggested that 
>> the salt residues left from the evaporation of a spray of sub-micron drops 
>> of sea water would be excellent condensation nuclei. They would be moved 
>> from the sea surface by turbulence to produce a fairly even distribution 
>> upwards through the marine boundary layer to where clouds form. 
>>
>> The condensation nuclei could be produced by wind-driven sailing vessels 
>> cruising along the hurricane breeding areas getting energy from their 
>> motion through the water. We can make spray by pumping water through very 
>> small nozzles etched in the silicon wafers used for making microchips. The 
>> main technical problem is that sea water is full of plankton much larger 
>> than nozzles.  This can be filtered using ultra-filtration technology 
>> with back-flushing, originally developed for removing polio viruses from 
>> drinking water. Each vessel would produce 0.8 micron diameter drops at 10
>> 17 a second.  
>>
>> Spray operations would depend on the pattern of sea surface temperatures 
>> as measured by satellites. We want the trajectory of temperature rises 
>> through the year from November to the following July to be those that an 
>> international panel of meteorologists think will give a desirable rainfall 
>> pattern from ‘gentle’ tropical storms. 
>>
>> Most ships are made in quite small numbers.  An exception was the Flower 
>> class corvettes built for the Royal Navy during World War II. If we 
>> index-link the 1940 cost to today we can predict that in mass production 
>> each spray vessel would cost $4 million. With assumptions which have not 
>> yet been rejected by hurricane experts, we think that controlling the 
>> Atlantic hurricane breeding paths would need about 100 vessels.  With 
>> typical ship lifetime the annual ownership and maintenance cost would be 
>> about $40 million. If these figures and recent estimates of the cost of 
>> hurricane damage are correct the benefit-to-cost ratio is quite attractive.  
>>  
>>
>>
>> Because of official UK Government policy updated in May 2018 the project 
>> is privately funded.
>>
>> I will send anyone who asks an update on recent hardware development, 
>> still privately funded.
>>
>> Stephen
>>
>>
>> -- 
>> Emeritus Professor of Engineering Design, School of Engineering, Mayfield 
>> Road, University of Edinburgh EH9 3DW, Scotland
>>
>

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