PART THREE: THE STABILIZATION OF THE CLIMATE |
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Part three
looks at how the Earth stabilizes the climate preventing either a runaway
global burning, or a global freezing, disaster. Over the last few aeons,
geophysiological factors have prevented the climate from lapsing into
a climatic extreme. Unfortunately, the Earth’s ability to stabilize the
climate is currently in decline. Lovelock believes that over the last
few million years, the primary factor preventing the climate from slipping
towards a climatic extreme has been astronomic forcing.
ONE: THE EARTH’S MODERATION OF GLOBAL WARMING.There are a number of geophysiological factors
which oppose a rise in the Earth's average temperature and prevent the
climate from continually getting hotter. 3.1.1.1: The Rate of Photosynthesis.
Over the last few aeons, the rate of Photosynthesis has had a cybernetic
role in stabilizing the Earth’s climate. When the Earth’s temperature
rises there is an increase in the rate at which Photosynthesis extracts
Carbon from the atmosphere thereby decreasing global temperatures. However,
the moderating role of the rate of Photosynthesis would be lost if global
temperatures reached 18C. 3.1.1.2: A Rise in Carbon Emissions; an Increase in Terrestrial Photosynthesis
- the Fertilization Effect.
If there is a sudden release of Carbon into the atmosphere, whether from
an earthquake, volcanic eruption or Forest fire, this boosts Photosynthesis
thereby moderating the increase to the greenhouse effect. However, since
the Photosynthetic extraction of Carbon from the atmosphere is a response
to the release in Carbon emissions, the moderating effect is always less
than the boost to global temperatures. Half of the Carbon released into
the atmosphere is still there a hundred years later so climatic moderation
occurs only marginally over a long period of time.
3.1.1.3: Soil Decomposition boosts Photosynthesis.
The warmer the climate, the greater the soil decomposition, the greater
the release of nutrients into the soil. This boosts Photosynthesis and
moderates the greenhouse effect, "Another possibility is that higher
temperatures would increase rates of organic decomposition, which in turn
would release nutrients to the soil and thus potentially boost the productivity
of Trees." There are a number of ways in which the greenhouse effect contributes
to the moderation of global warming. 3.1.2.1: Methane Depletion of the Ozone Layer.
As the Earth warms, increasing amounts of methane are released from Peatbogs
and methane deposits on ocean floors. If methane rises through the atmosphere
into the stratosphere it damages the Earth's ozone layer. Since ozone
is a greenhouse gas this moderates the greenhouse effect. However, once
again, the reduction in the greenhouse effect caused by the depletion
of stratospheric ozone lags behind the boost to the greenhouse effect
caused by the release of methane so the moderating role of stratospheric
ozone depletion is secondary. 3.1.2.2: Hydroxyl Radicals as a sink for Methane.
Atmospheric hydroxyl radicals react with methane and are thus regarded
as a methane sink, "Methane is primarily removed by a reaction with
hydroxyl radicals (OH) in the troposphere. This reaction represents a
sink of about 400-600 million tonnes per year." The reaction between
hydroxyl radicals and methane creates water and Carbon dioxide. Whilst
hydroxyl radicals are a sink for methane they are not a sink for Carbon.
The conversion of methane into Carbon dioxide reduces the greenhouse effect
because the global warming potential of methane is greater than that of
Carbon dioxide. Although the same amount of Carbon remains in the atmosphere
there is a decrease in the greenhouse effect because of the conversion
of methane to Carbon dioxide. 3.1.2.3: Forests.
3.1.2.3.1: The Dust Released by Forest Fires.
The warmer the climate, the greater the number of Forest fires, the greater
the release of aerosols. Aerosols contain nutrients which boost Photosynthesis
and this reduces the greenhouse effect. This happens whether the nutrients
end up on the land or in the sea, "If iron controls the productivity
of the oceans and thereby the natural level of atmospheric CO2 it follows
that iron supply to the oceans could affect global temperatures through
the heat trapping properties of CO2. Iron in the surface ocean comes mostly
from dust in the atmosphere, soaked up from deserts or other arid regions.
Measurements from ice-ages in Antarctica show that levels of wind blown
dust were regularly higher during the ice ages which would explain why
the atmospheric Carbon dioxide levels were substantially lower then."
Forest fires boost the greenhouse effect (through the
release Carbon) before Photosynthesis moderates the greenhouse effect
(through the extraction of atmospheric Carbon). On the other hand, the
release of dust does not boost the greenhouse effect - it just boosts
the Photosynthetic effect thereby countering the greenhouse effect. It
is not known whether Forest fires’ contribution to the moderation of global
warming through the release of aerosols is greater than the boost to global
warming caused by the release of Carbon emissions. Forest fires have multiple
impacts on the climate. Other impacts will be highlighted below.
3.1.2.3.2: Forest Fires and the Burial of Charcoal.
Some Forest fires moderate global warming through the creation of charcoal.
It depends on the type of Trees in the Forest, "When a tree, such
as an oak, burns incompletely and charcoal is formed, the burial of carbon
results. However, not all trees burn this way: a resinous piece of pinewood,
or a piece of eucalyptus, will practically explode into flames, leaving
next to nothing but the gases of combustion." The creation of charcoal permanently removes Carbon from planetary circulation
because it cannot be absorbed by micro-organisms and returned to the atmosphere,
"It might be that fires themselves are the regulators of oxygen.
There is no shortage of lightning strikes for their ignition. If fires
are the regulator it cannot be a simple relationship. Fires would lead
to the burial of much more Carbon because charcoal is entirely resistant
to biological degradation. Paradoxically fires lead to more oxygen in
the long run. If this grim scenario is followed to a conclusion there
would at first be a positive feedback on oxygen, but soon the Forests
would be so devastated that Carbon production would fall to the point
where oxygen was near or below its present level. A more subtle regulation
involving fire would come from the effects of fire ecology on selection
pressure." Recent research suggests this role is far more important than has previously
been assumed, "For years, everyone has assumed that plankton and other
marine organisms play a key role in regulating the amount of carbon dioxide
in the Earth's atmosphere. But they may have been given more credit than
they deserve, according to a new study which suggests that half of the
carbon found in ocean sediments may not have been removed from the atmosphere
by marine life but in fact came from forests. David Verardo, a geologist
at the University of Virginia in Charlottesville, was addressing this
question by studying organic matter in sections of a core of sediment
drilled from the bottom of the Atlantic. Amazingly, about half of all
the carbon in the core turned out to be charcoal .. In some sections,
charcoal accounted for as much as 90% of the carbon. His explanation is
that high winds, generated by the large temperature gradients which huge
ice sheets created, transported an unusual amount of debris and charcoal
dust from fires far out to sea." 3.1.2.4: The Consumption of Phytomass.
Decomposers play a vital role in consuming Phytomass (Plants) and biomass
(dead plants/Animals/manure) and then making the nutrients available to
Plants thereby stimulating further Photosynthesis. If the decay of Phytomass/biomass
occurred only as a result of weathering by the elements then most of the
Carbon would end up in the atmosphere boosting the greenhouse effect.
When the decay is aided by either micro-organisms or Animals more of the
Carbon is returned to the soil, thereby boosting Photosynthesis and moderating
global warming. For the first few aeons of the Earth’s history the main decomposers/scavengers
were micro-organisms but as Animals began to emerge they too began to
play a role in Phytomass/biomass decomposition. When Trees emerged on
Earth some 300 million years ago, they were so tough it would have taken
a long time for the elements to decomposed them. It would take less time
for micro-organisms to break them down. However, when larger forms of
Wildlife appeared they were able to break up Trees, and make the nutrients
available for the soil, much more quickly. According to lovelock, the
appearance of large Plants and Animals in the proterozoic period enabled
Phytomass/biomass to be broken down so rapidly that it led to the development
of an oxygen atmosphere, "The proterozoic period .. is poorly understood.
Scientists know that for the most part it was a world of micro-organisms
like the Archean. Unicellular life was hardly vigorous enough to bury
the larger quantities of Carbon needed to sustain a high level of oxygen
by counteracting its rapid removal by reaction with the rocks. I think
that oxygen did not increase much above 1% until the evolution of large
plants and animals."
3.1.2.5: Photosynthesizers Conserve Water and Reduce the Greenhouse Effect
of Water Vapour.
Some scientists believe that as global temperatures rise, Plants conserve
more and more water, "According to results published yesterday, Plants
may respond to extra Carbon dioxide in the atmosphere by conserving water.
This would create a drier world, with fewer clouds and less rainfall,
scientists said yesterday. Although the rainfall cycle depends on evaporation
of seas and lakes, huge quantities of water are transpired through the
leaves of Plants. (In the experiments Carbon rich atmospheres produced
a reduction in) the transpiration of water by 9%. The implication is that
there would be less water for cloud formation and a reduction of rainfall
by 6%. This was the reverse of computer models, which suggested a warmer,
wetter world." If this is true it will reduce the amount of water
vapour in the atmosphere and thereby moderate global warming.
3.1.2.6: Water Dissolving Carbon in the Atmosphere.
Carbon is removed from the atmosphere when it is dissolved by rainfall.
If there is more rainfall as a result of a rise in global temperatures
this will extract more Carbon from the atmosphere thus moderating global
warming. This section explores the albedo effect’s contribution to the moderation
of global warming.
3.1.3.1: Forests.
3.1.3.1.1: The Albedo Effect of the Cloud Cover Created by Forests.
If there is an increase in global temperatures there will be an increase
in the scale of the taiga Forest which will boost cloud cover and thus
moderate global temperatures. 3.1.3.1.2: The Albedo Effect of the Dust Released by Forest Fires.
As global temperatures rise there is an increase in Forest fires. Forest
fires release dust which increases the Earth’s albedo effect and thus
moderates global temperatures. 3.1.3.1.3: The Dust Released by Forest Fires stimulates Marine Algae
and boosts the Albedo Effect of Clouds.
As global temperatures rise there is an increase in Forest fires. The
aerosols released by Forest fires boosts the growth of marine Algae. Marine
Algae release dimethyl sulphide which stimulates cloud formation and thereby
moderates global temperatures. 3.1.3.2: Marine Algae.
3.1.3.2.1: Dust stimulates Marine Algae and boosts the Albedo Effect
of Clouds.
As global temperatures rise there is an increase in winds, which causes
an increase in wind erosion. The winds blow dust from deserts or drought
stricken areas into the sea boosting the growth of marine Algae. Marine
Algae release dimethyl sulphide which stimulates cloud formation, moderating
the rise in global temperatures, "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." Lovelock believes marine Algae are an important influence on the Earth’s
climate. He concludes that the white Daisies in his Daisyworld computer
model represent, in the real world, oceanic Algal blooms, "We can
speculate that the blankets of white marine stratus clouds reflecting
sunlight back to space above the Algal blooms of the ocean, are the white
Daisies, and the dark conifer Forests of the Northern temperate regions
are the black Daisies."
3.1.3.3: Oceans.
3.1.3.3.1: The Increase in Evaporation from the Oceans Increases the
Albedo Effect of Clouds.
A rise in global temperatures increases the evaporation of water from
the oceans which boosts the greenhouse effect. If, however, water vapour
is converted into clouds this increases the Earth’s albedo effect and
moderates global cooling, "Any overall rise in temperature will mean
an increase in the warming of moist air masses over the oceans. Global
warming will lead to an increase in cloud cover which will, in turn, help
to nullify the greenhouse effect."
3.1.3.4: Peatbogs.
3.1.3.4.1: The Increase in Evaporation from Peatbogs will Increase the
Albedo Effect of Clouds.
As the Earth warms, Peatbogs release more water vapour which increases
the albedo effect thereby cooling the Earth, "In summer they transpire
more water than Forests, stimulating the formation of reflective clouds."
3.1.3.5: Deserts.
It has been alleged that Micro-organisms reduce the albedo effect of
deserts, "Today such microbial terrestrial communities inhabit the
deserts in places where plants cannot live. These ‘cryptogamic’ microbial
crusts are essential agents that hold thin soils against erosion. .. the
surface temperature of Earth in the earliest days of land life, though
hot by our standards, was nevertheless significantly cooler than the hell
it would have been without this microbial crust." 3.1.4.1: The Oceans.
3.1.4.1.1: Ocean Currents Release Cool Water.
In the light of the 1997 el nino, the validity of the following phenomenon
is questionable but it is included just in case, "A team based in
new york has found that as the Earth warms up, currents in the tropical
pacific change so that more cold water reaches the sea’s surface, causing
air around the world to cool. This feedback mechanism is keeping global
warming in check - at least for now. .. the temperature difference between
the cool east and warm west should increase. This temperature difference
in turn drives the trade winds, which blow westwards, taking surface water
with them and allowing more cold water to reach the surface in the east." 3.1.4.2: Forests.
The warmer that global temperatures become, the smaller the scale of
the Rainforests, the less solar energy they absorb. This cools the Earth
and stabilizes the climate. As far as the taiga Forests are concerned
the opposite is true: the warmer the global temperatures, the greater
the scale of the taiga Forests, the greater the solar energy they absorb,
the greater the heat effect. However, it also has to be considered that
a rise in global temperatures could damage the taiga Forest and thus moderate
its boost to global temperatures, "Boreal Forests are likely to have
the hardest time in terms of climate change because they are in the regions
where the temperature is expected to rise faster than anywhere else 4-5C
above current temperatures." 3.1.4.3: The Limitations to the Evaporation of Water.
Some commentators have suggested that a rise in global temperatures will
lead to an increase in evaporation which will boost global warming. One
commentator has even argued this process is exponential, "As increases
in carbon dioxide warm the surface and the atmosphere, more water evaporates
from the surface and remains in the atmosphere. In fact, the amount of
water vapor that can be held by the atmosphere increases exponentially
with temperature." However, bunyard highlights the limitations of
this positive feedback process .. "this situation cannot go on forever
and a point is finally reached when the dynamics of water evaporation,
followed by precipitation, cancel each other out." 3.1.5.1: Rock Weathering.
Chemical weathering takes place when acidic rainfall dissolves minerals
from rocks whether these are on the surface or in the soil. Three types
of acid rain contribute to rock weathering; sulphuric acid, nitric acid
and Carbonic acid. Sulphuric acid is created through sulphur emissions
released either by volcanic eruptions or by marine Algae. Carbonic acid
is produced when water vapour/rainfall dissolves Carbon in the atmosphere,
"CO2 is slightly soluble and a little of it dissolves from the air into
rainwater, turning the water into weak carbonic acid (H2CO3). The carbonic
acid reacts with compounds of calcium, silicon, and oxygen in rock." The chemicals created by the reactions between acids and rocks, leech
through the soil into waterways and eventually drain into the seas, "Calcium
and bicarbonate (HCO3) are released and carried, dissolved in the water,
eventually to the sea." The Carbon is taken up by marine Algae, "Calcium
and bicarbonate (HCO3) are released and carried, dissolved in the water,
eventually to the sea. Once in the sea, living organisms convert the calcium
and bicarbonate into insoluble calcium carbonate (CaCO3) from which they
make their shells."; "Some algae (the diatoms) take the silicic acid to
make their skeletons; and other algae (the coccolithophores) take their
calcium bicarbonate to make skeletons of calcium carbonate." After marine micro-organisms have died their shells fall to the ocean
floor. Over millions of years, huge quantities of shells accumulate on
the ocean floor. They are gradually compressed, under their own weight
and the water above them, into limestone, "The fall of tiny shells from
the dead algae (coccolithophores) is responsible for calcium carbonate
and silica deposition in the sediments of the ocean floor..."; "The
concentration of CO2 in the mixed layer of the ocean, the top 250 feet,
is as much as the entire atmosphere itself. In this region of the ocean,
micro-organisms use the carbon dioxide in the form of bicarbonate to make
their skeletons and shells. When the animal dies, its hard shell or skeleton
settles on the bottom of the ocean where it contributes to the formation
of carbonate rock. If the calcium carbonate falls to greater depths, it
is dissolved in the cold deep waters of the abyssal. The abyssal region,
by virtue of its great volume, holds the vast majority of free carbon
dioxide." According to lovelock, rock weathering is the most important means of
removing Carbon from the atmosphere, "The abundance of CO2 in the
air depends on the balance between the amount being injected from beneath
the crust through volcanoes and the amount lost from the air by chemical
reaction at the Earth’s surface."; "Calcium silicate rock .. is the
only true sink for carbon dioxide." Lovelock believes that life accelerates rock weathering, "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 readily 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."; "If
the soil of a well-vegetated region almost anywhere on Earth is examined,
the Carbon dioxide content is between 10 and 40 times higher than the
atmosphere. What is happening is that living organisms act like a giant
pump. They continuously remove Carbon dioxide from the air and conduct
it deep into the soil where it can react with rock particles and be removed.
Consider a Tree. In its lifetime it deposits tons of Carbon gathered from
the air into its roots, some carbon dioxide escapes by root respiration
during its lifetime, and when the Tree dies the Carbon of the roots is
oxidized by consumers, releasing Carbon dioxide deep in the soil. In one
way or another living organisms on the land are engaged in the business
of pumping Carbon dioxide from the air into the ground. There it comes
into contact with, and reacts with, the calcium silicate of the rocks
to form calcium carbonate and silicic acid. Were life not present, the
carbon dioxide from the atmosphere would have to reach the calcium silicate
of the rocks by slow inorganic processes like diffusion." "Chemical
weathering of calcium and magnesium silicates in rocks is a much bigger
Carbon sink, and one that absorbs Carbon at 4 times the rate it is buried
as reduced organic Carbon. Chemical weathering acts as a sink for Carbon,
locking it up in limestone." 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." Forests play a major role in rock weathering, "Most geochemists
agree that Forests promote the chemical weathering of the crust, a process
that removes carbon dioxide from the atmosphere and thus tends to reduce
the greenhouse effect and global temperature. Organisms that influence
the global environment, like .. trees, which promote weathering, all perform
their vital functions for other reasons. .. trees create acidic soils
to acquire mineral nutrients. The dms climate feedback appears to be positive
today so climatic stability probably relies on stabilizing factors such
as the tree-weathering feedback."; "Solid support for increased
weathering by vegetation is coming from experiments .. We usually think
of trees as defined by trunks, branches, and leaves. But as a recent biochemical
guild (assemblage) of gaia, it may be tree roots that are most significant
in altering the cycle of elements. In the largest taxonomy of the guilds,
trees are photosynthesizers, big siblings to algae and cyanobacteria.
But they occupy a unique slot as rooted photosynthesizers. Rooted photosynthesizers
have worked distinctive effects on the cycles of carbon and other elements." Lovelock speculates that because Plants absorb, and release, roughly
the same amounts of Carbon, the Carbon added to the atmosphere by volcanoes
might be expected to increase the greenhouse effect. The reason it doesn’t,
he believes, is because volcanic emissions are balanced by rock weathering.
Geological rock weathering would not be fast enough to extract the Carbon
dumped into the atmosphere through volcanic eruptions. Rock weathering
needs micro-organisms to speed up the process, "Without the organisms
- with only the slow diffusion of carbonated rainwater through the rocks
- carbon dioxide would build up to a far greater concentration, he argues,
perhaps 100 times what it actually is, before reaching equilibrium. Such
a concentration of carbon dioxide would have a massive greenhouse effect:
Earth would be uninhabitable." Rock weathering moderates global warming because the warmer the Earth,
the greater the increase in chemical weathering, the greater the deposition
of Carbon, the bigger the decrease in the greenhouse effect, "Chemical
weathering acts as a sink for Carbon, locking it up in limestone. And
the warmer the Earth is, the faster the weathering proceeds and the more
CO2 is taken from the atmosphere. Chemical weathering, transforming calcium
silicates to carbonates, stabilizes the climate, removing more CO2 when
the climate is warmer and less when it is cooler." Rock weathering is
a major geophysiological process stabilizing the climate. Rock weathering is such a powerful factor it not merely moderates global
warming it can also produce global cooling, "The rise of the angiosperms
may have also contributed to global cooling during the last 100 million
years. Volk suggested that the spread of angiosperm-deciduous ecosystems
had caused a higher rate of global weathering, and thus increased fluxes
of Ca and Mg ions from continental silicates contributed to the increasing
importance of calcareous plankton. The plankton precipitation in turn
depleted the atmospheric carbon dioxide."
3.1.5.2: The Drying up of the Tundra.
It has been argued that as global temperatures rise the tundra will release
vast quantities of methane thereby boosting global burning. However, some
commentators believe the reverse is true: the tundra will dry out thereby
decreasing methane emissions. This is because methane is released by tundra
Flowers only in wet conditions whereas, when it is dry, methane is oxidized
by bacteria in the soil .. "in drier tundra soils the release of
methane gas decreased rather than increased. .. it seems that the increase
in temperature from global warming would result in a reduction of the
emission of methane gas from the tundra .." TWO: THE MODERATION OF GLOBAL COOLING.Over the last few aeons the Earth has been able to modify climate extremes
such as global freezing. However, over the last couple of million years,
as the intensity of solar radiation has increased, the Earth has found
it necessary to provoke ice ages in order to stabilize the climate. But
the Earth faces an acute difficulty over the generation of ice ages. Given
the ever increasing output of solar radiation, it is imperative that the
Earth possesses the capability for creating, and maintaining, ice ages.
On the other hand, the Earth has to prevent the climate from lapsing into
a runaway global freezing disaster which could destroy a significant proportion
of life on Earth. It seems as if the Earth needs an almost super-computer
like precision, and all-encompassing controls over its geophysiological
processes, to produce ice ages which combat increasing solar radiation
but don’t veer off into a runaway global freezing. The first chapter outlined
some of the factors preventing global cooling from accelerating into global
freezing. This section explores all such factors. If it ever became possible
to determine the limits of the Earth’s powers to perpetuate ice ages this
would indicate when the Earth is likely to start burning up. Paradoxically,
what has come to the Earth’s rescue is medium term astronomic changes
pushing the Earth out of ice ages and into inter-glacials thereby preventing
the Earth from slipping into a global freezing disaster. 3.2.1.1: The Rate of Photosynthesis.
The rate of Photosynthesis has a cybernetic role in stabilizing the Earth’s
climate. When the Earth’s temperature falls there is a decrease in the
rate of Photosynthesis which allows the build up of Carbon in the atmosphere
thereby boosting global temperatures. However, it is believed the scale
of Photosynthesis has a greater impact on the climate than the rate of
Photosynthesis so it has a greater role in determining what happens to
the climate.
3.2.1.2: The Scale of Photosynthesis.
3.2.1.2.1: The Irregularity of the Reduction in the Scale of Photosynthesis.
Over the last few million years, as global temperatures begin to fall,
so do the level of the Earth’s oceans thereby creating more Forested land
in the tropics than is lost under ice sheets on the amero-euro-asian continents.
This boosts global cooling. However, it is possible the increase in the
scale of Photosynthesis does not occur linearly over time. There may be
a slow down in the cooling trend - although the trend might be resumed
more forcefully later if it rebounds from such a constraint.
3.2.1.2.2: Cooling Damages Tropical Photosynthesis.
The fall in global temperatures might eventually affect the climate in
the tropics thereby reducing the rate of Photosynthesis carried out by
tropical Rainforests. This would decrease the extraction of Carbon from
the atmosphere and thus boost the greenhouse effect.
3.2.1.2.3: No further Increase in the Scale of Photosynthesis.
It is possible that as global temperatures fall there comes a point when
there is no further net increase in Forested land. This would stop the
Earth’s temperatures from falling any further. It is possible this factor
might produce an end to the current system of climate regulation before
the removal of all Carbon in the atmosphere.
3.2.1.2.4: The End of Photosynthesis.
The most obvious limit to the possibility of a spiralling global freezing
disaster is that once all the Carbon has been extracted from the atmosphere
it would not be possible for Photosynthesis to drive down global temperatures
any further.
3.2.1.3: Burning, and Suffocating, Peatbogs.
When global temperatures fall, Peatbogs absorb more atmospheric Carbon
thereby reinforcing global cooling. However, there are two limitations
preventing Peatbogs from provoking a perpetual ice age on Earth. Firstly,
Peatbogs boost the level of atmospheric oxygen which produces fires that
destroy Peatbogs, "Klinger speculates that the cycle (of Peatbogs
driving down temperatures which help to further drive down temperatures)
gets broken by the very success of the sedge mosses. Thus, in the equation
of Carbon dioxide drawdown and the burial of organic Carbon, oxygen gets
released into the atmosphere and tends slowly but surely to rise. Higher
oxygen levels mean that peatlands dry out and become more susceptible
to burning, causing Carbon dioxide levels to rise and large quantities
of methane to be released." Secondly, the ice sheets spreading across the amero-euro-asian continents
bury both Forests and Peatbogs. Peatbogs no longer extract Carbon from
the atmosphere thereby inducing global warming, "The advancing ice
of the glacial period also destroys the bogs and the process therefore
become self-limiting."; .. "peatlands could have been an important
part of the biological mechanisms that many believe have helped plunge
the Planet into and out of glaciation. Alterations in the extent of Peatbogs
would change the concentration of Carbon dioxide in the atmosphere by
up to 20%. Global cooling would encourage the growth of Peatbogs, at the
expense of Forests. Over thousands of years, the Peatbogs would extract
Carbon from the atmosphere and store it, so reducing the natural greenhouse
effect and driving temperatures still lower. Eventually ice sheets would
cover the bogs, perhaps helping to trigger the end of the glaciation."
3.2.1.4: Clouds Reduce Photosynthesis.
If global cooling increases cloud cover, this would reduce Photosynthesis
and moderate the fall in global temperatures, "More reflective clouds
dampen photosynthetic potential (of marine Phytoplankton) by reducing
the light that reaches the surface (of the oceans)." 3.2.2.1: Historical Examples of Carbon Emissions Combating Global Cooling.
If global temperatures fall and greenhouse gases are released into the
atmosphere this would moderate global cooling. There are historical examples
of Carbon escaping into the atmosphere and moderating falling temperatures.
3.2.2.1.1: Historical Perspective.
"Studying the isotope geochemistry of ancient rocks, geologists
found evidence that methanogenic bacteria was indeed a dominant fossil-organism
during the interval 2.9 to 2.5 billion years ago. (Methanogenic bacteria
are single celled creatures which convert carbonate mineral into methane
which heats the Earth). Their release of methane was to keep the Earth
warm enough to sustain life. When our planet was again over-heated, gaia
gave us cyanobacteria, an ‘air conditioner’ because it precipitates limestone.
This new lifeform was the dominant lifeform until some 650 million years
ago, when the over-zealous ‘air conditioner’ was about to turn the Earth
into an ice-box. Gaia had to act, and the new life forms were soft bodied
Animals: worms, Meldusas, etc. They ate up cyanobacteria, and gave back
to the atmosphere the Carbon dioxide and water .."
3.2.2.1.2: The Spurt of Carbon Emissions at the end of the last Ice Age.
Lovelock believes that at the end of the last ice age there was a sudden
release of Carbon emissions, "We know that Carbon dioxide has fallen
in abundance during the Earth’s history, but it jumped from 180 to near
300 ppm within a hundred years as the last glaciation ended. A rapid rise
like this cannot easily be explained by the slow processes of geochemistry."
He speculates that, "The sudden increase of CO2 that came before
the present inter-glacial could not have been due to a reduction in the
weathering rate. More probably it was connected with the decline of the
ocean algal system and with changes in the Peatbog ecosystems, as proposed
by lee klinger in 1991."
3.2.2.2: The Failure of Carbon Burial in the Oceans.
3.2.2.2.1: The Oceanic Absorption of Carbon; Saturation or Sediment?
Huge amounts of Carbon are dissolved in the oceans as a result of rock
weathering, rainfall or absorption from the atmosphere. If the Carbon
in the oceans is taken up by micro-organisms and buried on the ocean floor
then, theoretically, the oceans could continually absorb more and more
Carbon thus perpetually reducing the greenhouse effect - and maybe even
triggering off global freezing. However, if all the Carbon transported
to the oceans remains in solution there would come a point when the oceans
could no longer absorb more Carbon and the excess would be pushed back
into the atmosphere. If global temperatures were falling at the time,
this would moderate global cooling, "If most of the CO2 is absorbed in
solution then a limit will be reached, but if most is trapped in the sediments,
the absorption can continue indefinitely." It is not known whether the
oceanic absorption of Carbon has a saturation point or not. Whilst in
some parts of the ocean, sedimentation seems to take place, in other parts
it does not. There are a number of factors preventing the oceanic burial
of Carbon and they have the effect of moderating the falls in global temperatures.
3.2.2.2.2: The Carbonate Compensation Depth.
Some of the shells of dead marine organisms are prevented from sinking
to the ocean floor by ‘the carbonate compensation depth’. But, even if
Carbon is prevented from reaching the ocean floor this does not mean it
will automatically float back to the surface of the ocean and be released
into the atmosphere, "Carbon dioxide is only slightly soluble in
water and, as with oxygen, its solubility decreases as the temperature
rises. When it dissolves, some of the carbon dioxide forms carbonic acid
(H2CO3), and the remainder bicarbonate (HCO3) ions, and the reactions
proceed in either direction so carbonic acid and bicarbonate are constantly
dissociating and reforming. When water containing carbonic acid, and saturated
with carbon dioxide, comes into contact with rocks containing calcium,
the two react to form calcium bicarbonate {Ca[HCO3]2), which is soluble.
If the water then mixes with water containing little dissolved carbon
dioxide, or is exposed to the air, the calcium bicarbonate will dissociate,
yielding Carbon dioxide, water and calcium carbonate (CaCO3) - which is
insoluble and settles as a precipitate. Calcium carbonate is insoluble
in surface water, but it becomes increasingly soluble at lower temperatures
and at higher pressures it dissociates, releasing carbon dioxide. These
conditions occur in the deep oceans where there is a ‘carbonate compensation
depth’ below which carbonates break down to release carbon dioxide faster
than they form, so that the insoluble calcium carbonate sinking from above
fails to reach the ocean floor and there is no accumulation of sediment.
In the pacific ocean, the carbonate compensation depth lies between 13,000
and 16,500 feet. The release of Carbon dioxide below the carbonate compensation
depth does not return it to the atmosphere, however, because there is
little mixing between deep water and surface water - the deep water is
colder and, therefore, denser than the overlying water." 3.2.2.2.3: Upwelling of Carbon from Seabed.
Even if the shells of dead marine micro-organisms reach the ocean floor
this does not mean they will be permanently buried there as sedimentary
rock, "When the Animal (marine Algae) dies, its hard shell or skeleton
settles on the bottom of the ocean where it contributes to the formation
of Carbonate rock. If the calcium Carbonate falls to greater depths, it
is dissolved in the cold deep waters of the abyssal. The abyssal region,
by virtue of its great volume, holds the vast majority of free Carbon
dioxide. Due to upwelling of CO2-rich waters from the deep ocean ..."
It has been estimated that, "Carbon dioxide exchanges between the
ocean and atmosphere in the equatorial zone east of the international
dateline resulted in 1000 million tonnes of carbon being exported to the
atmosphere as a result of upwelling. This figure would be considerably
higher were it not for biological processes which re-use carbon brought
to the surface by upwelling in the eastern Pacific. Results from the ORSTOM
Research Institute in Noumea, New Caledonia, also indicated that during
El Nino events atmospheric carbon dioxide concentrations tended to increase
less rapidly and during La Nina carbon dioxide measurements indicated
a more rapid increase in atmospheric concentration."
3.2.2.2.4: Phosphate’s Role in Photosynthesis and Carbon Burial.
Lovelock argues that as Carbon is buried on the oceans floors, corresponding
amounts of oxygen are left in the atmosphere so that, over the aeons,
oxygen has in effect replaced Carbon in the atmosphere. Recent research
has suggested this process involves a further stage which moderates the
speed of Carbon burial. Dick holland has shown .. "how the concentration
of atmospheric oxygen in the atmosphere has remained stable at around
20% for the last 300 million years. It has long been presumed that this
was the result of biotic processes such as Photosynthesis and decay. But
Holland believes this is not enough. Oxygen is released to the atmosphere
for the long term, he explains, when Carbon is locked up for the long
term. This happens when the remains of dead marine organisms are deposited
in deep ocean sediments. And the growth of those organisms is limited
by the availability of phosphate, a vital Plant nutrient. Enter ferric
hydroxide, a "powerful scavenger of phosphate" formed in the oceans when
their abundant dissolved iron meets free oxygen. More oxygen means more
ferric hydroxide, which means less phosphate, thus less Photosynthesis,
which means less Carbon deposition in marine sediments, which means less
oxygen in the ocean, and ultimately in the atmosphere too - completing
the loop to make a self-regulating negative feedback cycle." The limit
on Carbon burial makes it more likely that Carbon will escape back into
the atmosphere and thus moderate global cooling. 3.2.2.2.5: Oceanic Decomposers/Fermenters prevent Carbon from being Buried
on the Seabed.
Decomposers at the bottom of the oceans digest organic material and release
methane into the oceans. Bacteria called sulphate reducers gain energy
by splitting sulphate for its oxygen, "Employing the oxygen they
gain in this way, these sulphate reducers feast on the carbon-rich detritus,
excreting carbon dioxide as a waste gas." Some of this methane might
escape into the atmosphere and moderate global cooling, "Oxygen in
the air comes from the burial of Carbon. Consumers are efficient, and
only about 2% of Carbon photosynthesized reaches the sediments, where
most of it is returned to the oxidized environment as methane. So only
one part in a thousand of the Carbon fixed by the plants is buried deep."
The movement of Carbon in the oceans seems just as vigorous as the movements
of Carbon in the atmosphere. 3.2.2.3: Volcanoes Releasing Greenhouse Gases.
Lovelock speculates that rock weathering and volcanism are two key determinants
of the concentration of atmospheric Carbon, "The abundance of CO2 in the
air depends on the balance between the amount being injected from beneath
the crust through volcanoes and the amount lost from the air by chemical
reaction at the Earth’s surface." If global temperatures are falling and
a volcanic eruption releases greenhouse gases this would help to moderate
global cooling. Whilst volcanic eruptions have an influence on the climate they do not
play a climate stabilization role i.e. increasing/decreasing global temperatures
have no effect on the frequency of volcanic eruptions. Volcanoes erupt
for their own geophysical reasons unrelated to the climate - although
some commentators have speculated about a relationship, "A team of US
researchers studying the history of volcanic eruptions in the northern
hemisphere has found that rapid changes in the climate - both cooling
and warming - may be linked with an increase in the rate of volcanic eruptions.";
"Nearly 60% of active volcanoes form islands or occupy coastal sites,
and nearly all of the rest lie within 250 kilometres of a coastline. So
changing sea levels could directly affect the stresses inside nearly all
volcanoes, helping to expel the magma explosively. .. if human activity
were to cause the catastrophic melting of the ice caps, this may well
be followed or accompanied by a burst of elevated explosive volcanic activity.
Nature’s way of cooling the planet may serve as an explosive warning about
the consequences if we continue to tinker with the enormously complicated
global system that is the Earth." 3.2.2.4: Carbon Emissions from Soil Decomposition.
Micro-organisms living in the soil, and in the sediments at the bottom
of lakes, marshes, and rivers, break down organic matter and release methane
which boosts the greenhouse effect. Over the aeons, anaerobic micro-organisms
have played a vital role in pumping Carbon back into the atmosphere, "A
world with photosynthesizers only is unstable. They would soon have locked
up in their bodies most of the available carbon. Their removal of carbon
dioxide would have so weakened the greenhouse that the world would have
frozen, and life ceased. This never happened. There co-existed with the
photosynthesizers simple fermenters, the methanogens. These organisms
processed the organic matter made by the photosynthesizers and returned
the carbon to the air as a mixture of methane and carbon dioxide, restoring
the greenhouse."; "The anaerobic sediments of the soil are also the source
of the methane that removes oxygen from the atmosphere, so keeping the
balance, and is essential to life on Earth." If global cooling increases
soil decomposition, dumping more methane into the atmosphere then this
would help to counter global cooling. 3.2.3.1: The Decrease in Oceanic Evaporation Decreases the Albedo Effect
of Clouds.
As the Earth’s temperatures fall, there is a decline in the evaporation
of water from the oceans. This reduces cloud formation, decreases the
albedo effect of clouds, and thus moderates global cooling. The greater
the fall in global temperatures, the smaller the evaporation of water,
the fewer the clouds, the smaller the albedo effect of clouds, the greater
the global warming. 3.2.4.1: The Heat Effect of the Tropical Rainforests.
The colder that global temperatures become, the greater the scale of
the Rainforests, the more heat which is absorbed and returned to the atmosphere.
3.2.5.1: Rock (Chemical) Weathering.
The colder the Earth, the slower the rate of chemical weathering, the
less Carbon which leeches into the oceans, the less Carbon permanently
stored on the ocean floor, the greater the boost to global warming.
3.2.5.2: The Decrease in Soil Decomposition Decreases Tree Growth.
As the climate cools there is a decrease in soil decomposition, a decrease
in the nutrients available to Trees and thus a decline in Tree growth
which moderates global cooling.
3.2.5.3: Floods counter Ice Sheets.
A freak geophysical event could reverse a period of global freezing,
"A huge flood may have ended one of Earth’s most recent ice ages,
say researchers in canada and the u.s. About 120,000 years ago, a freak
cold spell known as the ‘younger dryas’ shut down the north atlantic gulf
stream for 13,000 years. Without this flow of warm, tropical water to
the north, ice sheets advanced again and left much of northern europe
and north america uninhabitable. Climatologists believe that the north
could only have warmed up again once the gulf stream had restarted. Timothy
fisher and gerald smith .. suggested how the gulf stream might have restarted.
The pair claim that a lake the size of sweden flooded into the arctic
ocean. The heat radiating into the atmosphere when the lake water froze
in the ocean would have disrupted the circulation of air around the north
pole, "jump-starting" the gulf stream. When the lake water reached
the ocean and froze, it gave off some 13.5 billion billion joules of energy
a day, enough to alter global atmospheric circulation, says fisher." THREE: OVERALL CONCLUSIONS.It would be difficult to conclude from the above analysis that the Earth has
a highly-efficient, streamlined, dedicated, climate regulation system in which
every part of the Earth’s life support system contributes, in one way or another,
to the greater good of stabilizing the climate. On the contrary, the Earth seems
to be composed of a chaotic jumble of geophysiological factors pushing and pulling
the climate in every direction. Some factors push the Earth towards climatic
extremes and others moderate such changes. From this perspective it is a wonder
life has managed to survive on Earth let alone flourish. It is only when the
facts of the Earth’s climate history are taken into consideration that climate
regulation becomes apparent. Firstly, the fact that life has existed on Earth
continuously for the last two and a half aeons suggests there has been climate
regulation. Secondly, there is no evidence that the Earth’s climate became so
bad that it destroyed all life on Earth - so that years later it had to restart
again from the beginning. There have been calamities in which substantial proportions
of the Earth’s Biodiversity has disappeared but these mass extinctions were
caused by external disasters rather than the Earth’s climate going off the rails.
A part of the reason why the multiplicity of factors influencing the Earth’s
climate seems so chaotic is scientists’ ignorance about the climate. They have
not yet determined all the factors playing a role in the climate. They haven’t
determined the significance of their roles in the Earth’s climate. They cannot
say what the hierarchy of their significance is, "The relative influence
of life’s stabilizing and destabilizing feedbacks remains uncertain; what is
clear is that climate and natural ecosystems are tightly coupled, and the stability
of that coupled system is an important ecosystem service." The lack of
scientific evidence about the Earth's climate is considerable. The Earth seems to have as many factors destabilizing the climate as stabilizing
it. Scientists’ ignorance makes it difficult to say whether the Earth’s climate
stabilizing factors are more powerful than the destabilizing factors so, once
again, it only becomes obvious that the stabilizing factors are more powerful
when the facts of the Earth’s history are taken into account. The existence
of geophysiological processes that destabilize the climate suggests that the
Earth’s climate regulation ‘system’ is not a machine in which all the elements
fit together and work co-operatively like a watch. Gaia is not a gourmet recipe
with complementary ingredients designed to produce a precise taste experience.
It is more of a hotch potch stew which is rough on the palate but offers substantial
nourishment. The above analysis of the Earth’s two destabilization tendencies suggests the
Earth is much more likely to burn up like venus than it is to freeze like mars.
There seem to be far more factors pushing the Earth in the direction of global
burning than toward global freezing. This poses a considerable danger because
only global burning has the capability of destroying the biosphere. It is unlikely
that global freezing could become severe enough to destroy all life on Earth
and the biosphere itself. Life seems safer during ice ages than it is in periods
of global burning. In terms of Biodiversity, ice ages may cause a considerable
reduction in the numbers of species, especially those on land, whilst periods
of global warming might create an incredible profusion of life but, in terms
of tenure, life is much less insecure during glacial periods than when the Earth
is hotting up. As the Earth warms up there is an increase in the risk of the
climate slipping towards an extreme which could destroy the entire Biosphere.
Whilst life in the oceans seems safe no matter how cold it gets, it is the first
to disappear when global temperatures rise.
The main factor stabilizing the climate over the bulk of the Earth’s history
has been Photosynthesis. Photosynthesis is commonly perceived as being a provider
of food, whilst the most sophisticated bipeds bless it for the production of
oxygen but few appreciate its comprehensive role in making the Earth fit for
habitation and its critical in stabilizing the climate - after all, without
Photosynthesis, there would be no Carbon-based life-forms on Earth, no soil,
no hydrogen, no water, no clouds, no oceans. When the Earth first formed it
was a cauldron of volcanic activity, islands of molten lava, nuclear radiation,
and meteorite bombardments. It faced a sun which, although weak at the time,
would pump out increasing levels of solar energy for the next dozen aeons. It
contained vast quantities of Carbon in the atmosphere which would retain the
increasing levels of heat emitted by the sun. Given the Earth’s position between
venus and mars, it looked as if the Earth was destined to remain a very hot
planet where the prospects for life would increasingly diminish. If there had
been no Photosynthesis on Earth then global average temperatures would now be
in the region of 240-340C, "Without life the Earth would have an atmosphere
comparable to venus, with 98% carbon dioxide, 1.9% nitrogen, a trace of oxygen,
an atmospheric pressure 60 times that of the living Earth and an average surface
temperature between 240C and 340C." Somewhere between the intense heat
of its formation and the increasing intensity of solar radiation, the Earth
must have cooled enough to allow the first few Photosynthesizing organisms to
flourish. Once established, Photosynthesizers started extracting Carbon from
the atmosphere and began reducing global temperatures, preventing the increasing
levels of solar radiation from burning up the planet.
The miracle of Photosynthesis which produces the miraculous cooling of the
Earth means that the role of life on Earth is to keep the planet cool. The cooler
the Earth, the safer life is on the planet. The warmer the Earth, the greater
the danger of the climate slipping back towards its natural (pre-life) state
- the searing temperatures which could be expected from a planet in the Earth’s
position in the solar system. Life artificially cools a naturally hot planet.
Over the last couple of aeons life has stabilized the climate but, over the
last couple of million years the intensity of solar radiation and the depletion
of Carbon in the atmosphere, has meant the Earth is losing this capability.
The climate remains in a stable state merely on a wing and a prayer. It is not
so much geophysiological factors such as Photosynthesis which are preventing
a runaway global burning/freezing disaster, than medium term astronomic forcing.
There are still many geophysiological processes contributing to the stabilization
of the climate but they are weaker than the factors destabilizing it. Paradoxically,
although the sun’s long term increase in solar energy is threatening the Earth’s
climatic stability, it is the sun’s medium term astronomic oscillations which
are currently providing the Earth with a degree of climate stability. Astronomic
oscillations will probably provide declining degrees of climatic stability on
Earth for another few million years, so the Earth’s climate is not under any
immediate threat but, eventually, the sun’s long term increase in solar radiation
will overwhelm the influence of its medium term oscillations. The astronomic
oscillations which change the direction of the Earth’s climate between ice ages
and inter-glacials may gradually start pushing the climate between warm periods
and hot periods and then between hot periods and extremely hot periods, until
the Earth burns up. The factors stabilizing Earth’s the climate have not completely
disappeared and will continue to provide a degree of stability but this degree
is likely to decline over time and, eventually, the Earth will start burning
up. It is difficult determining whether the Earth’s climate stabilization system
is just in terminal decline or has disappeared altogether. Since this system
is composed of different elements then the question has to be answered about
each of those elements. The Earth will lose its ability to regulate the climate:-
when there is no Photosynthesis,
when there is no Carbon in the atmosphere,
when it is unable to create ice ages.
The critical issue seems to be the reduction in atmospheric Carbon. The reduction
in atmospheric Carbon will cause the decline of Photosynthesis and this will
mean the end of the Earth’s ability to generate ice ages.
James lovelock conceived of the idea of the Earth as a self regulating planet
in the 1970s. By the 1980s this revolutionary new perspective was reaping huge
rewards in terms of new scientific hypotheses about the functioning of the Earth’s
life support system which, over the years, has led to the discovery of new evidence
and new insights. The paradox of the discovery of the Earth’s climate stabilization
system is that it came at a time when this system has almost disappeared. The
Earth’s regulation of the climate has been discovered when it has virtually
lost this regulatory influence. Over the last couple of million years, the Earth
has been losing the self-regulating capability it had over the previous couple
of aeons. It has certainly lost its primacy in controlling its own climate which
is being increasingly influenced by astronomic oscillations. The Earth is managing
to combat increasing solar radiation through what is in effect a fluke, the
fact that when the climate gets colder, more land appears in the tropics which
increases Photosynthesis thereby pushing the Earth further into an ice age.
Lovelock’s cutting edge scientific breakthrough is so new and so breath taking
and yet, seemingly, so redundant. The implications of this scientific revolution,
which provides a new perspective on the Earth, the climate, and life, have barely
begun to filter into politics or philosophy before it becomes necessary to develop
a post-gaian perspective.
Virtually all books on global burning begin with the statement that global
warming is a natural state of affairs without which global average temperatures
would be approximately 33C lower than they are now i.e. approximately -18C.
The intention of this comparison is to publicize the fundamental importance
of global warming so that humans will take more care of the environment and
ensure their survival. What this comparison entails, however, is comparing the
Earth’s current climate not to a possible planetary condition but to an entirely
imaginary one. No matter what humans might do, no matter what might happen to
the Earth, global warming would never disappear so that the Earth ends up freezing
like mars. Like other theoretical constructions designed to make a simple point,
this comparison gives rise to complications which are misleading and muddle
the message. This artificial comparison implies not merely that global warming
could disappear and that the Earth’s Biosphere could freeze to death, but that
global warming is a good thing in the sense that the warmer the Earth the less
likely is it that life on Earth will freeze to death. This slips over easily
into the common sense view that it doesn’t matter if humans exacerbate the greenhouse
effect because it is better to have excessive concentrations of greenhouse gases
keeping the Earth warm than declining concentrations so that we all froze to
death. This comparison hooks into the fear fostered by many science fiction
films - the cold of outer space. It gives emotional support to the common sense
view that humans are better off having a climate that is too hot rather than
allowing the cold of outer space to encroach too close to the surface of the
Earth. These political implications are the exact opposite of those the designers
of the abstract comparison wanted to make. Climatologists’ artificial comparison not merely gives rise to dangerous political
views, it ignores the basic facts about the Earth’s climate e.g. that there
has never been a time when global warming hasn’t existed on Earth and that it
is highly unlikely there ever will be such a time within the imaginable future.
It overlooks the fundamental trends of the Earth’s climate e.g. that over the
last few aeons the sun has been getting hotter and that the Earth would have
burnt up if Photosynthesis had not cooled the planet. Scientists’ artificial
comparison makes it far more difficult to explain the nature of the climate’s
current predicament and outline the policies needed - policies which are the
exact opposite of those implied by this comparison. It is imperative to compare the Earth’s current climate not with an artificial,
unreal, abstraction but with the Earth’s climate history: that since the formation of the Earth, solar radiation has been increasing
and that the biggest threat to the survival of life and the Biosphere is not
global freezing but global burning; that the role of life on Earth has been to cool the planet not to warm it up
and certainly not to encourage the planet to warm up because of an entirely
non-existent threat that without the greenhouse effect all life would freeze
to death; that when the Earth first formed, Carbon was so thick in the atmosphere it
would have absorbed huge amounts of solar energy and the atmosphere would have
been so heavy it would have crushed most of the life forms that later emerged
on Earth. The role of life is not pushing Carbon into the atmosphere but extracting
it from the atmosphere to keep the planet cool; that without life global temperatures would be 240-340C higher than they are
now and the Earth would be uninhabitable; and finally, that if humans destabilize the climate they will not cause the greenhouse effect
to disappear so that the planet lapses into a frozen ball - they will cause
the Earth to burn up as it attempts to return to its natural state. The Earth is naturally more like venus than it is mars. Over the last few aeons,
life has ensured the Earth is more like mars than venus. If humans want to stabilize
the climate and survive they have to recognize the planet needs to be more like
mars than venus. They have to fear venus not mars.
Life, or to be more accurate, Photosynthesis, has prevented the sun from boosting
global temperatures, by extracting Carbon from the atmosphere. In so doing it
has released oxygen into the atmosphere which has not merely provided a means
for new life forms to breathe but, much more fundamentally, retained water on
Earth which has meant that the oceans, clouds and ice sheets have helped to
lower the Earth’s temperature. The role of life in the history of the Earth
has been to reduce global temperatures. It is time that humans started acting
in accordance not with nature and the war of all against all, nor in terms of
a scientific fabrication inducing a fear of global freezing, but in harmony
with life’s aeons-long endeavour of cooling the Earth. That life has been able to stop the sun’s increasing solar radiation from burning
up the Earth is an extraordinary achievement. But then along comes a horde of
insufferably arrogant, stupid, eco-nazis without the slightest interest in the
planet they live on, without the slightest clue that they live on a living,
breathing, planet, and without the slightest understanding of the battles that
have been fought over the last three aeons to enable life to flourish on Earth.
They are not merely stupid, self-obsessed, and clueless, they resent having
to understand anything which might inhibit their greed from devastating the
planet.
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