«By merging the ESA Climate Change Initiative's data with NASA's, we clearly see
negative ozone trends in the upper atmosphere before 1997 and positive trends after,» concludes Viktoria Sofieva, Senior Research Scientist at the Finnish Meteorological Institute.
Not exact matches
During the period of summer
ozone recovery (2000 — 2050), the SAM index exhibits weakly
negative, statistically insignificant
trends due to stratospheric
ozone recovery which offsets the positive forcing imposed by increasing GHG concentrations.
«Here, it is sufficient to note that many of the 20CEN / A1B simulations neglect
negative forcings arising from stratospheric
ozone depletion, volcanic dust, and indirect aerosol effects on clouds... It is likely that omission of these
negative forcings contributes to the positive bias in the model average TLT
trends in Figure 6F.
The observed positive height
trends over the continent may be indicative of a thermal response to greenhouse gas increases (Neff et al. 2008), counteracting the
negative height
trends associated with
ozone depletion and the dynamical response to greenhouse gas increases (Arblaster and Meehl 2006).
Recent changes in the location of maximum spring stratospheric
ozone depletion (Evtushevsky et al. 2008) may also be contributing to the
negative geopotential height
trends in the South Pacific sector and to the east — west asymmetry of Antarctic climate change.