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Role of gas and aerosol components of the atmosphere in the model of greenhouse explosion

Abstract

Within the model of an equivalent grey atmosphere, the analysis of different mechanisms of negative feedback in the heat balance of the Earth’s surface, forming the stability of its current temperature regime and the only positive feedback mechanism which is able to lead to stability loss and transition to more hot condition, as on Venus, has been carried out. The role of the main greenhouse gases such as CO2, H2O, CH4, and cloudy aerosol in the positive feedback mechanism, as well as evaporation, photosynthesis, and cloud cover in the negative feedback mechanism have been characterized. The criticality of the heat balance in relation to the growth rate of the planetary albedo with an increase in the temperature of the Earth’s surface has been elicited. Above the Earth’s surface, the current state can be the only stationary and globally stable one in the temperature range of >288 K.

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Correspondence to V. I. Zakharov.

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Original Russian Text © V.I. Zakharov, K.G. Gribanov, S.A. Beresnev, 2009, published in Optika Atmosfery i Okeana.

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Zakharov, V.I., Gribanov, K.G. & Beresnev, S.A. Role of gas and aerosol components of the atmosphere in the model of greenhouse explosion. Atmos Ocean Opt 22, 162–172 (2009). https://doi.org/10.1134/S1024856009020055

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Keywords

  • Heat Balance
  • Optical Thickness
  • Greenhouse Effect
  • Methane Hydrate
  • Surface Temperature Increase