The actual prevailing view of the paleoclimate research community that emerged during the early 1990s, when long - term proxy data became more widely available and it was possible to synthesize them into estimates of large - scale temperature changes in past centuries, was that the average temperature over the Northern Hemisphere varied by significantly less than 1 degree C in previous centuries (i.e.,
the variations in past centuries were small compared to the observed 20th century warming).
4 Dec 2004 Temperature
Variations in Past Centuries and the so - called «Hockey Stick» http://www.realclimate.org/index.php?p=7
Not exact matches
Over the
past quarter
century the level of the fed funds rate has explained nearly 50 % of the
variation in stock / bond correlations, according to Bloomberg data.
But as I noted last week (see Two Point Three Sigmas Above the Norm), nominal growth and interest rate
variations have historically canceled out over the
past century, with little effect on the accuracy of our valuation estimates — matched reductions
in the growth rate and the discount rate really don't affect fair value.
Rather than using complex computer models to estimate the effects of greenhouse - gas emissions, Lovejoy examines historical data to assess the competing hypothesis: that warming over the
past century is due to natural long - term
variations in temperature.
Variations in the Sun's brightness are known to have played a part
in global warming over the
past few
centuries.
However, unlike the climate model simulations, the new precipitation reconstruction does not show an increase of wet and dry anomalies
in the twentieth
century compared to the natural
variations of the
past millennium.
2) A better ability to constrain climate sensitivity from the
past century's data 3) It will presumably be anticorrelated with year to year
variations in global surface temperature that we see, especially from El Ninos and La Ninas, which will be nice whenever we have a cool year and the deniers cry out «global warming stopped!».
In fact, scientists have long recognized the importance of solar variability as one of the factors governing climate (see the very scholarly review of the subject by Bard and Frank, available here at EPSL or here as pdf) An understanding of solar variability needs to be (and is) taken into account in attribution of climate change of the past century, and in attempts to estimate climate sensitivity from recent climate variation
In fact, scientists have long recognized the importance of solar variability as one of the factors governing climate (see the very scholarly review of the subject by Bard and Frank, available here at EPSL or here as pdf) An understanding of solar variability needs to be (and is) taken into account
in attribution of climate change of the past century, and in attempts to estimate climate sensitivity from recent climate variation
in attribution of climate change of the
past century, and
in attempts to estimate climate sensitivity from recent climate variation
in attempts to estimate climate sensitivity from recent climate
variations.
Over the
past quarter
century the level of the e BoC overnight rate has explained nearly 29 % of the
variation in stock / bond correlations, according to Bloomberg data.
Over the
past quarter
century the level of the fed funds rate has explained nearly 50 % of the
variation in stock / bond correlations, according to Bloomberg data.
2) A better ability to constrain climate sensitivity from the
past century's data 3) It will presumably be anticorrelated with year to year
variations in global surface temperature that we see, especially from El Ninos and La Ninas, which will be nice whenever we have a cool year and the deniers cry out «global warming stopped!».
Records of tree - ring characteristics such as their width (TRW) and density (usually the maximum density of the wood formed towards the end of the growing season — the «maximum latewood density» — MXD) are widely used to infer
past variations in climate over recent
centuries and even millennia.
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 measurements).
If there was more natural
variation in the
past millenia, specifically due to solar changes, then that goes at the cost of the GHG / aerosol combination, as both are near impossible to distinguish from each other
in the warming of the last halve
century... Solar activity has never been as high, and for an as long period, as current
in the
past millenium (and even the
past 8,000 years).
For the station nearest my home, the range (max less min)
in annual average temperature for the
past century is just 3.3 C. Can't say whether 1C warming matters
in any tangible way, at this particular spot, but it's certainly large compared to the
variation observed over the last
century.
But as we started to try to piece together the puzzle of what those data were telling us, they also were telling us about natural
variations in temperature
in the
past and how they compared to the warming trends of the
past century.
This section focuses on global and regional sea level
variations, over time spans ranging from the last decade to the
past century; a brief discussion of sea level change
in previous
centuries is given
in Section 5.5.2.4.
Member of the team Alena Kimbrough says, «We've shown ENSO is an important part of the climate system that has influenced global temperatures and rainfall over the
past millennium... Our findings, together with climate model simulations, highlight the likelihood that
century - scale
variations in tropical Pacific climate modes can significantly modulate radiatively forced shifts
in global temperature.»
You can also look at the growth rings
in the oldest trees and
in pieces of wood that have been preserved from
centuries past, and try to untangle how much of the
variation in growth per year is due to temperatures versus rain, fertilization, disease, etc..
States that geological records of
past climates have shown
century - long
variations in TC numbers
On multi-decadal timeframes, GH gas forcing and the PDO / AMO combination have been having fairly even
in their relative forcing over the
past century, but the GH gas forcing is growing so large that it now dominating these longer - term natural
variations... so the kicker is that the rapidly increasing GH gases, now at their highest levels
in millions of years, are very likely influencing the nature of ENSO, PDO, AMO, and other formerly «natural» cycles.
«The temperature
variations read
in the
past century could be part of a larger process that is alien to humanity.»
In this new paper they write: «The most striking features in the reconstruction are the warm temperatures from ∼ 1050 to ∼ 1300 AD compared to the preceding and following centuries, the persistent cooler temperatures from ∼ 1400 to ∼ 1800 AD, and the subsequent rise to warmer temperatures which eventually seem to exceed in the last decades of the 20th century the range of past variatio
In this new paper they write: «The most striking features
in the reconstruction are the warm temperatures from ∼ 1050 to ∼ 1300 AD compared to the preceding and following centuries, the persistent cooler temperatures from ∼ 1400 to ∼ 1800 AD, and the subsequent rise to warmer temperatures which eventually seem to exceed in the last decades of the 20th century the range of past variatio
in the reconstruction are the warm temperatures from ∼ 1050 to ∼ 1300 AD compared to the preceding and following
centuries, the persistent cooler temperatures from ∼ 1400 to ∼ 1800 AD, and the subsequent rise to warmer temperatures which eventually seem to exceed
in the last decades of the 20th century the range of past variatio
in the last decades of the 20th
century the range of
past variation.
Although the I.P.C.C. allowed for the possibility that
variations in sunlight could have ended the «Little Ice Age,» a period of cooling from the 14th
century to about 1850, our data argues strongly that the temperature rise of the
past 250 years can not be attributed to solar changes.
Even while identifying some of the observed change
in climatic behaviour, such as a 0.4 C increase
in surface temperature over the
past century, or about 1 mm per year sea level rise
in Northern Indian Ocean, or wider
variation in rainfall patterns, the document notes that no firm link between the do...
Citation: Zhang, Q., W.H. Soon, S.L. Baliunas, G.W. Lockwood, B.A. Skiff and R.R. Radick, 1994; A method of determining possible brightness
variations of the Sun
in past centuries from observations of solar - type stars.
In the absence of an obvious amplification mechanism, evidence for strong amplification is meager, and is also apparently at odds with solar / temperature relationships over the
past century and earlier outside of the cyclic
variations.
Your observation that paleo records tend to miss the shorter term
variations seen
in instrumental records is interesting, as this weakness would lead to doubtful conclusions that
past centuries saw less climate variability than we now observe (Shaun Lovejoy article
in Climate Etc.
in January 2013).
Even if we could assign a certain fraction of warming over the
past century or so to natural
variation, we still would face very large uncertainty
in aerosol influences... and modelers would continue to use those vastly uncertain aerosol influences as as a «free» variable to «tune» the models.
Drought
variations in the eastern part of northwest China over the
past two
centuries: evidence from tree rings.
In order to extend diagnoses of recent sea - ice
variations beyond the
past few decades, a
century - scale digital dataset of Arctic sea - ice coverage has been compiled.
Indeed, Brown explained to Media Matters that Limbaugh is «wrong» to attribute recent warming to solar activity, and added that human activity is a much bigger contributor to warming
in the
past century than natural
variation:
Although natural
variations in the solar output can explain most of the temperature
variations over the
past centuries, it appears that global warming by heat - trapping gases, emitted by human activity, is required to explain the sharp rise
in global temperatures during the 1990s.
Changes
in the amount or distribution of the sunlight illuminating the Earth can produce substantial
variations in our climate, and we have proxy records of its variable output over
past centuries.