Kay added that «the fate of sea ice over the next decade depends not only on human activity but
also on climate variability that can not be predicted.»
Even though the observed ice loss has accelerated over the last decade, the fate of sea ice over the next decade depends not only on human activity but
also on climate variability that can not be predicted.
Not exact matches
«Regional changes are mostly due to natural
variability but
on top of that we see this pronounced overall weakening in summer storm activity,» says co-author Dim Coumou, «This is
also something projected by
climate models under future emission scenarios.
«A lot of the year - to - year
variability is for all practical purposes random and unpredictable,» said Sobel, who
also directs a new Columbia University Initiative
on Extreme Weather and
Climate.
So for this extended period in the evolution of life
on this planet, we are only very recently plunging, arguably at an accelerating rate, into previously not experienced degrees of cooling and
also probably into new extremes of rapid
climate variability.
Then we
also analyzed major
climate forcings that act
on the
variability of heat waves.
The research is particularly relevant given the expectation that
on top of an overall warming trend,
variability in key parts of the
climate system could
also grow in the future.
So for this extended period in the evolution of life
on this planet, we are only very recently plunging, arguably at an accelerating rate, into previously not experienced degrees of cooling and
also probably into new extremes of rapid
climate variability.
Based
on the comparison between reconstructions and simulations, there is high confidence that not only external orbital, solar and volcanic forcing, but
also internal
variability, contributed substantially to the spatial pattern and timing of surface temperature changes between the Medieval
Climate Anomaly and the Little Ice Age (1450 to 1850).
Also your inability to see that natural
variability occurs
on climate path based
on the radiative forcing illustrates your basic misunderstanding of these realities.
The solutions, however, must
also include a much better focus than present
on climate change adaptation and reducing vulnerability to drought — a «no - regrets» strategy that will help both with natural
variability, and the
variability that could be made more challenging by human - caused
climate change.
In principle, changes in
climate on a wide range of timescales can
also arise from variations within the
climate system due to, for example, interactions between the oceans and the atmosphere; in this document, this is referred to as «internal
climate variability».
She will
also investigate the combined affects of natural
variability and increased greenhouse forcings
on changes in
climate extremes throughout the 21st Century.
But their PNAS publication
also referred to natural
climate cycles, superimposed
on the trend line, like ENSO and solar
variability, both of which have been net contributors to global cooling over 1998 - 2008 [so
climate skeptics can not — as they still do — point to either the Sun or El Niño to explain the world's temperature graph over that period of time].
It is
also important to note that the models are not designed to project
climate on a decadal basis, but
on a centennial basis, where the effects of internal
variability can more reasonably be expected to average out.
They
also took account of natural factors such as volcanic eruptions and
climate variability to gauge the impact of human activity
on the amount of monsoon rainfall.
The influence of large - scale
climate modes of
variability (the Pacific Decadal Oscillation (PDO) and the El Niño - Southern Oscillation (ENSO)-RRB-
on APF magnitude is
also assessed, and placed in context with these more localized controls.
Although the NAO is the dominant pattern of atmospheric circulation
variability, accounting for about half of the total winter SLP variance
on both interannual and multi-decadal time scales, other large - scale structures of internal circulation
variability will
also undoubtedly contribute to uncertainty in future
climate trends.
The fact that unforced
variability in the
climate system can offset anthropogenic forcing changes
on a time scale of about 15 years and smaller does not logically imply that unforced
variability is
also the primary cause of the statistically significant temperature increase since the mid 1970ies.
«The authors write that North Pacific Decadal
Variability (NPDV) «is a key component in predictability studies of both regional and global
climate change,»... they emphasize that given the links between both the PDO and the NPGO with global
climate, the accurate characterization and the degree of predictability of these two modes in coupled
climate models is an important «open question in
climate dynamics» that needs to be addressed... report that model - derived «temporal and spatial statistics of the North Pacific Ocean modes exhibit significant discrepancies from observations in their twentieth - century
climate... conclude that «for implications
on future
climate change, the coupled
climate models show no consensus
on projected future changes in frequency of either the first or second leading pattern of North Pacific SST anomalies,» and they say that «the lack of a consensus in changes in either mode
also affects confidence in projected changes in the overlying atmospheric circulation.»»
It is
also defined by the United Nations Convention
on Climate Change as «change of climate which is attributed directly or indirectly to human activity that alters the composition of the global atmosphere and which is in addition to natural climate variability observed over comparable time periods
Climate Change as «change of
climate which is attributed directly or indirectly to human activity that alters the composition of the global atmosphere and which is in addition to natural climate variability observed over comparable time periods
climate which is attributed directly or indirectly to human activity that alters the composition of the global atmosphere and which is in addition to natural
climate variability observed over comparable time periods
climate variability observed over comparable time periods»
Russ R. - You did, I assume,
also note the uncertainties
on natural forcings and
on internal
climate variability?
As I will show later
on virtually all
climate variability is a result of internal system
variability and additionally the system not only sets up a large amount of
variability internally but
also provides mechanisms to limit and then reduce that internal
variability.
DelSole et al. (28)
also found 2.5 cycles by extracting the spatial pattern in the Intergovernmental Panel
on Climate Change, Fourth Assessment Report (IPCC AR4)(29) model control runs that best characterizes internal
variability and by projecting the observed global data onto this pattern.
It is
also responsible for the official reporting of observed
climate variability and change in Australia and
on collaboration with international agencies.
This assumption has been questioned
on the basis of both observational and model - simulated data suggesting that tropical to extratropical
climate variability can be decoupled (Rind et al., 2005), and
also that extratropical teleconnections associated with ENSO may vary through time (see Section 6.5.6).
If verified, this effect would represent a dramatic advance not only in the basic understanding of the Sun's variable activity, but
also in the potential influence of this
variability on the Earth's
climate.