Not exact matches
... The Earth's atmospheric methane concentration has
increased by about 150 % since 1750, and it
accounts for 20 % of the total radiative forcing from all of the long - lived and globally mixed greenhouse gases (these gases don't include
water vapor which is by far the largest component of the greenhouse effect).
Second, you have to
account for the energy cost of separating out
water vapor, which would probably substantially
increase the actual amount of LN2 needed.
(before
accounting for
increased water vapor), but with the greater warming at upper levels,... etc..
Since the CO2 forcing can
account for much of 0.6 C
increase, how do we know «instant» positive feedbacks like
water vapor will overwhelm negative feedbacks before slightly longer timescale feedbacks have a chance to kick in?
Because rising greenhouse gas emissions
account for all or part of the
water vapor increase, it is likely to continue for many decades.