However, England is talking about the yearly to decadal variations in surface temperature which are strongly
dominated by internal variability due to an unevenly heated, water - covered planet.
As far as there being a «guarantee», all I can say is that I personally have no idea on how to create a consistent model
dominated by internal variability — ie., a model with low climate sensitivity, a trend pattern similar to observations, and a positive heat uptake — as I tried to outline in this post.
In any case, it is good to have a list of what you have to question if, in particular, you want to argue that the warming in the past half - century has been
dominated by internal variability.
Not exact matches
The results indicate that naturally induced climate variations seem to be
dominated by two
internal variability modes of the ocean — atmosphere system: AMO and El Niño Southern Oscillation
So when you say; «Will the climate of the 21st century be
dominated by anthropogenic warming (green) or natural
variability (solar, volcanoes, natural
internal oscillations)?
I have a problem with your question: Will the climate of the 21st century will be
dominated by anthropogenic warming (green) or natural
variability (solar, volcanoes, natural
internal oscillations)?
Will the climate of the 21st century will be
dominated by anthropogenic warming (green) or natural
variability (solar, volcanoes, natural
internal oscillations)?
In reality, and as I keep pointing out,
internal climate
variability dominated by movements of ocean water is alone sufficient to explain ALL recent global climate variation.
The simulated sea surface temperature
variability from two global coupled climate models for the second half of the 20th century is
dominated by natural
internal variability associated with the Antarctic Oscillation, suggesting that the models»
internal variability is too strong, leading to a response to anthropogenic forcing that is too weak.
Local climate variations can be
dominated by internal climate
variability, often the result of the redistribution of heat
by regional climate processes.