A quick search on the absorption of infrared by seawater, see pages 81 and 
106 and figs 21 & 22 in the book "The Ocean, their Physics, Chemistry and 
General Biology" 
 
https://publishing.cdlib.org/ucpressebooks/view?docId=kt167nb66r&chunk.id=d3_2_ch04&toc.id=ch04&toc.depth=1&brand=eschol&anchor.id=fig021#X
 
indicates that 99.5% of IR is absorbed in a layer of thickness 5.3cm. 
Hence, it is hard to see how algae of most types could darken it in the IR 
spectrum much more than a thin layer of seawater itself does.

Sev Clarke

On Sunday, September 16, 2018 at 8:50:07 PM UTC+10, Andrew Lockley wrote:
>
> Algae doesn't lighten the sea. It darkens it in the IR, which is dominant. 
> Nadine Mengis and I looked into this; we presented at CEC-14, but didn't 
> publish.
>
> Andrew Lockley 
>
> On Sun, 16 Sep 2018, 07:59 Franz Dietrich Oeste, <
> [email protected] <javascript:>> wrote:
>
>> Hi all,
>>
>> The basis of the MCB method of Salter et al. is sea water. Sea water is a 
>> salty water with a slightly alkaline pH value above 7. The ISA method 
>> generated FeCl3 aerosol (ISA) has an acidic pH around 2. 
>> This are not the only differences of the methods: The ocean surface needs 
>> an efficient cooling to prevent from hurricane developement. Salter's 
>> method delivers this cooling *only* by cloud whitening. The ISA method 
>> use cloud whitening plus several additional cooling methods like sea 
>> surface whitening/brightening by algae, methane depletion..... According to 
>> this much more efficient sea surface cooling the ISA method is the better 
>> hurricane prevention than MCB.
>>
>> Another article about the physics of hurricanes below.
>>
>> Best,
>> Franz 
>>
>> ------ Originalnachricht ------
>> Von: "Russell Seitz" <[email protected] <javascript:>>
>> An: "geoengineering" <[email protected] <javascript:>>
>> Gesendet: 16.09.2018 00:49:39
>> Betreff: [geo] Re: Hurricane moderation
>>
>> 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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