M2009 use a simplified carbon cycle and climate model to make a large ensemble of simulations in which principal uncertainties in the carbon cycle, radiative forcings, and climate response are allowed to vary, thus yielding a probability distribution for global
warming as a function of time throughout the 21st century.
M2009 use a simplified carbon cycle and climate model to make a large ensemble of simulations in which principal uncertainties in the carbon cycle, radiative forcings, and climate response are allowed to vary, thus yielding a probability distribution for global
warming as a function of time throughout the 21st century.
Not exact matches
We have plotted most likely peak temperatures
as a
function of four different cumulative emission metrics: year 1750 — 2500 (figure 3a), year 1750 to the
time at which peak
warming occurs (figure 3b), year 1750 — 2100 (figure 3c) and year 1750 — 2200 (figure 3d).
Figure 15 - A has shown the global pacing by the El Niños (and their tele - connections)
of the temperature changes
of the lower troposphere
as function of both
time and latitude; this pacing may be due to the coming to the surface, at high latitudes,
of warm water from the Pacific
warm pool,
as they move to higher latitudes on the western rim
of the oceans after an El Niño.
The national total annual impact
of climate change expressed in welfare - equivalent income change for a 2.5 ˚C global
warming (relative to pre-industrial
times)
as a
function of per capita income (top panel) and temperature (bottom panel).