Of these proxies, some of the most useful for long -
term climate analyses are ice cores, sediment cores, tree rings and, of course, the fossil record.
Not exact matches
In the
analysis — this was [all] originally published as a scientific paper in Nature last fall and then we see it again here in Scientific American in a more a distilled form — what we show is that in
terms of
climate change, in
terms of nitrogen pollution into our waterways and oceans, and in
terms of biodiversity loss, we have already caused irreparable harm to the planet.
One of the major problems, as Latif explained, is that there are just very few long -
term oceanic measurements, thereby complicating the
analysis and interpretation of
climate change signals.
«We need both, realistic model simulations and long -
term data records, and really sophisticated
analysis methods to produce reliable
climate predictions.
According to McFadden, not only does this
analysis demonstrate that wintertime
climate can be important for northern cities, it also shows the effects in
terms of flood risks.
A new
analysis of global energy use, economics and the
climate shows that without new
climate policies, expanding the current bounty of inexpensive natural gas alone would not slow the growth of global greenhouse gas emissions worldwide over the long
term, according to a study appearing today in Nature.
On the whole, in
terms of magnitudes of risks that we used in our
analysis [in the Stern Review Report on the Economics of
Climate Change for the U.K. government], my best guess is that we underestimated them.
Their
analysis of ring width, published in today's Nature, revealed a number of long - and short -
term climate cycles with different periods.
However, the city needs to be planning for those types of huge barriers more as part of a longer -
term plan, and as preparation for the possibility that
climate change and sea - level rise may be worse than expected, warns the
analysis, published last week in Science.
Finally, a broader
analysis of the environmental variables in the aggregation sites can inform the long -
term impacts of
climate change in the movement of the whale sharks.
After a short in - service with a colleague early in
Term 1, I used the temperature probes and the
analysis software in a short
Climate Change investigation.
re: # 34 John Philips As it happens, in the near future, you may want to revisit the Wegman Report... — For example, Wegman & co were so expert at Social Network
Analysis that pp.17 - 22 of the WR bear «striking similarity» (that's the legal
term, most people say plagiarism) from Wikipedia, Wasserman & Faust (1994) and deNooy, Mrvar, and Bateglj (2005), as shown by Deep
Climate in April.
Now, clouds do not make heat exchange imponderable, especially in long
term trends of
climate analysis, the averages due to what we already know about dynamic equilibrium outcomes and what we observe in the feedbacks going back even greater then 30 years.
Climate analysis requires absolute accuracy as a means of ensuring long
term data quality if technology changes are to be made.
The authors take advantage of a very straightforward
analysis of
climate proxy data, avoiding the highly technical and arcane issues of statistical calibration and methodology that are so frequently seized upon by those who dispute that recent large - scale warmth is anomalous in a long -
term context.
[UPDATE, 2:30 p.m.: William Patzert of NASA's Jet Propulsion Lab has just written to explain that the PDO index above is the result of
analysis in which any long -
term climate trend is removed.
Mike's work, like that of previous award winners, is diverse, and includes pioneering and highly cited work in time series
analysis (an elegant use of Thomson's multitaper spectral
analysis approach to detect spatiotemporal oscillations in the
climate record and methods for smoothing temporal data), decadal climate variability (the term «Atlantic Multidecadal Oscillation» or «AMO» was coined by Mike in an interview with Science's Richard Kerr about a paper he had published with Tom Delworth of GFDL showing evidence in both climate model simulations and observational data for a 50 - 70 year oscillation in the climate system; significantly Mike also published work with Kerry Emanuel in 2006 showing that the AMO concept has been overstated as regards its role in 20th century tropical Atlantic SST changes, a finding recently reaffirmed by a study published in Nature), in showing how changes in radiative forcing from volcanoes can affect ENSO, in examining the role of solar variations in explaining the pattern of the Medieval Climate Anomaly and Little Ice Age, the relationship between the climate changes of past centuries and phenomena such as Atlantic tropical cyclones and global sea level, and even a bit of work in atmospheric chemistry (an analysis of beryllium - 7 measure
climate record and methods for smoothing temporal data), decadal
climate variability (the term «Atlantic Multidecadal Oscillation» or «AMO» was coined by Mike in an interview with Science's Richard Kerr about a paper he had published with Tom Delworth of GFDL showing evidence in both climate model simulations and observational data for a 50 - 70 year oscillation in the climate system; significantly Mike also published work with Kerry Emanuel in 2006 showing that the AMO concept has been overstated as regards its role in 20th century tropical Atlantic SST changes, a finding recently reaffirmed by a study published in Nature), in showing how changes in radiative forcing from volcanoes can affect ENSO, in examining the role of solar variations in explaining the pattern of the Medieval Climate Anomaly and Little Ice Age, the relationship between the climate changes of past centuries and phenomena such as Atlantic tropical cyclones and global sea level, and even a bit of work in atmospheric chemistry (an analysis of beryllium - 7 measure
climate variability (the
term «Atlantic Multidecadal Oscillation» or «AMO» was coined by Mike in an interview with Science's Richard Kerr about a paper he had published with Tom Delworth of GFDL showing evidence in both
climate model simulations and observational data for a 50 - 70 year oscillation in the climate system; significantly Mike also published work with Kerry Emanuel in 2006 showing that the AMO concept has been overstated as regards its role in 20th century tropical Atlantic SST changes, a finding recently reaffirmed by a study published in Nature), in showing how changes in radiative forcing from volcanoes can affect ENSO, in examining the role of solar variations in explaining the pattern of the Medieval Climate Anomaly and Little Ice Age, the relationship between the climate changes of past centuries and phenomena such as Atlantic tropical cyclones and global sea level, and even a bit of work in atmospheric chemistry (an analysis of beryllium - 7 measure
climate model simulations and observational data for a 50 - 70 year oscillation in the
climate system; significantly Mike also published work with Kerry Emanuel in 2006 showing that the AMO concept has been overstated as regards its role in 20th century tropical Atlantic SST changes, a finding recently reaffirmed by a study published in Nature), in showing how changes in radiative forcing from volcanoes can affect ENSO, in examining the role of solar variations in explaining the pattern of the Medieval Climate Anomaly and Little Ice Age, the relationship between the climate changes of past centuries and phenomena such as Atlantic tropical cyclones and global sea level, and even a bit of work in atmospheric chemistry (an analysis of beryllium - 7 measure
climate system; significantly Mike also published work with Kerry Emanuel in 2006 showing that the AMO concept has been overstated as regards its role in 20th century tropical Atlantic SST changes, a finding recently reaffirmed by a study published in Nature), in showing how changes in radiative forcing from volcanoes can affect ENSO, in examining the role of solar variations in explaining the pattern of the Medieval
Climate Anomaly and Little Ice Age, the relationship between the climate changes of past centuries and phenomena such as Atlantic tropical cyclones and global sea level, and even a bit of work in atmospheric chemistry (an analysis of beryllium - 7 measure
Climate Anomaly and Little Ice Age, the relationship between the
climate changes of past centuries and phenomena such as Atlantic tropical cyclones and global sea level, and even a bit of work in atmospheric chemistry (an analysis of beryllium - 7 measure
climate changes of past centuries and phenomena such as Atlantic tropical cyclones and global sea level, and even a bit of work in atmospheric chemistry (an
analysis of beryllium - 7 measurements).
Relevant — Don't Count on Long -
Term Success in Climate Policy, Warns Paper in Decision Analysis Journal (``... consideration of path dependence in the context of climate policy justifies greater near - term emissions reductions in what amounts to a hedging strategy.&raq
Term Success in
Climate Policy, Warns Paper in Decision Analysis Journal (``... consideration of path dependence in the context of climate policy justifies greater near - term emissions reductions in what amounts to a hedging strategy.&
Climate Policy, Warns Paper in Decision
Analysis Journal (``... consideration of path dependence in the context of
climate policy justifies greater near - term emissions reductions in what amounts to a hedging strategy.&
climate policy justifies greater near -
term emissions reductions in what amounts to a hedging strategy.&raq
term emissions reductions in what amounts to a hedging strategy.»)
The long -
term warming of the
climate may be threatening the celebrated Dutch tradition of skating frozen canals and rivers between towns in Friesland, according to a new
analysis of
climate and skating trends there.
However, in
terms of the fast - feedback Charney
analysis, changes in CO2 is treated simply as a forcing being applied from to system from «outside» of the
climate system, and as a forcing it is not viewed as feedback — at least according to Hansen (2007)-- see above.
Given that models have been improving in their ability to model processes, I personally find it difficult to believe that, at least in
terms of a Bayesian
analysis, the models themselves aren't doing better in
terms of their ability to identify
climate sensitivity by applying first principles to our
climate system.
Indeed, scope 3 emissions accounted for three - quarters of offset buyers» emissions, according to Ecosystem Marketplace's
analysis of public CDP disclosures — the elephant in the room in
terms of companies» true
climate impact.
Of course, as they point out «because rainfall is such a variable element, trend values are highly dependent on the start and end dates of the
analysis» and the fact they are simply using linear interpolation it is very difficult to derive anything meaningful in
terms of
climate change from just one map.
Hansen and colleagues put the design of pathways targeting 350 ppm in the context of a detailed
analysis of likely long -
term climate sensitivity.
Conclusion The science of
climate - change teaches that economic
analyses whose outlook is short -
term and / or ideology - driven are moronic and destructive, eh?
Thus, what is that theory, that upon objective examination, rigorous, scientific examination — not by
climate change refuters seeking solely to fit everything into predetermined boxes while self reinforcing such notions by castigating everybody else, but by dispassionate, reasoned,
analysis and objective scientific examination — says or reasonably suggests all this won't have, or doesn't even present a high risk of having, a major impact upon long
term climate.
That is why links to your favorite exemplars of reasoned - yet - short -
term climate - change
analysis would be a welcome contribution to the public discourse, Willis!
Nor do I think that your word «citizen auditor», one of Judy's
terms that I don't use myself and rather dislike, does justice to the fact that the «core» statistical commenters at
Climate Audit and related blogs (Jean S, UC, Ross McKitrick, Roman Mureika, Hu McCulloch, Nic Lewis, Ryan O'Donnell, Jeff Id, Lucia and myself) to name only a few) are more «credentialed» in statistical
analysis than the «scientists» that are being criticized.
the 1.5 to 2 m observations of minimum temperatures that are used as part of the
analysis to assess
climate system heat changes (e.g., such as used to construct Figure SPM - 3 of Intergovernmental Panel on Climate Change [2007] and of Parker [2004, 2006] study) lead to a greater long term temperature trend than would be found if higher heights within the surface boundary layer wer
climate system heat changes (e.g., such as used to construct Figure SPM - 3 of Intergovernmental Panel on
Climate Change [2007] and of Parker [2004, 2006] study) lead to a greater long term temperature trend than would be found if higher heights within the surface boundary layer wer
Climate Change [2007] and of Parker [2004, 2006] study) lead to a greater long
term temperature trend than would be found if higher heights within the surface boundary layer were used.
When Gregory turned the discussion to the potential effects of
climate change and ways to combat them, Blackburn insisted that all potential remedies must be subject to short -
term cost - benefit
analysis.
Most of the costs of
climate change are long -
term, unquantifiable, worst - case, and non-market costs, which are not included in cost - benefit
analyses of
climate action like that of the Garnaut Review.
Similarly,
analyses consistently show the costs of the UK's
Climate Change Act will be more than offset by a combination of fuel savings, avoided climate impacts and reduced air and noise pollution, even before wider economic impacts in terms of jobs and growth are taken into a
Climate Change Act will be more than offset by a combination of fuel savings, avoided
climate impacts and reduced air and noise pollution, even before wider economic impacts in terms of jobs and growth are taken into a
climate impacts and reduced air and noise pollution, even before wider economic impacts in
terms of jobs and growth are taken into account.
«Rather than justifying a lack of response to
climate change, the emphasis on uncertainty enlarges the risk and reinforces the responsibility for pursuing successful long -
term mitigation policy,» according to a 2010
analysis by researchers at Sandia National Laboratory.
In an
analysis of global warming cloud feedbacks, Dessler (2010) used short
term (i.e., not
climate) variations in surface temperature and CERES data to determine that cloud cover was negatively correlated with temperature.
It builds on recent improvements in models, in the reanalysis of
climate data, in methods of initialization and ensemble generation, and in data treatment and analysis to propose an extended comprehensive decadal prediction investigation as a contribution to CMIP6 (Eyring et al., 2016) and to the WCRP Grand Challenge on Near Term Climate Prediction (Kushnir et al.,
climate data, in methods of initialization and ensemble generation, and in data treatment and
analysis to propose an extended comprehensive decadal prediction investigation as a contribution to CMIP6 (Eyring et al., 2016) and to the WCRP Grand Challenge on Near
Term Climate Prediction (Kushnir et al.,
Climate Prediction (Kushnir et al., 2016).
Assuming that
climate change and other deep uncertainties can not be eliminated over the short
term (and probably even over the longer
term), it then summarizes existing decision - making methodologies that are able to deal with
climate - related uncertainty, namely cost - benefit
analysis under uncertainty, cost - benefit
analysis with real options, robust decision making, and
climate informed decision
analysis.
Many
climate trends are small and require careful
analysis of long time series of sufficient length, consistency, and continuity to distinguish between the natural long -
term climate variability and any small, persistent
climate changes.
«Here we present an
analysis based on sea - level data from the altimetry record of the past ~ 20 years that separates interannual natural variability in sea level from the longer -
term change probably related to anthropogenic global warming... Our results confirm the need for quantifying and further removing from the
climate records the short -
term natural
climate variability if one wants to extract the global warming signal.»
Jeff Knight said: «Our
analysis shows that
climate change likely did make a contribution to the record rainfall in 2013 - 14 through a long -
term increase in UK winter rainfall that is not associated with changing weather patterns.
In
terms of jobs, economics and U.S. energy security, Keystone XL makes sense — without significant
climate or environmental impacts, according to the U.S. State Department, which conducted five
analyses of the project.
«
Climate Services» sounds to me like one or two have done the same
analysis and are desperately trying to find a future role in medium
term weather forecasting.
An
analysis by Bjorn Lomborg, the former director of Denmark's Environmental Assessment Institute and advocate for long -
term climate solutions, found that the Accord would only reduce global temps up to 0.17 degrees Celsius by 2100!
As someone who isn't bright or knowledgeable enough to understand the science, I'd say that any conclusions made on
analysis of long -
term climate trends that looks dramatically different based on the inclusion or exclusion of only 10 years of data should be viewed as «information» — useful but certainly not dispositive..
And this all supports the
analysis that the
climate is much more sensitive to changes in greenhouse gas emissions and other «forcings» than the IPCC models have been saying and that a doubling of atmospheric concentrations of carbon dioxide from preindustrial levels to 550 ppm will ultimately warm the planet far more than 3 °C, as NASA's James Hansen argues (see «Long -
term»
climate sensitivity of 6 °C for doubled CO2).
In summary, given the large uncertainties, I am unconvinced by Annan and Hargreave's
analysis in
terms of providing limits to the range of expected
climate sensitivity values.
Analyses of ωo from long -
term AERONET sites influenced by Saharan dust suggest an average ωo of 0.95 at 0.67 µm (Dubovik et al., 2002), while unpolluted Asian dust during the Aeolian Dust Experiment on
Climate (ADEC) had an average ωo of 0.93 at 0.67 µm (Mikami et al., 2006 and references therein).
Bioenergy from annual crops has a poor life cycle
analysis in
terms of
climate impact, but some perennial bioenergy crops have modest potential.
My
analysis shows that the most frequently adopted
term in the studied sample is «
climate change», while other
terms such as «global warming» and «greenhouse effect» are rarely used.
These and other observations can be integrated into a model with feedbacks and having two unstable end ‐ points that is consistent both with classical studies of past
climate states, and also with recent
analysis of ice dynamics in the Arctic basin by Zhakarov, whose oscillatory model identifies feedback mechanisms in atmosphere and ocean, both positive and negative, that interact in such a manner as to prevent long ‐
term trends in either ice ‐ loss or ice ‐ gain on the Arctic Ocean to proceed to an ultimate state.
«Based on the results from this emergence timescale
analysis we urge extreme caution in attributing short -
term trends (i.e. over many decades and longer) in normalized US tropical cyclone losses to anthropogenic
climate change,» says Crompton.