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<article>
 <update>2008.10.26</update>
 <newsletter number="61" />
 <topic link="../topics/greenhouse.html">Greenhouse</topic>
 <title>Climate science - an introduction</title>
 <author>Sophia van Ruth</author>
 <date>2008.5</date>
 <author_note>Sophia is MSc Holistic Science student, Schumacher College, UK. At the time of publishing, Sophia was a UEA Board member - participating in UEA meetings through Skype.
 </author_note>
 <summary>As human activities are currently emitting excessive levels of carbon dioxide into the atmosphere, it is fast becoming a very real possibility that the system will not be able to regulate carbon dioxide well enough anymore to maintain liveable global temperatures.
 </summary>
 
 <entry id="gaiatheory">
  <title>Gaia theory</title>
  <p>Gaia theory, proposed by James Lovelock, broadly proposes 
    that life on the planet could be considered to operate as 
    one organism (named Gaia). Like other organisms, Gaia 
    regulates conditions to keep them favourable to her own 
    existence. Atmospheric gas concentrations, temperature 
    and ocean salinity are all tightly regulated and kept within 
    the bounds that support the living beings of Gaia.
  </p>
  <p>This is 
    more remarkable than it may seem at first glance. If we 
    take atmospheric gases as an example, the concentration 
    of oxygen in the air is kept at approximately 21%. <q>So what</q> 
    you may say. But oxygen is a highly reactive gas which 
    rapidly combines with other elements, making it utterly 
    remarkable for the level to remain constant at 21% - which it 
    has for around 300 million years! 
  </p>
  <p>This provides evidence of a complex regulatory system 
    maintaining what in the human organism is called 
    homeostasis. The mechanisms by which this kind of 
    regulation occurs are not fully understood as there are so 
    many different interactions and relationships on the planet 
    that combine to bring about such stability. However, some 
    of the interactions have been identified, and looking at one 
    such group of interactions may help build an appreciation of 
    the kind of dynamics that maintain life as we know it.
  </p>
 </entry>
 
 <entry id="carboncycle">
  <title>Carbon Cycle</title>
  <p>The relationships governing the regulation of the carbon 
    cycle seem a good example to choose, as Gaia's balance 
    of carbon is becoming dangerously disturbed and carbon 
    dioxide levels are affecting global temperature. There is 
    more than one web of relationships that regulates carbon 
    dioxide levels in the atmosphere, the one represented in the 
    diagram below is known as the long term carbon cycle, as it 
    takes a long time for carbon to travel through the processes 
    involved.
  </p>
  <p>
   <image text="carbon flow diagram" source="images/climatescienceintroduction/carbonflowdiagram.jpg" width="409" height="290" />
  </p>
  <p>Taken from Stephan Harding's book <cite>Animate Earth</cite> p115
  </p>
  <p>Arrows with solid lines represent <q>direct couplings</q>. If we take 
    the arrow from temperature to plant growth as an example, 
    this means that if the temperature rises, so does the amount 
    of plant growth. Conversely, if the temperature decreases, so does the amount
    of plant growth. Arrows with dashed 
    lines indicate an <q>inverse coupling</q>.
  </p>
  <p>This time we'll use
    the example of the arrow from silicate rock weathering to 
    carbon dioxide in the atmosphere. 
  </p>
  <p>Silicate rock weathering 
      is a process in which granite and basalt rocks react 
      chemically with carbon dioxide and water. One of the 
      outcomes of this reaction is the removal of carbon dioxide 
      from the air. Plants enhance this process greatly. </p>
  <p>Plants 
   break up rocks with their roots, increasing the surface 
   area available to react with the water and carbon dioxide. They also
   release carbon dioxide from their roots, adding to the ingredients necessary
   for rock weathering (Other living beings also assist silicate rock weathering. 
   Worms, lice, nematodes, millipedes etc. all break up soil and allow 
   water to penetrate. Microbes secrete substances that break 
   up rocks and also produce carbon dioxide).
  </p>
  <p>The inverse 
    coupling in the diagram below indicates that if the amount 
    of rock weathering increases then the amount of carbon 
    dioxide will decrease. Conversely, if the amount of rock 
    weathering decreases, the amount of carbon dioxide will 
    increase. There are actually many processes represented 
    on this one diagram, taking just one <q>feedback loop</q> as an 
    example we can look at:
  </p>
  <p>
   <image text="carbon feedback negative" source="images/climatescienceintroduction/carbonfeedbacknegative.jpg" width="365" height="245" />
  </p>
  <p>If you imagine carbon dioxide being released into the 
  atmosphere and run this feedback circuit in your head, 
  you'll see that it triggers processes that bring carbon 
  dioxide levels back down again. This is known as a negative 
  feedback loop (negative to change) and is one of the ways 
  the gases in the atmosphere are kept at constant levels.
  </p>
  <p>However, taking this further, if too much carbon dioxide 
    enters the atmosphere and the temperature rises too 
    much, it will not provide an environment favourable to 
    plant growth and plants will start to die, changing the 
    temperature/plant link to an <q>inverse coupling</q> as follows:
  </p>
  <p>
   <image text="carbon feedback positive" source="images/climatescienceintroduction/carbonfeedbackpositive.jpg" width="423" height="294" />
  </p>
  <p>If you follow this circuit in your mind you will see that it is a 
  vicious circle and will lead to temperature spiralling out of 
  control. This is known as a positive feedback loop.
  </p>
  <p>Luckily such feedback loops as we just explored do not 
    exist in isolation, but the more positive loops that manifest 
    within a system, the more pressure is put on the negative ones. There may come
    a time where the negative loops 
    left in the system cannot resist changes on the Gaian level 
    anymore. Once this happens, large scale change might 
    occur quite quickly, with a similar quality to the <q>phase 
    transition</q> or sudden change in order described for the ant 
    colonies above.
  </p>
   <p>As human activities are currently emitting 
      excessive levels of carbon dioxide into the atmosphere, it is 
      fast becoming a very real possibility that the system will not 
      be able to regulate carbon dioxide well enough anymore to 
      maintain liveable global temperatures. 
   </p>
 </entry>
 
 <entry id="transition">
  <title>Transition</title>
   <p>Within the time humans have been on the planet, Gaia has 
      been in a relatively stable state (appearing homeostatic).
      However, history reveals that, ultimately, Gaia is more 
    homeorhetic than homeostatic. Homeorhesis is a term 
    coined by C H Waddington, and relates to transitions from 
    one stable state to another. In Waddington's definition 
    a human too is homeorhetic, especially as the person is 
    growing. This term relates to being able to make changes 
    to an organism (like the growing form changing) whilst 
    keeping other things the same (like the concentrations 
    of chemicals in the bloodstream). Waddington describes 
    homeorhesis as <q>preserving a flow</q>.
   </p>
 </entry>
 
 <entry id="oscillation">
   <title>Oscillation</title>
   <p>Actually, Gaia has oscillated between hot and cold climatic 
  states throughout her existence, Lovelock even speculates 
  that glacial, cold states seem the more stable and healthy 
  state of the two, with warmer states (interglacials) being 
  shorter lived and possibly comparable to running a fever 
  in humans. It is in an interglacial period that we find 
  ourselves now. 
  </p>
 </entry>
 
 <entry id="extinctions">
  <title>Mass Extinctions</title>
  <p>
  There have also been numerous previous 
  mass extinctions on earth, changing the <q>players</q> in the 
  living biosphere profoundly.
   </p>
   <p>One of the most startling and sobering of these was what 
    Lynn Margulis and Dorian Sagan have dubbed the <q>oxygen 
    holocaust</q> and describe as a <q>worldwide pollution crisis 
    that occurred about 2000 million years ago</q>. Before this 
    time there was very little oxygen in the atmosphere, until 
    the microbes alive at this time discovered a new way to 
    get the hydrogen that they needed out of water by using 
    a new form of photosynthesis. The oxygen left over from 
    this process was released into the atmosphere.
   </p>
   <p>Oxygen 
      is toxic to many microbes and the very microbes releasing 
      the oxygen were threatened severely by it as it started to 
      build up (Sound familiar? Carbon dioxide threatens the very 
      beings responsible for its emission now).
   </p>
   <p>However, although this has been described as a mass 
  holocaust, there was a remarkable creative evolution amongst the microbes that
  survived. They learned to utilise the toxin threatening 
    them as a resource (inventing respiration). This 
    created such rich new opportunities that life 
    on earth eventually moved into a new phase 
  of abundance.
   </p>
 </entry>
 
 <entry id="conclusion">
   <title>Conclusion</title>
   <p>Gaia seems perfectly capable 
    of changing the goalposts and 
    establishing a new world order when 
    pushed.
   </p>
 </entry>
 
 <entry id="bibliography">
   <title>Bibliography</title>
   <p>Stephan Harding, <cite>Animate Earth</cite>, Green Books, 2006 
    James Lovelock,<cite>The Ages of Gaia</cite>, Oxford University Press, 
    1988
   </p>
   <p>James Lovelock, <cite>Gaia, Medicine for an Ailing Planet</cite>, Gaia 
    Books, 2005
   </p>
   <p>James Lovelock, <cite>The Revenge of Gaia</cite>, Penguin Books, 
    2006
   </p>
   <p>Lynn Margulis and Dorian Sagan, <cite>Microcosmos</cite>, 
    Touchstone, 1986
   </p>
   <p>Lynn Margulis and Michael F. Dolan, <cite>Early Life: Evolution on 
    the Precambrian Earth</cite>, Jones and Bartlett, 2002
   </p>
   <p>Fritjof Capra, <cite>The Web of Life</cite>, Flamingo, 1997
   </p> 
   <p>C H Waddington, <cite>Tools for Thought</cite>, Granada Publishing, 
    1977
   </p>
 </entry>
 <entry id="comments">
  <title>Comments</title>
  <p>Sophia's closing comment does perhaps leave some room 
    for hope! - Joan</p>
 </entry>

</article>
