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ŠUMARSKI LIST 9-10/1998 str. 61     <-- 61 -->        PDF

T. Dimitrov: GORENJE GLOBALNE BIOMASE Šumarski list br. 9 10, CXX1I (1998), 443-455
University of Buenos Aires, Argentina. NapoStocks,
B. J., M. A. Fosberg, T.,J.,.Ly nham, L.
mena: Citirana literatura pod fusnotom (1), naMearns
, B. M. Wotton , Q., Jang, J-Z. Jin ,
vedena je u gorecitiranom radu. K. Lawrence, G. R. Hartley, J. A. Mason and


D. W. McKenney: 1998, Climate Change and
S imard , A.: 1997, Towards Criteria and Indicators for


Forest Fire Potential in Russian and Canadian


Wildland Fire: A Canadian Example, 2nd


Boreal Forests, Climate Change 38: 1-13.


International. Wildland Fire Conference ´97,


Napomena: Citirana literatura pod fusnotom (3),


Conference papers, May 25-30, 1997, Vancou


navedena je u gorecitiranom radu.


ver, B.C., Canada.
Velez , R.: 1997, FAO Silva Mediterranean Forest Fi


Stocks , B.J.: 1996, The Extent and Impact of Forest


re Network, 2nd International Wildland Fire


Fires in Northern Circumpolar Countries, edited


Conference ´97, Conference papers, May 25-30,


by Joel S. Levine, Vols. 1&2, the MIT Press,


1997, Vancouver, B.C., Canada.


Cambridge, Mass. & London, England. Napomena:
Citirana literatura pod fusnotom (2), navedena
je u gorecitiranom radu.


SUMMARY: In this paper the most recent research on forest fires made by
renown scientists in the world are presented, where the climate change and its
implications on forest fire, fire emissions and their impact on the atmosphere,
catastrophic situation predictions on the global level caused by biomass burning
particularly in Tropics, and on the Protocol of the International
Conference on the climate change, held in Kyoto, Japan, are analyzed.


There is very important research B. J. Sto cks and others on the climate
change and forest fire potential in Russian and Canadian boreal forests by
simulating through current general circulation models scenario of doubled
CO2 (2 x CO2) and its implications on the fire weather severity increase, extending
the fire season by warming up of struck regions and shifting forest vegetation
northward.