Although earlier data are less complete, the observations also suggest that stratospheric water contributed to
enhancing the warming observed during 1980 — 2000.
Not exact matches
Moreover if the natural forcing since 1950 should be slightly negative, an
enhanced natural forcing would mean that anthropogenic forcing must be greater than expected to explain the
observed warming.
Moreover if the natural forcing since 1950 should be slightly negative, an
enhanced natural forcing would mean that anthropogenic forcing must be greater than expected to explain the
observed warming.
Utterly wrong: the computer climate models on which predictions of rapid
warming from
enhanced atmospheric greenhouse gas concentration cowdungare based «run hot,» simulating two to three times the
warming actually
observed over relevant periods
First, the computer climate models on which predictions of rapid
warming from
enhanced atmospheric greenhouse gas concentration are based «run hot,» simulating two to three times the
warming actually
observed over relevant periods — during which non-anthropogenic causes probably accounted for some and could have accounted for all the
observed warming — and therefore provide no rational basis for predicting future GAT.
Arctic low cloud changes as
observed by MISR and CALIOP: Implication for the
enhanced autumnal
warming and sea ice loss
Wu, D. L., and J. N. Lee, 2012: Arctic low cloud changes as
observed by MISR and CALIOP: Implication for the
enhanced autumnal
warming and sea ice loss.
To quote Karl Braganza from the Bureau as published by that online rag The Conversation, «Patterns of temperature change that are uniquely associated with the
enhanced greenhouse effect, and which have been
observed in the real world include... Greater
warming in winter compared with summer... Greater
warming of night time temperatures than daytime temperatures».
Note that the residual from a proxy - based global reconstruction is much smaller (Crowley et al., 2014), raising questions if the strong bias of
observed data toward the Atlantic sector
enhances the residual
warming.
Northward atmospheric winter fluxes are
observed after the
enhanced global
warming after 1970, and, for the first time over the period considered, a positive correlation is
observed between atmospheric and oceanic reducing effects on the ice extent.