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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