Not exact matches
Note that the old GISS model had a climate sensitivity that was a little higher (4.2 ºC for a doubling of CO2)
than the best estimate (~ 3ºC) and as stated in
previous years, the actual forcings that occurred are not the same as those used in the different
scenarios.
Assuming distributions of 0.5 percent, one finds that the after - tax return drops to 1.3 percent, which will turn the initial investment of $ 10,000 into $ 13,700 over 25
years — that's less
than 40 percent of the growth experienced by the low - cost, low - turnover investor in the
previous scenario.
These assumed that the largest decreases in rainfall would be in winter and spring (decreases of 5 % and 11 % between 1990 and 2030 on the low and high global warming
scenarios respectively), but rainfall was fractionally HIGHER in winter / spring in the more recent period (1995 - 2006)
than in the
previous 11 -
year period.
Both wetland drying and the increased frequency of warm dry summers and associated thunderstorms have led to more large fires in the last ten
years than in any decade since record - keeping began in the 1940s.9 In Alaskan tundra, which was too cold and wet to support extensive fires for approximately the last 5,000
years, 105 a single large fire in 2007 released as much carbon to the atmosphere as had been absorbed by the entire circumpolar Arctic tundra during the
previous quarter - century.106 Even if climate warming were curtailed by reducing heat - trapping gas (also known as greenhouse gas) emissions (as in the B1
scenario), the annual area burned in Alaska is projected to double by mid-century and to triple by the end of the century, 107 thus fostering increased emissions of heat - trapping gases, higher temperatures, and increased fires.
The ozone losses predicted in the study are much larger
than losses estimated in
previous «nuclear winter» and «ultraviolet spring»
scenario calculations following nuclear conflicts -LSB-...] A 1985 National Research Council Report predicted a global nuclear exchange involving thousands of megatons of explosions, rather
than the 1.5 megatons assumed in the PNAS study, would deplete only 17 percent of the Northern Hemisphere's stratospheric ozone, which would recover by half in three
years.