... In short, if CM3's internal variability is realistic, there is some chance that a rapid underlying warming rate of 0.2 K decade − 1 could be ongoing as of 2015, but that this warming signal has been substantially masked (and may continue to be masked for even another decade or more)
by an internal variability cooling episode.
Not exact matches
However, satellite observations are notably
cooler in the lower troposphere than predicted
by climate models, and the research team in their paper acknowledge this, remarking: «One area of concern is that on average... simulations underestimate the observed lower stratospheric
cooling and overestimate tropospheric warming... These differences must be due to some combination of errors in model forcings, model response errors, residual observational inhomogeneities, and an unusual manifestation of natural
internal variability in the observations.»
We have warm El Ninos followed
by cooler La Ninas, the North Atlantic Oscillation, the Pacific Decadal Oscillation, the Julian Oscillation,... When we want to refer to them as a whole, we will call it «
internal variability.»
«The science of climate dynamics: continues to publish findings about solar / climate relationships and
internal variability of the climate system that invalidate the account of the Earth's climate dynamics presented
by the IPCC; predicts the likelihood of an extended period of global
cooling, if the emergent solar cycle 24 has a low amplitude, as seems increasingly likely on the basis of current science,» Mackey explained.
As you can see, over periods of a few decades, modeled
internal variability does not cause surface temperatures to change
by more than 0.3 °C, and over longer periods, such as the entire 20th Century, its transient warming and
cooling influences tend to average out, and
internal variability does not cause long - term temperature trends.
The 25 D - O events during the last glacial, where temperatures rose and fell
by 5 to 10 degrees C (10 - 15 degrees C for Greenland) within a span of decades that were «explained
by internal variability of the climate system alone ``, deemed global in scale, and they occurred without any changes in CO2 concentrations, which stayed steady at about 180 ppm throughout the warming and
cooling.
You write: «If
internal variability (such a a
cool PDO phase) reduces the rate of increase of surface temperature, while the e [x] ternal forcing still is increasing, this means the radiative imbalance is impeded from being cancelled
by surface warming.»
If
internal variability (such a a
cool PDO phase) reduces the rate of increase of surface temperature, while the eternal forcing still is increasing, this means the radiative imbalance is impeded from being cancelled
by surface warming.
Tett SFB et al., JGR 2002 (Estimation of natural and anthropogenic contributions to twentieth century temperature change,) says «Our analysis suggests that the early twentieth century warming can best be explained
by a combination of warming due to increases in greenhouse gases and natural forcing, some
cooling due to other anthropogenic forcings, and a substantial, but not implausible, contribution from
internal variability.
If you know what the forcings are and their magnitude, you can predict whether the climate will warm or
cool in the future and
by how much, excepting the effect of natural
variability (ie the
internal variability of the climate system).
They will refer to ENSO as showing «
internal variability»
by which they mean that ENSO can run warm at some times and
cool at others but that these temperatures must sum to zero, or approximately so, over longer periods of time.
In this letter, we propose that the extensive winter NH extratropical
cooling trend amidst a warming planet can not be explained entirely
by internal variability of the climate system.
«Modelling studies are also in moderately good agreement with observations during the first half of the 20th century when both anthropogenic and natural forcings are considered, although assessments of which forcings are important differ, with some studies finding that solar forcing is more important (Meehl et al., 2004) while other studies find that volcanic forcing (Broccoli et al., 2003) or
internal variability (Delworth and Knutson, 2000) could be more important... The mid-century
cooling that the model simulates in some regions is also observed, and is caused in the model
by regional negative surface forcing from organic and black carbon associated with biomass burning.