Light gray bars denote deglaciations (terminations), while the two dark gray bars denote the Younger Dryas and the Younger Dryas - like event during termination III (i.e.,
decreased atmospheric methane and East Asian Monsoon (higher δ18O).
Not exact matches
Near Titan's surface, about 5 percent of the
atmospheric molecules are
methane, the fraction
decreasing with altitude.
We find that the global
methane hydrate inventory
decreases by approximately 70 % (35 %) under four times (twice) the
atmospheric CO2 concentration and is accompanied by significant global oxygen depletion on a timescale of thousands of years.
The effect of this increase on the growth rate of
atmospheric methane has been masked by a coincident
decrease in wetland emissions, but
atmospheric methane levels may increase in the near future if wetland emissions return to their mean 1990s levels.
On longer timescales, our results show that the
decrease in
atmospheric methane growth during the 1990s was caused by a decline in anthropogenic emissions.
The discovery in ice core records that
atmospheric concentrations of two potent greenhouse gases, carbon dioxide and
methane, have
decreased during past glacial periods and peaked during interglacials indicates important feedback processes in the Earth system.