This is the paper I submitted for the Virgin Earth Challenge in early 2007. I got a letter recently saying that Virgin did not wish to invest in my project. I didn’t realise that I was proposing a commercial project; I thought the idea was to find ideas to save the world.

 This paper was written before I found out that many other scientists were suggesting similar ideas. (JG 2008)

 

On the Control of Global Temperature.

Philosophy and Implementation

(by means of jet fuel additives.)

Contents

Page 1 Philosophy.

Page 5 Implementation

Page 18 App. 1  Why We Can't Solve Global Warming by Reducing Emission Of CO2.

Page 21 App. 2 Stability –and Control Engineering.

Page 24 App. 3  References.

Page 25 App. 4  Biography and contact details of author, John Gorman.

 

 

Part 1: Philosophy.

I will suggest in this paper that the normal philosophy of trying to eliminate effects on the environment and restore a natural balance will not solve this problem on its own.  Instead, our philosophy should be to control global temperature directly by some means.

 

Sea Level.

Rise in sea level is the most obvious undesirable consequence of global warming.  For the rich countries of the world only a few metres would be catastrophic for many major cities. Similar rises would inundate the living areas of millions of poorer people in Bangladesh and various island communities.

 

The recent Intergovernmental Panel on Climate Change estimates a rise of approximately half a metre this century but there is much uncertainty in this figure.  The potential rise from the loss of Greenland and Antarctica is about 80 metres or from Greenland alone about eight metres.  All the rest of the world’s glaciers would contribute less than one metre.

 

All of these ice masses are melting, now, at today's very slightly elevated global temperatures.  Because of the delay between heat input and temperature rise, this would continue even if we could hold global temperature at today's level.  In order to stop this melting completely, it is only reasonable to assume that we will have to reduce atmospheric CO2 concentration to preindustrial levels. This would, we hope, return us to the previous stable situation.

 

Stability

Stability of sea level and global temperature has been a characteristic of the few thousand years of recorded human history. This is misleading. A longer look at history shows violent swings in climate. In the last million years there have been ten ice ages, with sea levels hundreds of metres lower than present and ten relatively short interglacial phases, with sea levels in some cases significantly higher than the present. (Five metres higher during the last interglacial period, 125,000 years ago. Ref 0)

 

Based purely on the average length of previous interglacial phases the present one should be close to its end and an ice age should be starting soon.  For all its problems, global warming has certainly eliminated that possibility.

 

We have now disturbed the temporary stability of the world’s climate. If we were, by some means to reduce atmospheric CO2 concentration to preindustrial levels, there is no guarantee that we would return to the previous stability. We might find ourselves at almost any part of the ice age / interglacial cycle.

 

If at some artificially induced cool point in global temperature we were unlucky enough to have a nuclear war or a volcanic eruption as large as Mount Tamboro in 1815 (Ref 1) the first steps towards an ice age would be very likely and we would be desperately spraying coal dust onto glaciers to absorb heat!

 

Some people believe that the present situation is just a natural variation, which does not require action.  I suggest that the natural variations that did occur just prior to recorded history would now be catastrophic for our complex society. We must now use the present situation to ensure the long-term stability of global temperature and sea level.

 

Proposal.

We should accept some elevated level of CO2 concentration in the atmosphere above preindustrial levels and the consequent global warming tendency.

To counteract this we should concentrate our efforts on screening solar radiation in some controllable way. 

The combination of these two effects would then allow us to control global temperature and sea level, even in the event of most foreseeable natural variations.

 

Note 1) This is not to suggest that we should ignore CO2 emissions or that we should not capture CO2.  This is merely to suggest that we should accept some elevated level in the long-term as part of the control system. This elevated level might be above the present level.

Note 2) This control system will work regardless of the cause of the present increase in global temperatures. If the major cause were extra solar radiation rather than extra CO2, then stability would still be achieved by this system.

Note 3) Compare the way that this system would react to a major volcanic eruption with the previous scenario’s possibly disastrous consequences.  In this case we could turn off the solar screening as soon as the eruption occurred allowing the global warming effect of the elevated CO2 concentration to oppose the cooling effect of the eruption products.  A nuclear war, and nuclear winter, may be unlikely but a volcanic eruption at least as severe as 1815 is inevitable at some stage.

Before Mount Pinatubo in 1991 an eruption was considered "very likely" for about six months.  The solar screening could probably be turned off in anticipation without disrupting the control system.

 

 

 

Conclusion On Philosophy.

 

I believe a world with an elevated atmospheric CO2 concentration is a safer world, in its ability to maintain stable temperature and sea level in the face of natural and man-made influences, than a world with no atmospheric pollution was or would-be.

 

All we need to do is find a way of screening some solar radiation and to be able to control it reasonably quickly.  This is the subject of the next section "Implementation".

 

With this control we will stop the previous ice age/interglacial cycle.  We may be able to eliminate the effects of a reasonably large volcanic eruption (e.g. Mount Tamboro 1815.  "1816 -- the year without a summer" Ref 1) and we will be able to mitigate the effects of a very large volcanic eruption (and possibly also a "nuclear winter") Additionally the control system will work regardless of the real cause of the present global warming.


Part 2. Implementation Of a Solar Radiation Screen.

 

The idea of screening solar radiation is, of course, not new.  There have been several television programmes recently on the subject following a meeting at NASA in California in November 2006.  I will divide these to three different categories:

1) In space.

2) In the troposphere. (Lower atmosphere below about 9km,30,000 ft.)

3) In the stratosphere.  (i.e. atmosphere above the troposphere.)

 

 

1)In Space.

As well as being very expensive, any form of screening in space could not be controlled or switched off.  This would make it useless as a part of the global temperature control system proposed in this paper.

 

2)Troposphere.(lower atmosphere up to 30,000ft-9km approx)

Any screen in the troposphere must essentially be cloud.  The whole of our weather and cloud is in this lower part of the atmosphere and any other chemical or particle put into this part of the atmosphere would quickly be brought to earth in rain.  There are several detailed proposals on increasing cloud cover.  These would obviously be very easy to control since any artificial input would quickly be swamped by the natural weather systems as soon as it was switched off or reduced.

 

Unfortunately there is considerable scientific disagreement as to whether cloud cover has a net global warming or global cooling effect.  This seems to apply to cloud at all levels including aircraft vapour or contrails.  The paper ‘In Search of Balance’ by Charlson, Valero & Seinfeld in Science by was summed up in the online magazine Live Science with the headline “Scientists Clueless over Sun's Effect on Earth” (Ref 2) Technically the problem seems to be that we can easily estimate the loss of incoming solar radiation due to clouds, but it is nothing like so easy to evaluate the blanketing of outgoing radiation from the earth.

 

While this scientific uncertainty exists it is hard to see any cloud system being implemented.

 

3)Stratosphere.

In the stratosphere there is one area of scientific unanimity.  In the last 250 years there have been 13 large volcanic eruptions.  All have these have resulted in global cooling in the subsequent one or two years.  The data available from these eruptions has been studied in detail by many different researchers with not a single voice opposing that basic statement. (Ref 3)

 

In particular the eruption of Mount Pinatubo in 1991 allowed the confirmation of many previously developed theories and models of climate. It was also confirmed in that case that the level of global cooling would be enough to completely counteract global warming over the same, or indeed a longer period. (Ref 4 “--1991 Pinatubo eruption produced a cooling forcing larger than the warming forcing of all the anthropogenic greenhouse gasses in the atmosphere at that time.”)

 

 

It was also universally accepted that the cooling is the result of volcanic products, which spread throughout the stratosphere in both hemispheres and persist for one to two years.  Where there was not such universal agreement, was on the particular components of the eruption, which are most effective in global cooling.  The assumption in the past was that it was solid dust particles. More recent research tends to suggest that micron sized droplets of sulphuric acid, an aerosol, is more important.  This results from chemical reactions, in the atmosphere, of the sulphur or sulphur dioxide produced in the eruption.

 

Resulting from this understanding, several proposals have been made to simulate these volcanic products in the stratosphere and at least two of these were discussed at the NASA meeting in California in November 2006.

 

Firstly there was the Nobel prizewinner, Paul Crutzen's, proposal to launch rockets, which would burn hydrogen sulphide in their stratospheric phase, releasing sulphur dioxide.  The animations of this have had wide television coverage since the meeting.  This would spread an aerosol of sulphuric acid.  Obviously the sulphur dioxide and the sulphuric acid would be chemically active and would have some effect in depleting the ozone layer.  As Paul Crutzen's Nobel prize was for his work on the ozone layer, he is in a good position to claim that the effect on the ozone layer would not be excessive.

 

Another proposal discussed at the meeting was the spreading of crushed diatomite into the stratosphere.  This seems to have received no publicity.  Diatomite is a mineral, mined in various places including Scotland, which consists of the shells of micron sized sea creatures.  The shells are made of silica, which is sand chemically, and would therefore be chemically inert in the stratosphere and on falling to earth.  Because of their small size and purity these particles would probably have good reflective properties and would, like other volcanic products, stay in the stratosphere for one to two years.  No particular method of delivery into the stratosphere was suggested except that aircraft would obviously be involved.  (In the words of Robert Chatfield, a host of the NASA meeting: ""if --it is possible to disperse the diatoms individually (how to do that is not obvious.)" This proposal stems from a wish to avoid the chemical effect of the sulphur products.

 

I suggest that both the sulphur dioxide and the silica particles could be delivered into the stratosphere by dissolving an additive in jet aviation fuel.

 

 

 

Proposal.

An Aviation Fuel Additive To Counteract Global Warming

 

This proposal is the reason for this paper and is indeed the only original part of this paper.  Some original experimental work has been done and is described in detail elsewhere. (Ref 5)

 

Different chemicals would obviously be required for the two products but the delivery system would be the same and is therefore described first as follows.

 

 

How to Deliver Products Into the Stratosphere.

 

Obviously we would not want to release these products at other phases of the aircraft flight so it is not suggested that an additive should be put generally into aviation fuel.  We would want to burn fuel containing the additive specifically when the aircraft was cruising in the stratosphere.

 

The following information comes from a 747-400 captain flying regularly from the Far East to Europe and the West Coast of United States.  Being near retirement, and having started his career with the RAF, he describes the flight plan provided to him for a long flight now as amazingly comprehensive and accurate.  Such plans rely on detailed knowledge of weather along the whole route including lower stratospheric winds.

 

In addition he tells me that it is perfectly possible for the pilot to select, for instance, the outer starboard wing tank to feed the outer starboard engine at a particular time during the flight.

 

It would seem therefore to be perfectly possible to put the additive into one tank only and to use that tank when the plane was defined in the flight plan to be in the stratosphere.  Aircraft cruising altitudes vary between about 30 and 40,000 ft (9 to 12km).  The lower boundary of the stratosphere varies from about 20,000 ft. (6 km) near the pole to close to 55,000 ft. (17km) at times on the equator.  These heights also vary considerably with weather conditions so careful planning as part of the flight plan would obviously be necessary.

 

Fuel Additive To Produce Sulphur Dioxide on Burning.

 

Sulphur dioxide is already present in the combustion products of aviation fuel.  This is because of the organic sulphur compounds naturally present in oil and great trouble is taken to reduce the proportion because of the acid effects of sulphur dioxide in the lower atmosphere.  It should be very easy to use these same sulphur compounds as the additive, which would then only be burned in the stratosphere.  Since these compounds are already present in aviation fuel it is very unlikely that they will cause any problem to the engine.

 

I have been experimenting with dimethyl sulphide, which is the nearest that I could get to Paul Crutzen’s hydrogen sulphide with an organic compound. It is a clear oily liquid which dissolves in aviation kerosene in any proportion. The solution burns in a paraffin blow lamp exactly like pure kerosene.

 

Fuel Additive to Produce Microscopic Silica Particles.

 

I propose adding tetra ethyl silicate to aviation fuel. This will, on burning, produce particles of silica similar in size to the diatoms referred to previously.

 

At first sight it might seem difficult to produce solid particles from the liquid fuel. It is however perfectly normal chemistry to have a compound which is mainly hydrocarbon like jet fuel but has one or two other atoms in the molecule which have a solid oxide on burning.

 

I have been experimenting with tetra ethyl silicate.  There is only one silicon atom of the thirty-three in the molecule.  The rest of the molecule is hydrocarbon so it is not surprising that it is a colourless liquid similar to aviation kerosene, which dissolves in kerosene in any proportion.

 

To simulate a jet engine I have used a paraffin blowlamp.  The solution burns just like paraffin.  At a concentration of 1% a mist or smoke is visible in a spotlight beam.  It is probable that the mist is microscopic crystals of silicon dioxide. This is chemically the same as the diatomite, which was proposed at the NASA meeting in November 2006.

 

 Tetra ethyl silicate is so similar to aviation kerosene that it will probably make no difference to the engine when used in low concentration. Obviously this needs to be tested properly and it is also possible that the microscopic particles will coalesce near the end of the turbine and cause erosion. (Ref 6)

 

It is also obviously necessary to confirm that the combustion product is silica, to determine the size of the particles, to compare this with the diatomite particles and many other points.

 

 

Testing

 

As suggested above there will have to be detailed testing of both additives in a jet engine.  This would be done at a static engine test facility where the exhaust could be analysed with regard to particle size and type.  Safety and the effects on the engine, the pumps, the fuel tanks etc. would all have to be checked.  Such testing is however the bread and butter of the aviation industry and could be completed very quickly.

 

Assuming satisfactory completion of such engine testing, atmospheric testing could be started almost immediately.  I would like to point out here that this is the only way that a solar screening proposal discussed at the NASA November 2006 meeting could be started quickly.

 

I would also like to point out that it is the only proposal that I have heard of, where satisfactory testing could be transferred into large scale implementation immediately at negligible cost.

 

Atmospheric Testing.

 

Though this method of distribution is new, the idea of distributing micron size silica particles has been proposed previously and was discussed at the NASA November meeting.  As I understand it silica has been proposed because it is chemically inert, unlike sulphur dioxide, and because it is available in micron sized particles in the form of the mineral diatomite. The particles are micron sized because each is the shell of a sea creature called a diatom.

 

The possible effectiveness of silica as a sunscreen has therefore been discussed together with possible problems and advantages and various atmospheric testing scenarios.  There is as yet no suggested way of distributing the diatoms individually into the upper atmosphere.  This would of course be solved by this fuel additive proposal with other possible advantages like control of particle size by varying the concentration in the fuel.

 

In brief, atmospheric testing scenarios have already been defined by experts in the field and could be implemented almost immediately following the jet engine test facility phase.  For example the suggestion of Gregory Benford of the University of California (Ref 7)

 

Such testing could be of each of the additives proposed, in different areas or at different times, at different altitudes to compare effectiveness.  For the testing phase commercial aircraft would of course not be used, instead it is probable that military aircraft could be made available.  If so, spreading could be done at higher altitudes than would be possible with most commercial aircraft.  The B-52 for instance flies up to 50,000 ft.(15km) Such an aircraft would probably also have a military arrangement of fuel tanks with some smaller emergency tanks and greater flexibility to connect tank to engine. This could be very convenient in testing.

 

What is Satisfactory Testing?

Initial testing would be mainly aimed at checking that there were no unexpected problems and that those negative effects predicted were only as expected.

 

Obviously one would also check that solar radiation screening was of the expected level corresponding to the concentration of the product in the stratosphere.

 

It should not be expected that there would be any actual global or local cooling effect from a necessarily local experiment.

 

It is unlikely that there would be any negative effects at ground level.  The stratospheric concentration necessary to provide the global cooling effect should be far less than the stratospheric concentration caused in 1992 by Mount Pinatubo.  This is because the cooling resulting from Mount Pinatubo was of the order of one degree centigrade.  This is approximately 50 times the present rate of global warming.

 

Since no ground level harmful effects of Mount Pinatubo were reported worldwide it is very unlikely that significantly lower concentrations will be detected at all at ground level.

 

 

What quantity would be needed?

The following is a very rough estimate of feasibility. Bluth et al. 1992 estimated that Mount Pinatubo put ten million tons of SO2 into the stratosphere in 1991, so maybe five million tons were still there one year later. This reduced the global temperature by about 1C, which is about fifty times the current annual rate of global warming. (0.14 to 0.2 of a degree C per decade!) So we might need 100,000 tons in the stratosphere continuously to counteract current global warming. If it stays up there for one and a half years, we will need a continuous input of 200 tons per day.

There are about 77,000 commercial aircraft flights per day! The daily use of jet aviation fuel approaches a million tons worldwide! If we assume a 5% solution of the SO2 producing chemical or tetra ethyl silicate used for one twentieth of the flight time, that would deliver 2500 tons!

 

This very rough calculation does confirm that delivery by commercial aircraft is feasible. In fact it suggest s that a fleet of dedicated high altitude aircraft such as B52’s could also do the job.

 

There are hundreds of academics in this field worldwide with a lifetime’s experience of the effects of volcanic eruptions. Some of these would obviously have to be involved in planning the testing phase and of course in implementation and would be able to make much more accurate estimates.

 

In addition, the reflective properties of SO2 based aerosols are known from volcanic studies but silica could be more or less reflective requiring therefore less or more material. Only experiment will give this information.

 

 

Possible Problems.

1) The Jet Engine.  It is very unlikely that the additives will have any effect on the engine until the silicon dioxide coalesces into particles in the exhaust.  This might however be at some point in the turbine and might cause some erosion.  Testing will show whether this is no problem, a minor problem or a major problem.

 

If there is only slightly accelerated erosion of some of the turbine blades this might be accepted by the airline industry as only a small price to pay for avoidance of the restrictions which will undoubtedly hit commercial flying unless a solution is found to global warming.

 

Hopefully the particles will not solidify until the exhaust cools after the exit from the turbine.

 

2) Ideally we would want the best screen to be laid near the equator where the greatest solar radiation concentration is.  This is however where the bottom of the stratosphere is at its highest; in some cases being as high as 17 kilometres (55,000 ft.) This could be no problem at all or it might be a small problem.

 

It is probable that careful flight planning will give perfectly adequate screening near enough to the equator.  For instance a flight plan could ask an aircraft to rise to its maximum safe altitude for a relatively short period at a point where the stratosphere was known to be slightly lower.

 

The only commercial aircraft, which flew high enough to be always in the stratosphere over the equator, was Concorde.  Looking slightly further ahead the airline industry might be delighted to have an excuse for reintroducing high-level supersonic aircraft with subsidies because they are so environmentally friendly!  The seriousness of the global warming problem justifies such major steps.

 

3) Silica, Sand and Asbestos.

Just as silica is the same as sand chemically it is also the same as asbestos chemically.  Although this sounds worrying it will probably not be a problem for various reasons.

-- micron sized particles stay in the stratosphere for one or two years so only small quantities will be falling into the troposphere.

-- particles from the stratosphere will generally be brought to earth in rain soon after they drop into the troposphere.

-- asbestos fibres are relatively long fibres rather than particles.  These are particularly difficult for the lungs to remove.

-- in a modern urban life we breathe a multitude of particles that cannot be dissolved by the body such as carbon particulates from vehicles.

-- only those who have a high exposure to particulates over a long period due to their job seem to get the serious lung diseases such as asbestosis, silicosis and pneumoconiosis.  Or they smoke!

 -- for most people and animals a certain level of dust, including nondegradable minerals, is just one of the things our lungs are designed to deal with.

 

This aspect of silica as a diatom has also been looked at by attendees at the NASA November 2007 meeting.  For instance Bob Chatfield of NASA said "Diatomaceous earth hardly seems to have clear dangers.--Concentrations in the removal region in the troposphere should be minute ---Near-surface respirable concentrations reduced by at least a factor of ~5000 --Tentative conclusion; The form of the particle does not appear particularly health-affecting compared to other particles currently in the atmosphere in ultra trace quantities.---The diatom consequences are just not that uncertain, and could well be studied" (Ref 8)

 

4) Since experts in this field are already looking at the pros and cons of the use of silica particles (diatoms) it seems unnecessary to expand on the other possible problems here.  Such climate experts would obviously have to be involved in detailed planning of a test phase.

 

Incidental Advantages.

1 ) Ultraviolet Screening.

A short deviation onto heat, light and radiation might help some readers.  Others will of course wish to skip this.

It would be easy to get the impression that heat only exists in infrared radiation not in light.  In fact heat energy is present in all light wavelengths and radiation.  It is just that cold bodies like the earth and people can radiate infrared energy while they cannot radiate light.  That is why infrared night cameras work.  During the day we see people and things only due to reflected light, which has been radiated from the sun.

 

The hot sun radiates heat throughout the whole visible spectrum (and beyond) and much of this gets to the surface of the earth and is eventually absorbed warming the earth.  CO2 in the atmosphere doesn't change this much because it doesn't absorb visible light.  Although the earth can't radiate light it is always radiating quite a lot of infrared, much of which would escape into space.  This is where CO2 does make a big difference by significantly increasing the proportion of the infrared from the earth's surface, which is absorbed in the atmosphere.  This is global warming or the greenhouse effect of the CO2.

 

To be effective, screening of solar radiation must reflect part of the incoming radiation back into space.  It so happens that the micron sized particles of silica will reflect ultraviolet light rather than parts of the visible spectrum.  This is due to the particle size.

 

Much life on this planet is already dependent on the ultraviolet screening provided by the ozone layer.  Ultraviolet is largely harmful to life and, as we know, to human skin being the main cause of skin cancers.  It is probable that a reduction in ultraviolet radiation at the surface could be seen as a significant advantage for a sun loving population.

 

Since the wavelength, which is preferentially reflected, depends on the size of the particle it may be possible to choose the particle size specifically to reduce the proportion of the most harmful ultraviolet radiation.

 

 

2) Global Temperature Distribution

 

One of the effects observed following recent volcanic eruptions was warmer winters in higher latitudes (further from the equator) in addition to the general global cooling.  This effect was observed particularly in 1992 after Pinatubo in 1991 and is now well understood in terms of climate models.

 

This could mean that the significant global cooling necessary to halt Arctic and Antarctic melting would not necessarily mean more unpleasant winter weather for those living in northern latitudes. ( The Arctic melting would still be reduced by the cooler summers.)

 

As this system of solar radiation screening is brought into operation there will be many such local effects, some predicted some not.  Climatologists will use their climate models to predict effects and weather patterns and will have to modify their computer models where effects are found which are not predicted.

 

 Climatology or climate engineering or geo-engineering will change to become a completely new science, which is not only dedicated to explaining and predicting global climate, but to controlling it to ensure long term stability of sea level and global temperature.  Then Charles Dudley Warner’s comment "everyone talks about the weather but no one does anything about it" will no longer be as amusing as it was in 1900.

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Appendix 1. Why We Can't Solve Global Warming by Reducing Emission Of CO2.

 

-- The most obvious problem so far is melting in Greenland and the Antarctic Peninsula.

-- These ice masses are melting seriously now in a way that has not occurred during this interglacial phase since the last ice age ended 10,000 years ago.  (Position statement by British Antarctic survey--Ref9. Also Ref 10 for Greenland)

-- This melting is occurring at today's very slightly elevated global temperatures.

-- Even if we could keep global temperature at today's level, the melting would obviously continue indefinitely.  This will result in a sea level rise of maybe 15 metres (seven to eight metres for the whole of the Greenland ice sheet plus the same for the Antarctic Peninsula assuming a similar geographical size and assuming that the melting did not extend to the whole of Antarctica.)

 

But the situation is worse than this because there is no possibility of keeping global temperature rise to today's level.

Because the temperature would continue to rise even if we could stop all emissions today.

-- This is because of the net heating effect of the CO2 already in the atmosphere.  This is now forty per cent above the preindustrial level and would only decline very slowly (decades or centuries) to that preindustrial level.

--If we could stop all emissions now, it is reasonable to assume that the rate of increase of global temperature would remain at about 0.2°C per decade for most of this century.  This would give a further rise of about 2° C by 2100

 

But the situation is worse than this because there is no possibility of stopping CO2 emissions now.

Which is fairly obvious.  But maybe we can keep total emissions close to present levels by international agreement. This might limit the rise to 4 - 6°C by 2100. (The IPCC figure.)

 

But the situation is far worse than this.

Because global industrial development is bound to result in increased emissions.  Probably greatly increased in the short-term.

This is simply because of the human numbers involved. The rich nations of the world constitute about one billion people of the six and a half billion now. By 2050 the UN estimates that there will be nine billion. Presumably ten billion well before 2100.

 

This rich tenth of the worlds population has a carbon footprint ten to twenty (USA) times that of the poor population.

 

Even if the rest of the rich world followed the UK’s legal commitment to cut emissions by 60% by 2050, it would only require one billion of the present agricultural population to become urbanised to cancel any gains.

 

But the situation is far, far worse than this. China expects half a billion agricultural workers to move to the towns by 2030 (not 2050!) Jeffrey Sachs in the Reith lecture on 17th April estimated world economic activity by 2050 at six times today’s level. And most of the development will be low tech. This means coal, which can be dug out of the ground and has the worst CO2 footprint of all energy sources.

 

In conclusion; emissions will continue to rise. Global temperature will continue to rise, and probably accelerate. Melting of the ice masses throughout the world will continue and probably accelerate. Sea level will rise and probably accelerate.

 

These human numbers, and a multitude of other reasons, make it vital that we reduce carbon emissions and other forms of pollution, but this will not solve the problem of global warming this century.

 

Most people who have read and watched the debate unfolding are fully aware of all of this. They understand the global situation and realise that no reduction in emissions will save the Greenland ice sheet and the coral reefs.

 

This was my situation till I started reading the academic literature on climate less than a year ago. It was with amazement that I found that the academics concentrated on reduction of emissions with religious zeal and that any talk of geoengineering solutions was not ‘politically correct’.

 

This ‘corporate thinking’ even opposed the proposal of the Nobel laureate, Paul Crutzen leading to the comment by Ralph Cicerone, The President of the American Academy of Sciences; "Various individuals have opposed the publication of Crutzen's paper for sincere reasons that are not wholly scientific,"

 

I am concerned that this attitude by the experts is stopping the development of the only tool that we have at the moment to control global temperature and sea level and restore stability.

 

It is essentially a natural tool, the simulation of a volcanic eruption, but with only 2% of the intensity of Mount Pinatubo in 1991-2. It doesn’t seem to have major disadvantages. It may have complications that we don’t predict but it is hard to envision any that are more catastrophic than not doing anything.

 

Note; This is not an argument against reducing carbon emissions by all possible means. The human numbers and a multitude of other reasons make this vital, but no reduction of emissions will lower global temperature and avoid sea level rise.


 

Appendix 2.Stability –and Control Engineering

(This section was originally in the main text as “stability” but was considered too detailed.)

 

It is important to understand the delay between cause and effect in sea level rise.

 

Man made greenhouse gas emissions raise the concentration in the atmosphere but the rate of emission today defines the rate of increase of concentration today.  The concentration today depends on the emissions of the last 30 years or more.

 

Similarly, the rate of increase of global temperature today depends upon the concentration today but the actual temperature today depends on the atmospheric concentrations over the past 20 or 30 -- or maybe 100 -- years.  This is because it takes time to warm up a large body like the earth(only its surface!), its seas or its atmosphere.

 

This delay applies even more to sea temperature where heat does not easily travel downwards.

 

There is another large delay before an increased global or sea temperature causes significant melting of a large ice mass like the Greenland or Antarctic ice sheet. But the melting will continue for ever unless the temperature is lowered to the preindustrial level.

 

One obvious conclusion from this should be that the melting of these ice sheets, and sea level rise, would continue for centauries even if we were able to stop man-made emissions immediately.

 

If we were to postulate controlling sea level by controlling greenhouse gas emissions we would probably have to extract enough from the atmosphere to lower the concentration below preindustrial levels for a time in order to stop the melting of the ice sheets.  As well as being highly undesirable for plant life, which needs CO2, this would probably make the world much more likely to enter a new ice age.

 

Control Theory.

A short deviation into control theory would probably help some readers but others can of course skip this.

The first mathematical approach was by James Clerk Maxwell in the early days of steam engines.  Real theoretical understanding of control advanced enormously with the development of weapons in the middle of the 20th century.  One of the simple points is that you must be able to change the control input much more quickly than the natural rate of change of the thing you're trying to control otherwise it will oscillate or swing wildly.

 

Take as an example the pitch control of an aircraft.  i.e. nose up or nose down.  The pilot can alter the angle of the elevators at the tail very quickly.  The aircraft itself only responds relatively slowly to this input.  The result is good control.  If the pilot had to announce "would 10 passengers please move from seats at the front to seats at the back" the plane would obviously be unstable.  This is because of the delay in applying the control input.  I would suggest that attempting to control sea level or global temperature by controlling CO2 emissions or extractions from the atmosphere would also be unstable because of the delays mentioned above.

 

Taking the aircraft analogy one step further it should also be obvious that the pilot could not talk through a voice tube to someone at the tail who would manually adjust the elevators.  The adjustment would obviously be delayed too much on the pilot's intentions and the plane would oscillate wildly up-and-down.  However this is exactly the system that was used throughout most of the history of steam powered ships.  In this case it worked perfectly well in steering ships because the response of the ship is so much slower than that of a plane.  In control theory, the control input must be compatible with the response of the whole system.

 

All of this is the bread and butter of many different branches of engineering but might be new to the climatologists who would have to implement a control system for world temperature.  In the aeroplane analogy the trainee pilot will initially tend to make large corrections in pitch but will quickly learn the skill to fly smoothly.  Early automatic pilot equipment used various analogue systems to simulate the skill.  Almost all automatic pilot systems would now use digital calculations called algorithms based on control theory that is well understood.  Similar theory would have to be developed for global temperature control.

 

Using another everyday analogy; A skilled driver taking a right turn a bit too fast will feel the tail sliding to the left. He will adjust the steering to the left slightly and the car will smoothly come out of the turn. The less skilled driver will not recognise what is happening till the car is pointing much too far to the right whereupon he will steer sharply to the left. This will straighten the car up much too sharply; the tail will swing to the inside of the turn, spinning the car into the ditch on the outside of the turn.

 

The moral is “we must react to global warming now. It will be much more difficult if we let the deviation get bigger before reacting.”


 

 

Appendix 3. -References.

If those reading this in hard copy would like to get to the page www.naturaljointmobility.info/refs.htm

on their computer they will be able to click directly to the ref number in the text.

Ref 0   Science Volume 316, Number 5821, Issue of 06 April 2007 (Ocean  Conditions Past and Present)

 

Ref 1    1816-the Year without a Summer

 

Ref 2   Livescience website article “Scientists Clueless –“

 

Ref3    Page 2 in  Robock, Alan, 2000: Volcanic eruptions and climate. Rev. Geophys., 38,

 

Ref 4   Page 1086 vol8 journal of Climate 2nd paragraph of “The volcanic Signal in surface temperature observations” Robock &Mao http://climate.envsci.rutgers.edu/pdf/RobockMaoJClim1995.pdf

See also “Individual large eruptions certainly produce global or hemispheric cooling for 2 or 3 years and this signal is now clearer”. Page 12 in Robock, Alan, 2000: Volcanic eruptions and climate. Rev. Geophys., 38, 191-219

 

 

Ref 5    www.naturaljointmobility.info/globalwarming.htm

 

Ref 6    www.naturaljointmobility.info/TESinjetengine.htm

 

Ref 7   Saving the Arctic - geoengineering | Google Groups  start of thread by Greg Benford

 

Ref 8   ditto Contribution by Bob Chatfield

 

Ref 9  British Antarctic Survey. Climate Change Position Statement

 

Ref 10  Greenland. Also  Dallas Times and many other articles.


Appendix 4. Biography and Contact Details of Author.

(Relevant bio details only as written for google geoengineering group.)

Unlike most of the members of this group, none of my careers have been even vaguely connected with geoengineering or climate.  Born in 1943 (63 now) I studied engineering at university and control engineering in a post degree year.  My first job was on the control of the electric motors in steel mills using analogue computers for control and simulation.

 

Next I worked for Digital Equipment (DEC, the PDP 8 and 11 for those old enough to remember them!) in Maynard Mass., Munich and Reading UK on the interfacing of computers to control things.  My last big project was an engine test control system with lots of different digital control algorithms.

 

My second short career was as a ski instructor and my third career since 1983 or so is on seating, office chairs, car seats, the human spine and chiropractic.

 

As a control engineer I have always found it obvious that we must control global temperature.  This morning I received a multi-page glossy from the Institution of Mechanical Engineers for a conference on "Climate Control".  Great, I thought -- I'll go to that -- till I looked at the price of £1000 for three days and realised that it was about climate control in cars!

 

We expect temperature control in our cars, houses and offices.  Why is it not obvious that we need control for global temperature?

 

I only mention the ski instructor bit because I love snow, ice, glaciers and wild snowy places.  I am absolutely convinced, from what I have read and seen for myself, that really serious melting is underway in all these places.

 John Gorman. Oaklands, New Mill Lane, Eversley, Hants. UK

Home tel. 0118 973 2365    email gormans@waitrose.com

Website;    www.naturaljointmobility.info/globalwarming.htm 

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