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<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics Discussions</journal_title>
		<journal_url>www.atmos-chem-phys-discuss.net</journal_url>
		<issn>1680-7367</issn>
		<eissn>1680-7375</eissn>
		<volume_number>2</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2002</publication_year>
	</journal>
	<doi>10.5194/acpd-2-289-2002</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/2/289/2002/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/2/289/2002/acpd-2-289-2002.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/2/289/2002/acpd-2-289-2002.pdf</fulltext_pdf>
	<start_page>289</start_page>
	<end_page>337</end_page>
	<publication_date>2002-03-08</publication_date>
	<article_title content_type="html">Greenhouse effect dependence on atmospheric concentrations of greenhouse substances and the nature of climate stability on Earth</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>V. G. Gorshkov</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>A. M. Makarieva</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Petersburg Nuclear Physics Institute, 188300, Gatchina, St.-Petersburg, Russia</affiliation>
	</affiliations>
	<abstract content_type="html">Due to the exponential positive feedback between sea surface temperature and
      saturated water vapour concentration, dependence of the planetary greenhouse
      effect on atmospheric water content is critical for stability of a climate
      with extensive liquid hydrosphere.&lt;br&gt;
      &lt;br&gt;
      In this paper on the basis of the law of energy conservation we develop a simple physically transparent approach to description of radiative transfer
      in an atmosphere containing greenhouse substances. It is shown that the analytical solution of the equation thus derived coincides with the exact
      solution of the well-known radiative transfer equation to the accuracy of
      20% for all values of atmospheric optical depth. The derived equation makes it possible to easily take into account the
      non-radiative thermal fluxes (convection and latent heat) and obtain an analytical dependence of
      the greenhouse effect on atmospheric concentrations of a set of greenhouse
      substances with arbitrary absorption intervals.&lt;br&gt;
      &lt;br&gt;
      The established dependence is used to analyse stability of the modern climate of Earth. It is shown that the modern value of global mean surface
      temperature, which corresponds to the liquid state of the terrestrial hydrosphere, is physically unstable. The observed stability of modern
      climate over geological timescales is therefore likely to be due to dynamic
      singularities in the physical temperature-dependent behaviour of the greenhouse effect. We hypothesise that such singularities may appear due to
      controlling functioning of the natural global biota and discuss major arguments in support of this conclusion.</abstract>
	<references>
	</references>
</article>

