The team then compared the oxygen isotope ratio for each year's wet season from 1990 to 2010 with a cyclone activity index of
the average accumulated energy expended, based on factors such as number of cyclones, cyclone strength, size and time on storm track.
Not exact matches
The
Accumulated Cyclone
Energy (ACE) index of tropical cyclone activity also indicated a below -
average season in the North Atlantic.
«We use a massive ensemble of the Bern2.5 D climate model of intermediate complexity, driven by bottom - up estimates of historic radiative forcing F, and constrained by a set of observations of the surface warming T since 1850 and heat uptake Q since the 1950s... Between 1850 and 2010, the climate system
accumulated a total net forcing
energy of 140 x 1022 J with a 5 - 95 % uncertainty range of 95 - 197 x 1022 J, corresponding to an
average net radiative forcing of roughly 0.54 (0.36 - 0.76) Wm - 2.»
Thus, as more
energy accumulates in the lower - troposphere
averaged over the whole planet, we would expect the temperatures of the near - surface troposphere to increase.
«We use a massive ensemble of the Bern2.5 D climate model of intermediate complexity, driven by bottom - up estimates of historic radiative forcing F, and constrained by a set of observations of the surface warming T since 1850 and heat uptake Q since the 1950s... Between 1850 and 2010, the climate system
accumulated a total net forcing
energy of 140 x 1022 J with a 5 - 95 % uncertainty range of 95 - 197 x 1022 J, corresponding to an
average net radiative forcing of roughly 0.54 (0.36 - 0.76) Wm - 2.»