Role of stratospheric aerosols in antagonizing the Climate Global Warming

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Role of stratospheric aerosols in antagonizing
the Climate Global Warming

• Academician Yu.A.Izrael,Director of the
  Institute of Global Climate and Ecology, Moscow

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Radiative Forcing Components
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Mon-Pele, et al. (1902 ?.)
S ()
120
100
80
60
40
20
0
1902 1903
1904
1905
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Direct solar radiation Katmai (1912 ?.)
S ()
120
100
80
60
40
20
0
1911 1912
1913
1914
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Direct
Diffuse
1982 El-Chichon
1992 Pinatubo
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Severe and catastrophic volcanic cruptions in
the 18th20th centuries
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Variation of (a) the tree-ring index () at the
northern boundary of forest in the Northern
Hemisphere and (b) electric conductivity (µ-equiv
H/kg of ice) of the ice core from the Crete
glacier (Greenland)
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Numerical computation of Es from Eq. (2) within
the wavelength range 0.3 m 2.5 m for
particles with different radii gives the maximal
value of average intensity of the flux into space
to be 5.23 W/m2 for a particle with radius 0.275
m.
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Pinatubo (1991). McCormick et al., 1995
RadIatIve forcIng
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Puttern Pinatubo (1991). (McCormick et
al.,1995).
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SO2
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1. The method, proposed in this note, is
essentially operational (expeditious) and it is
in tens-hundreds times cheaper that measures
proposed by the Kyoto method for achieving the
objectives discussed. For a reference this
method was proposed by Russian scientist
academician M.I. Budyko in 1974, then it was
developed and updated by myself Izrael, 2005 in
connection with extreme necessity to struggle for
conservation of the present-day climate. It was
published in 2005 Izrael Yu.A. Russian
Meteorology and Hydrology, and later on in my
report at the International Conference in Moscow
of 2006 Izrael et al.,. The problem of such
method was raised by the Nobel Prize winner,
professor Paul Krutzen in his publication of
2006. It was earlier discussed in common view by
outstanding American specialist Edvard Teller.
2. Taking into account a low efficiency of the
Kyoto Protocol and significant quantity of both
the time and funding for its realization, it is
necessary to develop non-kyoto methods for
conservation of our climate and for struggle
against the warming. 3. Some methods those
are already published, such as using nuclear
energy and energy of renewable resources in the
power industry instead of organic fuel where
significant time (tens and hundreds of years)
together with huge funds will be needed for their
efficient use (that is for sufficient provision
of the humanity needs).
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REFERENCES

• M. I. Budyko, Climate Change (Gidrometeoizdat,
  Leningrad, 1974) in Russian.
• Climate Change 2001 Synthesis Report of the
  Intergovernmental Panel on Climate Change, Ed. by
  R.T. Watson et al. (WMO, Geneva, 2003).
• Yu. A. Izrael, Ecological Consequences of a
  Possible Nuclear War, Meteorologiya i
  Gidrologiya, No. 10 (1983) Russian Meteorology
  and Hydrology, No. 10 (1983).
• Yu. A. Izrael, An Efficient Way to Regulate
  Global Climate is the Main Objective of the
  Solution of the Climate Problem, Meteorologiya i
  Gidrologiya, No. 10 (2005) Russian Meteorology
  and Hydrology, No. 10 (2005).
• Yu. A. Izrael, I. I. Borzenkova, and D. A.
  Severov, The Role of Stratospheric Aerosols in
  the Maintenance of the Present-Day Climate, in
  Proceedings of the International Conference on
  the Problems of Hydrometeorological Safety,
  September 2629, 2006, Moscow (Roshydromet,
  Moscow, 2006).
• Yu. A. Izrael and S. M. Semenov, Calculation of
  a Change in CO2 Concentration in the Atmosphere
  for Some Stabilization Scenarios of Global
  Emissions Using a Model of Minimal Complexity,
  Meteorologiya I Gidrologiya, No. 1 (2005)
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  (2005).
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