I: The Factors Contributing to the Earth’s Climate.
It has been noted that life stabilizes the climate but the climate is also influenced by three other sets of factors.

A: Solar Factors.
a) The Sun’s Radiation.
During the Earth’s 4 billion year long existence, the sun’s radiation has increased by approximately 30%. This increasing luminosity will continue into the future until the Earth can no longer protect itself from the intense heat. In the short term, however, the Earth is more affected by variations in the sunspot cycle. Sunspots tend to appear every 11 years and are associated with an increase in solar radiation.

b) The Solar Wind.
The sun emits a stream of ionized gas, or plasma, known as the solar wind. The solar wind fluctuates over time, “The solar wind is the blast of ionizing radiation, rich in hydrogen, that spreads in all directions from the sun, and from which Earth is largely shielded by its magnetic field ..” (Preston Cloud ‘Cosmos, Earth and Man. A Short History of the Universe’ Yale University Press New Haven 1978 p.121-122).

c) The Earth’s Orbit.
The climate is also affected by variations in the Earth’s orbit around the sun, “The Earth's orbit is an ellipse. But the ellipse is not stable. Sometimes it is almost circular, sometimes it is more elliptical. Thus over periods of hundreds of thousands of years the Earth gets more light and heat from the sun, sometimes less.” (Tim Radford 'The Crisis of Life on Earth. Our Legacy from the Second Millenium. Thorsons Publishing Group 1990. p.138); “The Earth orbits the sun, but its speed is not constant. What is more the orbit itself changes over a 95,000 year cycle.” (Michael Allaby 'Living in the Greenhouse. A Global Warning.' Thorsons Publishing Group 1990 p.45); “Over a period of about 96,000 years the shape of the orbit varies from almost circular to strongly elliptical.” (Andrew Goudie ‘The Nature of the Environment’ Basil Blackwell, London 1989 Second edition p.56).

d) The Earth’s Tilt.
The Earth tilts on its axis as it orbits the sun. The Earth’s tilt makes a bigger impact on the climate than the Planet’s proximity to the sun e.g. the winter in northerly latitudes occurs when the Earth is at its closest to the sun, whilst the summer occurs when the Earth is furthest away from the sun, “The Earth is at its closest to the Sun in January - the orbit of the Sun thrusts the planet some 3 million miles further away from the Sun in July.” (Anthony Milne 'The Earth's Changing Climate. The Cosmic Connection' Prism Press 1989 p.74); “The Earth’s tilt gives us our seasons. The bigger the tilt the stronger the contrast between summer and winter.” ('Living in the Greenhouse' p.46); “Every 20,000 years or so the Earth alters between being 21.8 from the perpendicular (or more upright) to 23.4 (more tilted). The orbital variations of the Milankovitch kind will bring about far more severe changes to the climate than solar variations.” ('The Earth's Changing Climate' p.75).

e) The Earth’s Wobbles.
The Earth does not rotate smoothly on its axis as it orbits the sun. Like a spinning top, the Earth wobbles on its axis causing a tiny slowing down in the Earth’s spin. These tiny delays give rise to what is called the precession of the equinoxes. The wobble causes the Earth’s axis to trace out a circle on the sky every 25,800 years.

f) The Earth’s Rotation.
The Earth’s rotation on its axis produces the Coriolis effect, “The air (warmed by the sun) would move precisely north and south were it not for the Earth’s rotation.” (Michael Allaby ‘Living in the Greenhouse’ Thorsons Publishing Group 1990 p.52).

B: The Shifting of the Earth’s Continents.
The second major set of factors which influence the climate is the shifting of the Earth’s continents.

The movement of the Earth’s tectonic plates has a profound influence on the climate. It is believed that when the Earth was formed most of the Planet was covered by water and that land masses began to form only slowly during Earth’s history. It is not known where the continents first began to form, “It is not yet possible to draw map of the continents prior to about 350 million years ago because the distance between the fragments that collided to form Pangaea prior to their collision cannot be estimated.” (The Times Concise Atlas of the World p.9).

The first known location of the Earth’s continents indicate that they were far away from those they have today, “A bit less than 500 million years ago glaciers were active in what is now the Sahara Desert, while it lay at the South Pole. Africa and North America were then about 10,000 kilometres apart.” (Preston Cloud ‘Cosmos, Earth and Man. A Short History of the Universe’ Yale University Press New Haven 1978 p.107).

About 300 million years ago there were only two continents: laurasia which consisted of eurasia, greenland and north america, and gondwanaland which consisted of all other continents. These two giant continents sidled towards each other to create a gigantic supercontinent called pangaea surrounded by one super ocean panthalassa, “Pangaea was itself formed some 250-300 million years ago by a collision of Gondwanaland with Laurasia west of the Urals and of Asia east of the Urals.” (The Times Concise Atlas of the World p.9). Quite why the two large continents merged together and how long the process went on for is not known. Similarly it is not known why pangaea began to break up. Laurasia still existed even a mere 80 million years ago. Eventually laurasia began to disintegrate and the continents drifted towards their current locations. Some of these continents drifted thousands of mile apart whilst others collided with each other producing some fantastic results, “Of all the dramatic motions (of plate tectonic) .. the most remarkable is that of India. Wedged free from its position between southeastern Africa and northern Antarctica about 150 million years ago, it has since then travelled some 8,000 kilometres northward to collide with southern Asia and elevate the world’s highest mountains.” (Preston Cloud ‘Cosmos, Earth and Man. A Short History of the Universe’ Yale University Press New Haven 1978 p.108).

The changing position of the continents around the Earth not only had a considerable impact on the continents’ climates but on that of the Earth as well, “The positioning of continents helped determine climatic conditions.” (Jon Erickson ‘Greenhouse earth. Tomorrow’s Disaster Today’ Tab Books, Blue Ridge Summit PA 1990 p.17); “The movement of continents itself affects the global climate because of the change in the distribution of the Earth’s albedo and because of the difference in the way land and sea warm and cool.” (Michael Allaby ‘Living in the Greenhouse’ Thorsons Publishing Group 1990 p.72).

C: Global Warming.
The third major set of influences on the Earth’s climate is global warming.

Although the sun bathes the Earth in heat it is global warming which keeps the Earth warm not direct sunlight. Global warming retains some of the sun’s heat preventing it from making an immediate escape back into space. Global warming[1] is composed of three different factors.

a) The Greenhouse Effect.
The greenhouse effect consists of a number of gases in the Earth’s atmosphere which act as a blanket keeping the Earth warm. The greenhouse gases allow the sun’s short-wave, ultra-violet radiation to pass through the atmosphere but blocks the long-wave, infra-red radiation reflected from the Earth’s surface from escaping into space. This causes a build up of heat around the Earth. The most important of the greenhouse ‘gases’ is water vapour. Other greenhouse gases include Carbon dioxide, methane, nitrous oxide and about 40 other minor contributors. The biggest anthropogenic contributor to the greenhouse effect is Carbon whether in the form of Carbon dioxide, methane, Carbon monoxide, or chlorofluorocarbons.

b) The Photosynthetic Effect.
The concentration of Carbon greenhouse gases is determined not merely by global Carbon emissions (what is called here the supply side of the Carbon spiral) but by the Earth’s terrestrial and aquatic Plants which extract Carbon from the atmosphere (the demand side of the Carbon spiral). It is not possible to reduce the concentration of atmospheric Carbon by relying solely on limiting Carbon emissions. Even if Carbon emissions were curbed dramatically, the greenhouse effect could get worse if there was a continuous reduction in the demand side of the Carbon spiral.

c) The Heat Effect.
The heat effect consists of a number of factors.

1. The Earth’s Internal Heat Sources.
The Earth has two main sources of internal heat - geothermal, and nuclear, energy.

2. Metabolic Thermal Pollution.
Virtually all life on Earth whether Micro-organisms, Plants or Animals (including humans) generate body heat through their bio-chemical metabolism. In the 1970s one superstore calculated that it did not need to provide any additional heating because its store was kept warm by shoppers or as they were termed by the store - ‘mobile heating units’. It has also been calculated that if all humans lived on Antarctica, their body heat alone would be enough to melt the continent’s ice sheets.

3. Anthropogenic Thermal Pollution.
Humans also generate thermal pollution through their domestic and industrial activities.

4. The Albedo Effect.
The albedo effect is the amount of sunlight reflected by the Earth’s surface. Surfaces with a high albedo reflect most sunlight back into space e.g. snow, whilst surfaces with a low albedo absorb a high proportion of sunlight e.g. Forests. The Earth’s surfaces whether the land, (including ice sheets, Forests, and human artifacts, etc.), oceans, clouds, and atmospheric dust (thrown up by seismic/volcanic activity and by cars) have a different albedo effect.

5. Evapotranspiration.
Evapotranspiration is the process by which Plants release latent heat in the form of water vapour into the atmosphere.

6. The Relative Contributions made each Factor to the Heat Effect.
The contribution made by geothermal energy seeping into the atmosphere is minimal. The contribution made by metabolic thermal pollution is also probably minimal. Anthropogenic thermal pollution may be increasing but is also minimal, “Direct input from geothermal sources such as volcanoes and from our own generation of heat are both negligible.” (Dick File ‘Weather Watch’ Fourth Estate, London 1990 p.35). The quantity of heat absorbed by the world’s oceans, however, is colossal, “The oceans heat the atmosphere more than the sun’s rays do and the top 3 metres of the oceans contain as much heat as the 100 kilometres or so over which the atmosphere extends.” (Daniel Clary, New Scientist 27.4.91. p.41-43). Evapotranspiration is also responsible for huge quantities of heat being released into the atmosphere. It is not known, however, what the precise contribution is of each of these factors and it is not possible, therefore, to give an exact ordering as to their relative contributions.

D: The Contribution of the Various Factors Influencing the Earth’s Climate.
Three main sets of factors have been described above which have an influence on the Earth’s climate. The precise contribution made by each of these factors to the Planet’s average temperature is not known. There are a number of calculations which help to expose the hidden factors influencing the Earth’s climate.

a) Planetary Positioning.
The global average temperature on Venus is 477C whilst that on Mars is -53C. The Earth is twice as close to Venus as it is to Mars and yet the Earth’s temperature is seven times closer to Mars, “Lovelock calculates that, based on the facts of planetary positioning, Earth’s average surface temperature should range between 240C and 340C.” (Lawrence E Joseph ‘Gaia. The Growth of an Idea’ Arkana, England 1990 p.147). There is some factor then which is causing the Earth to be much cooler than it should be according to its location in the solar system.

b) The Sun’s Increasing Luminosity.
It has been noted above that the sun’s luminosity has increased throughout the Earth’s history and yet, quite startlingly, there has been no corresponding increase in the Earth’s average temperature.. “the sun has warmed some 30% over the last 4.5 aeons of the planet’s existence .. The Earth’s mean surface temperature has (not) risen anywhere near the 50-60C that the sun’s warming would imply.” (Lawrence E Joseph ‘Gaia. The Growth of an Idea’ Arkana, England 1990 p.122). Once again, there seem to be factors which are causing the Earth to be much cooler than it should be. Current discussions about the state of the Earth’s climate concentrate on why the Earth is heating up and yet, just as importantly, there are powerful factors which are keeping the Earth much cooler than predicted.

c) The Astronomical Theory.
The contribution which astronomic factors make to the Earth’s climate tend to be cyclical, “The astronomical theory of climate change .. involves shifts in the angle of the ecliptic (the tilt of the earth’s axis of rotation from the plane in which the earth orbits the sun), changes in the eccentricities of the earth’s orbit and the precession of the equinoxes. Each of these factors varies in a cyclical manner. The first exhibits a periodicity of 40,000 years, the second of c.96,000 years and the third a periodicity of c.21,000 years.” (A M Mannion ‘Global Environmental Change. A Natural and Cultural Environmental History’ Longman New York 1991 p.24). It is not known how powerful astronomic factors are. The intergovernmental panel on climate change believes that current increases in Carbon emissions are more powerful than astronomic forcing which is pushing the climate in the direction of another ice age.

d) The Greenhouse Effect.
It has been argued that the heat generated by greenhouse effect is greater than that coming directly from sunlight, “The surface of the earth receives about 18% of its heat directly from the sun and a little less from solar radiation scattered on the way through the atmosphere by clouds: some 65% of the radiation reaching the ground is in the form of infra-red energy radiated back down to the surface by the atmosphere - the natural greenhouse effect.” (John Gribbin ‘Hothouse Earth’ Bantam Press 1990 p.129). This quote does not indicate, however, what the greenhouse effect’s contribution is to the Earth’s global average temperatures in comparison to other factors.

Over the last decade or so a number of scientists have attempted to discover how the amount of the greenhouse gas CO2 has varied over time. The evidence derived from ice core samples in the Antarctic seems to suggest that variations in the level of atmospheric Carbon roughly match the variations in global temperature. Although the greenhouse effect is composed of a number of different greenhouse gases, many scientists seem to have focussed upon CO2 as the key gas which acts almost like the Earth’s thermostatic device - a rise in atmospheric CO2 boosts global temperatures whilst a decline causes a reduction in global temperatures .. “carbon dioxide in the atmosphere functions as a sort of thermostat for the Earth.” (Jon Erickson ‘Greenhouse Earth. Tomorrow’s Disaster Today’ Tab Books, Blue Ridge Summit PA 1990 p.16).

The Antarctic findings have been criticised, however, by scientists who argue the match is not always good and that in some cases the fall in Carbon happened after the fall in temperatures, “The fall in carbon dioxide did not occur until about 10,000 years after the temperatures began to plummet, at the start of the last ice age, so it was following rather than leading the trend.” (Nigel Calder ‘Spaceship Earth’ Viking, London 1991 p.192).

There is no conclusive evidence as yet about the link between the level of atmospheric CO2 and global temperatures. If an increase in atmospheric Carbon tends towards a rise in global temperatures but other, more powerful factors, cause an actual decrease in global temperatures then the greenhouse effect is still valid but clearly it is not powerful enough to warrant being called the Earth’s thermostat. It may be that the greenhouse effect produces a rise in temperature which causes an ice age.[2] If, however, an increase in atmospheric Carbon is not a cause of, but the effect of, a rise in global temperatures then this would undermine the greenhouse theory. The concentration of atmospheric CO2 might still play a role in influencing global temperatures (for example by helping to maintain the rise in temperature), but the theory of the greenhouse effect would be wrong because CO2 would no longer be a cause of temperature change. Proving whether a change in the concentration of atmospheric Carbon is a cause or an effect of temperature change will be extremely difficult.

It is possible that, on occasions, the greenhouse effect may be a bigger contributor to changes in global temperature than astronomical factors whilst on others it may not. In some cases it might reinforce astronomic changes. In other words, whilst astronomical changes push the Earth towards an ice age the greenhouse effect may either overwhelm and reverse this trend, make little difference to it, or it may reinforce the tendency to an ice age. If astronomic changes produce changes in the concentration of atmospheric Carbon which reinforce the direction in which astronomic changes are taking place then although increases (or decreases) in Carbon emissions may boost (or decrease) global temperatures it could be argued that the greenhouse effect is just a function of astronomic changes. The theory that the concentration of atmospheric Carbon determines global temperatures does not explain what brought about the change in the concentration of atmospheric Carbon. Once again, proving the relationship between the greenhouse effect and astronomic changes will be extremely difficult.

e) The Heat Effect.
The greenhouse effect is a blanket of gases which prevents heat from escaping from the Earth’s atmosphere. This theory says nothing about the Earth’s albedo effect, the amount of sunlight reflected back into the atmosphere (in the form of infra-red radiation) by the Earth’s surfaces. The effectiveness of the greenhouse effect would be quite different with different albedo effects. If the Earth’s surface was a perfect mirror which reflected heat straight back into the atmosphere, the greenhouse effect would be much greater than it would be if the Earth’s surface was covered in tar which reflected a much smaller proportion of heat back into the atmosphere.

If there was no such thing as a greenhouse effect on Earth then global temperatures might be colder but not that much colder because the oceans and Forests absorb vast quantities of heat which would continue to keep the Earth warm - even though this heat, once released, would escape back into space more rapidly than it would where a greenhouse effect exists.

1. The Oceans.
There are some commentators who believe that the Earth’s average temperature is determined more by the heat absorbed by the Earth’s oceans than by the greenhouse effect, “Richard Lindzen .. claims that global temperatures are much more dependent on the magnitude of heat transfer between the tropics and the poles than on the amount of greenhouse gases in the atmosphere.” (New Scientist 27.11.93 p.7). The oceans store vast quantities of heat which are transported around the Earth but whether this means that the oceans make a bigger impact on global temperatures than the greenhouse effect is not known, “The oceans act as vast solar energy reservoirs; every 90 minutes the Gulf Stream releases to the air as much energy as humans worldwide produce in a year from burning coal.” As a result, the Gulf Stream, “dominates the climate of western Europe. It keeps Siberian weather away from most of western Europe and ensures for instance, that London remains many degrees warmer in winter than in New York, even though London is 1,000 kilometres further north.” (Fred Pearce p.148).

It was pointed out above that the quantity of heat absorbed by the top 3 metres of the world’s oceans is greater than that in the atmosphere. This seems to support the argument that the Earth’s global temperature is determined more by the oceans than by the greenhouse effect. Whether it does, however, is not clear for even if the top 3 metres of the oceans contain more heat than the atmosphere this may be due to the infra-red radiation reflected back to Earth by the greenhouse effect rather than because of the direct sunlight absorbed by the oceans so it does not prove that the oceans are a more powerful determinant of global temperatures than the greenhouse effect.

f) Global Warming.
It has been calculated that global warming keeps the Earth 33C warmer than it would otherwise be. Without global warming the Earth’s average temperature would be -19C. This is the difference between a Planet which would be totally inhospitable for life and one which is teeming with a vast variety of Plant and Animal life. Unfortunately, it is not known how these figures for the Earth’s temperatures with and without global warming have been calculated. It is not known whether these figures have been based on calculations for the greenhouse effect alone or global warming as a whole. In either case they do not seem to be compatible either with the Earth’s temperature as determined by the Earth’s position in the solar system nor the expected increase in heat caused by the sun’s increasing luminosity. It could be that whilst the greenhouse effect/global warming are keeping the Earth warmer than it should be, clouds, which reflect a large proportion of sunlight back into space, are responsible for keeping the Earth far cooler than it should be.

The theory of global warming outlined above would not be seriously damaged by the untenability of the greenhouse effect since it supposes that there are a number of other factors besides CO2 emissions which influence global temperatures and that these causes occur independently of changes in the concnentration of atmospheric Carbon.

g) Conclusions.
It is far from clear which are the main contributors to the Earth’s global temperatures. The greenhouse effect may or may not be a more powerful factor than astronomic climate forcing. The world’s oceans may or may not be more powerful than the greenhouse effect. The albedo effect of clouds in reflecting heat back down to Earth may be greater than the greenhouse effect. The global cooling caused by the albedo effect of clouds in reflecting sunlight back into space, preventing the Earth from warming up as it should do according to its position in the solar system and the sun’s increasing luminosity, may be a much more powerful influence on the climate than the increase in global temperatures brought about by global warming.

E: Life Regulates the Climate.
It has been pointed out above that it is life which controls the climate. Although it may be difficult to provide a definition for the term life it is used here to cover the activities of Micro-organisms, Phytomass, and Animals.

a) The Role Played by Life in Rock Weathering.
The two main global Carbon spirals are the Photosynthetic/exhalation spiral and the volcanoes/rock weathering spiral. Both of these phenomena have an important role in influencing the climate. Whilst the former is clearly involves life, the latter seems to be an entirely inorganic process divorced from any connection with life. Rock weathering, however, does have a close connection to life, “When plants die, their roots decay into the soil, and the organic carbon reacts with the rocks in a process known as weathering. (Weathering also occurs while the plants are alive, since some of the carbon dioxide they absorb is not used but is conducted and deposited deep into the soil, initiating the same chain of chemical reactions). In a process catalyzed and hastened by bacteria, the carbon and the oxygen of the plant materials react with the calcium silicate, the substance of rock particles, releasing oxygen into the atmosphere and forming calcium carbonate (limestone) and gelatinous silicic acid. Unlike their rock-solid silicate predecessors, limestone and silicic acid dissolve readliy into the groundwater and are transported to local streams and rivers, which empty into the sea. Marine organisms filter the limestone from the water to form their shells, essentially reconstituting the land stones for use as their shelter.” (Lawrence E Joseph ‘Gaia. The Growth of an Idea’ Arkana, England 1990 p.127). Trees are also involved in rock weathering as will be noted later. Lovelock has argued, “All life forms, from micro-organisms to trees, from amoebae to elephants, in various ways increase the rate of rock weathering, which is the sink for the greenhouse gas, CO2.” (James Lovelock ‘Gaia. The Practical Science of Planetary Medicine’ Gaia Books Ltd, London 1991 p.137).

b) The Role Played by Life in the Creation Clouds.
Whilst some commentators believe that the oceans are primarily responsible for controlling the Planet’s climate since they absorb such vast quantities of heat, other commentators hold that clouds are the most important influence on the climate. The important role played by clouds in influencing the Earth’s climate does not necessarily contradict either the theory that life controls the climate or the theory that the oceans control the climate. As regards the former, life itself helps to create clouds through evapotranspiration whereas as regards the latter, clouds are created by evaporation from the oceans.

c) The Role Played by Forests in Influencing the Climate.
The influence of Trees/Forests on the climate is so complex that it would be useful to clarify their impact by looking at the relationship between Forests and, firstly, the Carbon spiral; secondly, the water cycle; and, thirdly, the heat effect.

1. Forests and the Carbon Cycle.
Trees/Forests have a number of relationships with the Earth’s global Carbon spiral all of which have a direct or indirect impact on the climate.

One: Forests and Photosynthesis.
Forests have an important influence on the concentration of atmospheric Carbon, and thus the greenhouse effect, because they extract Carbon from the atmosphere through Photosynthesis. It has been estimated that 51% of Photosynthesis on Earth takes place on land - primarily through Forests. “Forests conduct more photosynthesis worldwide than any other form of vegetation.” (Jon Erickson ‘Greenhouse earth. Tomorrow’s Disaster Today’ Tab Books, Blue Ridge Summit PA 1990 p.137).

Two: Forests and Carbon Emissions.
Forests boost the greenhouse effect through pumping huge quantities of Carbon into the atmosphere. This happens in a number of ways.

* Burning.
If Forests catch fire, or are razed by humans, they release Carbon into the atmosphere. Until recently the razing of Forests was the most important source of atmospheric Carbon, “Until the mid 20thC, temperate deforestation and the loss of organic matter from soils was a more important contributor to atmospheric CO2 than was the burning of fossil fuels.” (JT Houghton: GJ Jenkins and JJ Ephraums 'Climate Change. The IPCC Scientific Assessment' Cambridge University Press, Cambridge 1990 p.xxxii).

** Decay.
When Trees die they decay and slowly release the Carbon they have accumulated throughout their lives.

*** Respiration.
When Trees suffer heat stress they tend to respire giving off Carbon dioxide.

Three: Forests and Soil Protection.
One of Forests’ roles is protecting the soil from wind, and water, erosion. In addition, by providing shade, Trees also protect the soil from dessication caused by prolonged sunlight. Trees play a vital role in enabling soils to store Carbon. Once Trees have been removed, the soil cannot retain as much Carbon which gradually seeps back into the atmosphere.

Four: Forests and Rock Weathering.
Forests also play a role in rock weathering, “one type of vascular plant ecosystem, angiosperm-deciduous plants .. weathers the minerals in the rocks and the soil at a rate three to four times faster than the ecosystems comprised primarily of conifers ...” (Lawrence E Joseph ‘Gaia. The Growth of an Idea’ Arkana, England 1990 p.132). For Lovelock, rock weathering is a more important means of extracting Carbon from the atmosphere than Photosynthesis.

2. Forests and the Water Cycle.
One: General.
Forests have as complex a relationship with the water cycle as they do the Carbon spiral and, once again, some of these relationships have impacts on the Earth’s climate, “They act as brakes on the wind, and by fanning the air they promote the transfer of heat and moisture from the land surface to the air. Plants intervene in the transfer of water from rain to soil, and their shade reduces evaporation from the soil. On the other hand, plants consume water and expel water vapour through their leaves. This floral sigh, called transpiration, adds moisture and latent energy to the air, for making clouds and driving ‘wanton winds’.” (Nigel Calder ‘Spaceship Earth’ Viking, London 1991 p.102).

* Water Storage.
Forests are usually regarded as Carbon stores but in fact, just like all other living things, they contain more water than they do Carbon. So great is this storage of water that, “More water is stored in the forests of the earth - especially the tropical rainforests - than in its lakes.” (Al Gore ‘Earth in the Balance. Forging a New Common Purpose’ Earthscan Publications Ltd, London 1992 p.106). Forests have been called ‘green lakes’.

** Water Protection.
By providing shade, Trees reduce evaporation. Trees not merely conserve Carbon in soil but water.

*** Photosynthesis.
Photosynthesis by Trees involves the breakdown of water molecules.

**** Forests Seeding Clouds.
Forests are responsible for releasing particles which help to seed clouds.

Two: Water Vapour and the Greenhouse Effect.
Trees influence the water cycle and the greenhouse effect through evapotranspiration. “One factor which affects the rate at which moisture enters the air from land and which is of global importance is the presence of plants, particularly trees. Plants lose water from their leaves by a process known as transpiration. The total loss of water vapour from plants and soil is called evapotranspiration.” (Jonathon Silvertown & Philip Sarre (editors) ‘Environment and Society’ Houghton and Stoughton, London 1990 p.77).

Water vapour is a greenhouse gas. The scale of the water vapour released by Forests through evapotranspiration is colossal, “Although only a small fraction of a leaf surface bears the pores through which moisture evaporates, the potential rate of water loss from a many leaved canopy of leaves can approach that of loss from the same area of an open water surface.” (Jonathon Silvertown & Philip Sarre (editors) ‘Environment and Society’ Houghton and Stoughton, London 1990 p.77); “This transpiration (of trees) is a very effective mechanism, and a square kilometre of moist, ‘steamy’ tropical rainforest can push more water vapour into the atmosphere than a square kilometre of ocean.” (Dick File ‘Weather Watch’ Fourth Estate, London 1990 p.253). A square kilometre of trees has a much larger total surface area because of its leaves, than a square kilometre of ocean.

Three: Evapotranspiration and the Albedo Effect.
The water vapour released through evapotranspiration often contributes to the formation of clouds whose albedo effect reflects sunlight back into space thereby affecting global temperatures. Whilst water vapour is a greenhouse gas which boosts global temperatures, clouds’ albedo effect cools the Earth, “The evaporation of water from forests is part of Gaia's cooling system.” (James Lovelock 'Gaia. The Practical Science of Planetary Medicine' Gaia Books Ltd London 1991. p.179).

The scale of evapotranspiration’s influence on the formation of clouds, and thus its cooling role in the Planet’s climate, can be appreciated indirectly from the fact that, “Rainfall on the continental land masses of the Earth is, to a considerable extent, a consequence of evapotranspiration; the pumping by trees and large plants of water from the soil to their leaves where it evaporates.” (James Lovelock ‘The Ages of Gaia. A Biography of Our Living Earth’ Oxford University Press 1988 p.90); “Each year approximately 70% of the precipitation which occurs in the (Amazon) tropical forests returns to the atmosphere due to the forests own contribution to the process of evaporation.” (Worldwide Fund for Nature Special Report no.6 May 1991 p.13).

3. Forests and the Heat Effect.
Forests also have a major impacts on the Earth’s climate through the heat effect.

One: The Albedo Effect of Forests.
It was pointed out above that water vapour from Trees produces clouds which have an albedo effect. But Trees also have an albedo effect in their own right, “By colouring the land, plants increase the local intake of solar energy.” (Nigel Calder ‘Spaceship Earth’ Viking, London 1991 p.102).

Two: The Heat Effect Produced by Evapotranspiration.
The water vapour released into the atmosphere through evapotranspiration contains latent heat. This heat is released when water vapour condenses into rain, “In addition to controlling the flow of water, the processes of evaporation and condensation represent a system of temperature regulation. The water that evaporates in the Amazon region absorbs heat that is returned to the atmosphere during the condensation process. On the one hand, this permits the tropical areas of the Amazon region to cool down, and, on the other, it permits heat to reach the upper strata of the atmosphere. As the atmosphere circulates it carries these upper layers as far as the polar regions.” (Worldwide Fund for Nature Special Report no.6 May 1991 p.13).

4. Summary.
It is not possible to say with any scientific certainty which of the above factors connected with Forests has the biggest impact on the climate and it is not possible to indicate their order of importance. Some of these factors vary according to the type of Tree/Forests and its geographical location e.g. some types of Trees in some areas have a much greater rate of Carbon absorption and evapotranspiration than other types of Trees in other areas. This makes it more difficult to make generalizations. Nevertheless, it can be speculated, that the biggest contribution which Forests make to global warming is not through the greenhouse effect (the release of Carbon into the atmosphere) nor through Photosynthesis but the heat effect produced by evapotranspiration (which increases global warming) and by the albedo effect caused both by Forests themselves and by the clouds generated through evapotranspiration. Forests have contrary influences on the climate - in some cases boosting global warming whilst in others boosting global cooling.

It is possible to argue, without being able to confirm such speculation, that Forests are one of the most important ecological phenomena influencing the Planet’s temperature and thus its climate. The albdeo effect of Forests may be secondary to that of the oceans’ but it is greater than that produced by ice sheets, glaciers, and fresh water systems. Although Forests cover a far less extensive area of the Planet than the oceans, they generate more Photosynthetic activity. It might be suspected that the oceans produce vastly more water vapour than Forests but the huge surface area of all the leaves in Forests means that the difference between them is not as great as might be suspected. It can’t be negligible given that, as Lovelock points out, much of the rainfall falling over the land stems from Forests. It could well be then once all of the factors which influence the climate are taken into account that, at the very least, “Forests rival oceans in their influence on the biosphere.” (Kilaparti Ramakrishna & George M Woodwell (eds) ‘World Forests for the Future: Their Use and Conservation’ Yale University Press New Haven 1993 p.xi).

d) A Sumary of the Role Played by Life in Regulating the Climate.
Lovelock’s theory that life regulates the climate is a profound thesis which has already been the subject of intense debate and will doubtlessly continue to be so for many decades. Ever since the hypothesis was put forward in 1979 it has been capable of explaining more and more Planetary phenomena and has given rise to fruitful predictions which have been able to test the hypothesis.

G: An Overview of Climate Theories.
There are then a number of different hypotheses which attempt to explain the Earth’s climate. There is the astronomic theory; the greenhouse effect in which changes in the concentration of atmospheric carbon produce changes in the Earth’s global temperature; the oceanic theory in which the Earth’s climate is determined by the amount of heat absorbed by the Earth’s oceans; the cloud theory in which the climate is determined by the Earth’s cloud cover; and, finally, the Gaian theory. Of all the theories outlined above the gaian theory is by far the most sophisticated.

II: Whither the Climate?
A: The Earth’s Climate over the Aeons.
The Earth’s global temperature has been fairly consistent over the last 4 billion years, “The earth's climate has changed very little over 3,500 million years.” (JE Lovelock 'Gaia. A New look at Life on Earth' Oxford University Press 1979 p.9). The Earth’s global average temperature does vary over time but nothing like to the same extent as that found on neighbouring planets.[1] This is remarkable given the large number of factors which influence global temperatures and the dramatic extent to which some of these factors have changed over time. During the Earth’s lifetime, there has been a 30% increase in the Sun’s solar radiation; the Earth’s terrain has changed from a lifeless, barren state to one covered in a thick blanket of Plants and Forests; the Earth’s continental landmasses have drifted around Earth having once been separated, then huddled together as a supercontinent, and now located thousands of miles apart; and, finally, there has been an almost total extraction of Carbon from the atmosphere. It seems unquestionable that there is some relationship between these changes in the Earth’s geophysiology and the stability of the Earth’s average temperature. The consistency of global average temperatures is even more remarkable given that even the smallest change in global temperature can produce dramatic changes in the Earth’s climate. A reduction in global temperatures of a mere 4C from its current average i.e. a mere one-seventh of the 33C temperature increase produced by global warming, would produce massive ice sheets over much of the north american and euro-asian continents.

B: The Earth’s Climate over the Last Few Million Years.
Despite the sun’s increasing luminosity, the Earth has not become hotter but has recently moved into an ice age.[2] The Earth’s climate has been oscillating between ice ages and inter-glacials, “Ice ages tend to last for 100,000 years. The spell between them, usually, lasts for 10,000 years.” (Tim Radford 'The Crisis of Life on Earth. Our Legacy from the Second Millenium. Thorsons Publishing Group 1990. p.135).

This is not the first time the Earth has experienced a spate of ice ages, “It used to be thought that there had only been four or five ice ages, and all within the last one or two million years. Now it is clear that ice ages occurred much earlier in the Carboniferous period (between 345-280 million years ago) and the Permian period (between 280-250 million years ago) and that there were many of them, interspersed with warmer interglacials.” (Dick File ‘Weather Watch’ Fourth Estate, London 1990 p.6).

In terms of the Earth’s recent history, these oscillations are rather strange. It is not known why they are happening nor what is preventing the climate from veering off into a runaway ice age or runaway global warming. There are a number of theories. Firstly, some commentators support the astronomical theory of climate change - that these oscillations are caused by changes in the shape of the Earth’s orbit, “Roughly, the ice ages of the past (about 10 in the last million years) correspond to a 100,000 year cycle; the cycle of the change in the Earth’s orbit from elliptical to circular and back again.” (Tim Radford 'The Crisis of Life on Earth. Our Legacy from the Second Millenium. Thorsons Publishing Group 1990. p.143); “The best explanation of the recurring pattern of ice ages is the changing orbital geometry of the earth as it moves around the sun, which alters the balance of heat between the seasons. The key to the ice ages, it turns out, is that when northern hemisphere summers are sufficiently cool, snow that falls in winter on the land at high latitudes does not melt, but stays and gradually builds up into great ice sheets; the process is reinforced because shiny white snow and ice fields reflect away incoming solar heat, keeping the planet cool .. An ice age ends only when the changing astronomical influences bring very hot northern summers, capable of melting the ice ..” (John Gribbin “In the Beginning. The Birth of the Living Universe’ Viking, London 1993 p.129)

Gribbin believes that astronomical changes triggered the greenhouse effect into reinforcing these changes, “How is carbon dioxide removed from the air when the world cools? During an ice age the world is dry. Winds blow the dust from the arid land out over the oceans, where the iron in the dust helps marine organisms to grow. One effect of this is that plankton thrive, absorbing carbon dioxide, turning it into carbonates in their shells, and dropping it onto the sea floor when they die. Another is that marine algae thrive, increasing the cloud cover of the planet - and clouds reflect away some of the heat of the Sun.” (John Gribbin “In the Beginning. The Birth of the Living Universe’ Viking, London 1993 p.130-131). In other words, when astronomical changes push the Earth towards an ice age this increases marine photosynthesis, decreases the concentration of atmospheric Carbon and thus boosts global cooling. Unfortunately, gribbin does not explain why the Earth does not get colder and colder when astronomic changes decrease the concentration of atmospheric Carbon; and he does not explain how astronomic changes which warm the Earth help to boost the greenhouse effect. The major drawback of the astronomical theory though is that since the Earth’s orbit around the sun hasn’t changed for aeons, it does not explain why these climatic oscillations started a mere 5-2 millions years ago.

Secondly, another commentator believes the arrival of ice ages was caused by the rise of the Rocky mountains which disturbed wind and ocean currents. This hypothesis is much better placed to help to explain the more recent ice age oscillations.

Finally, the gaian theory is that ice ages are a means of combatting the sun’s increasing luminosity, “In the last few tens of millions of years the solar output has reached a level where it is becoming increasingly difficult for the CO2 pumping system to operate. To keep cool when the solar output is as high as now requires efficient pumping by the system so that a carbon dioxide level below 200 parts per million is sustained.” (James Lovelock ‘Gaia. The Practical Science of Planetary Medicine’ Gaia Books Ltd, London 1991 p.148). The Earth’s response to increasing solar radiation is to extract more CO2 from the atmosphere thereby decreasing the greenhouse effect. This has happened through the evolution of new Plants which are able to retain more Carbon and also carry out Photosynthesis in conditions where there is less Carbon in the atmosphere, “Although the appearance of trees (in the geological past) may not have altered the overall rate of CO2 deposition, they have increased the efficiency of the process.” (Lawrence E Joseph ‘Gaia. The Growth of an Idea’ Arkana, England 1990 p.133). It is believed that once the level of atmospheric Carbon is reduced even further than is common during the ice ages then Trees will die out.

In contrast to the astronomic theory of climate in which astronomic changes are reinforced by marine biological activity, gaians argue that the astronomical changes are opposed by marine Photosynthesis. In other words, when astronomic changes begin to cool the Earth, marine activity declines in order to boost the level of atmospheric Carbon and decrease cloud cover whilst, at the other extreme, when astronomic changes warm the Earth, marine activity increases to decrease the concentration of atmospheric Carbon and increase cloud cover, “Since the major agents of fluxes between the atmosphere, the terrestrial and oceanic pools of carbon dioxide are living organisms, the astronomical forcing factors must somehow promote or demote organic productivity. The implication is that during ice ages organic productivity was higher than during interglacials ..” (A M Mannion ‘Global Environmental Change. A Natural and Cultural Environmental History’ Longman New York 1991 p.321).

C: The Earth’s Climate over the Last 10,000 Years.
The Earth’s climate has varied considerably since the last ice age, “The most recent ice age was at its coldest 20,000 years ago. It began to relent about 15,000 years ago, after which the world warmed rapidly, reaching its hottest perhaps 6,000 years ago.” (Fred Pearce ‘Climate and Man. From the Ice Ages to the Global Greenhouse’ Vision Books, London 1989 p.12). Despite the changes in the climate, global average temperatures have been stable, “Since the end of the last ice age, about 10,000 years ago, global surface temperatures have probably fluctuated by little more than 1%.” (JT Houghton: GJ Jenkins and JJ Ephraums 'Climate Change. The IPCC Scientific Assessment' Cambridge University Press, Cambridge 1990 p.xxviii).

It has been pointed out above that the stability of the Earth’s average temperature over the aeons is a remarkable phenomena. Given the huge, global-wide, changes which humans have inflicted on the Earth since the end of the last ice age it is even more remarkable that there has been so little change in global temperatures. As the ice sheets retreated at the end of the last ice age, the Earth’s landmasses were gradually covered in Forests, “Forests once covered about 90% of the surface of the Earth.” (Herbert Giradet ‘Earthrise. How We Can Heal our Injured Planet?’ Paladin, London 1992 p.12). Some regions, like the Mediterranean, which are now deserts, were once luxurious Forests teeming with a wide array of Wildlife. The scale of global deforestation since this time is extensive, “Over the last 10,000 years, the earth’s mantle of forests and woodland has shrunk by a third as trees were cleared to make way for crops, pasture and cities.” (Sandra Postel and John C Ryan 'Reforming Forestry' in Lester Brown, ed 'State of the World 1991. A Worldwatch Institute Report on Progress Toward a Sustainable Society' Earthscan Publications Ltd, London. 1991. p.74). “Two thousand years ago, the tropical rainforest alone extended over 5 billion acres, covering 12% of the earth's land surface.” (Jeremy Rifkin 'Biosphere Politics. A New Consciousness for a New Century' Harper San Francisco 1991 p.73). The situation now is that, “One third of the Earth’s total land surface is covered by forests, of which 45% or two billion hectares are tropical.” (Worldwide Fund for Nature Special Report no.6 May 1991 p.10); “The planet’s mantle of trees .. (is) .. shrinking by more than 11 million hectares per year.” (Alan P Durning 'Ending Poverty' in 'State of the World 1990' A Worldwatch Institute Report on Progress Towards a Sustainable Planet' Unwin Paperbacks, London 1990 p.187). For the first time in history, it is possible to envisage the eradication of the boreal Forests of Canada and Alaska, as well as the world’s tropical rainforests, “The rate of destruction of tropical forests means that by the end of the century and given current trends, nearly all forests will be gone in India, Thailand, Vietnam, the Philippines, Madagascar, East Africa, West Africa, and central America, and virtually all primary forest will be eliminated in Burma and Ecuador.” (Norman Myers 'Deforestation Rates in the Tropical Forests and their Climatic Implications' Friends of the Earth 1989). It is highly surprising that although the Earth has lost such a vast scale of tropical and temperate Forests, global average temperatures have not varied by more than 1%. This seems to suggest that Forests are not vital for controlling the Planet’s global average temperature.

D: The Next Ice Age?
At the moment the Earth should be coming to the end of its current inter-glacial and, if it was evolving according to its own tendencies, would be heading towards the next ice age, “The present interglacial warm period could be regarded as a fever for Gaia and that left to herself she would be relaxing into her normal, comfortable for her, ice age.” (Lovelock 'Stand Up for Gaia' Resurgence no.132 January/February 1989 p.10); “The earth is anyway moving steadily towards a position on the Milankovich cycle where solar heating is low and an ice age due.” (James Lovelock ‘Gaia. The Practical Science of Planetary Medicine’ Gaia Books Ltd, London 1991 p.152).

III: Humans Changing the Climate.
Humans have had an impact on the local, and, probably, even the global, climate ever since they evolved as a species some two million years ago - which was, by some estimations, around the same time as the start of the Earth’s periodic ice-ages.[3] Since the beginning of the industrial revolution, however, the over-industrialized world has been dumping so much pollution into the atmosphere and deforesting such vast areas of the Earth, they have started to boost global warming, “Global mean surface air temperature has increased 0.3C to 0.6C over the last 100 years, with the five global average warmest years being in the 1980s.” (JT Houghton: GJ Jenkins and JJ Ephraums 'Climate Change. The IPCC Scientific Assessment' Cambridge University Press, Cambridge 1990 p.xii). More recent evidence shows that, “The eight hottest years (globally averaged) in the past century were, in increasing order: 1980, 1989, 1981, 1983, 1987, 1988, 1991, 1990.” (D.H. Meadows, D.L. Meadows & Jorgen Randers 'Beyond the Limits. Global Collapse or a Sustainable Future' Earthscan, London 1992 p.92).[4]

It is suspected that the only reason global average temperatures have not increased much more dramatically in line with the wholesale geophysiological damage caused by over-industrialized oomans is because the Earth may have been heading back into another ice age. Human induced global warming could be offsetting the return of the next ice age .. “global mean surface temperature has increased by 0.3 to 0.6C over the last 100 years. Thus the observed increase could be largely due to this variability; alternatively this variability and other human factors could have offset a still larger human-induced greenhouse warming.” (IPCC 'Climate Change 1992. The Supplementary Report to the IPCC Scientific Assessment' Ed by J T Houghton, B A Callander & S K Varney World Meteorological Organization/United Nations Environment Programme Cambridge University Press, Cambridge 1992 p.5). One commentator goes even further and suspects that the Earth’s climate began slipping back into an ice age during the medieval period but was dragged out of it by the destruction which humans inflict on the Earth during that time, “As Gribbin has pointed out, there is the real possibility that the enhanced greenhouse effect is preventing the onset of the next ice age. It is also pertinent to examine the possibility that it may have already done so. There is widespread evidence for cooling during what is generally recognized as the ‘Little Ice Age’ of the fourteenth to the early 19C. While it is unequivocal is that interglacial environments were characterized by climatic variation .. there is no precedent for cold periods similar to the ‘Little Ice Age’ in earlier interglacial periods.” (A M Mannion ‘Global Environmental Change. A Natural and Cultural Environmental History’ Longman New York 1991 p.321). The impact of the over-industrialized world on the Planet’s global temperature is becoming so overwhelming it is threatening not merely to delay the next ice age but to create the conditions for runaway global warming which could devastate the Planet’s geophysiology.

In conclusion, life, including humans, has always influenced the Earth’s average temperature and thus the climate so what is happening today is no different - except in scale and rapidity - to what has happened throughout most of the Earth’s history. Whether humans had evolved or not, the Earth’s climate would still undergo constant change. If, at the moment, humans ‘lived in harmony with nature’ and minimized their interference of the Planet’s geophysiology then huge ice sheets may already have begun to appear, or would soon start to appear, across the northern continents. It is clear that if the human race wants to survive in perpetuity on Earth then it must prevent the return of an ice age and, far more pertinently, prevent the over-industrialized world from generating a climate like that found on Venus. Humans should aim to maintain climatic stability.


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