Not exact matches
The final
years of work and the first few
years of retirement tend to have
increased variability of either income, deductions, or both.
Such
variability between
years is the reason why the number of chicks dying from climate change is not a tidy, ever -
increasing figure each
year.
I plotted out the
variability in million -
year intervals and found that about 6 million
years ago, that
variability went off the charts and kept
increasing.
«My view on this is that the research needs to broaden out to have more of a focus on
variability more generally so that a) we can predict the next few
years better b) we can refine our estimates of the sensitivity of the climate system to
increases in greenhouse gas concentrations.»
The
increase in
variability among the later points suggests a decrease in social learning and possibly a reduction in overall interactions among North American populations beginning around 12,500
years ago, the researchers say.
«The challenge is really first understanding what the natural
variability looks like in this data - poor region, and then making measurements long enough that we can tease out the long - term ocean acidification trend, which is this gradual
increase through time,» he said «It's really hard to see with just one or two
years of data.»
has decreased in winter, but no significant change in annual mean precipitation potentially because of very slight
increases in spring and fall precipitation; precipitation is projected to
increase across Montana, primarily in spring; slight decrease in summer precipitation;
variability of precipitation
year - to -
year projected to
increase
As the first mission to provide extensive time series measurements on thousands of stars over months to
years at a level hitherto possible only for the Sun, the results from Kepler will vastly
increase our knowledge of stellar
variability for quiet solar - type stars.
El Niño is one of the biggest drivers of
year - to -
year variability,
increasing the likelihood of warm weather in the Pacific Northwest and cooler weather in the Southeast as well as a host of other global impacts.
By looking at the signatures of climate change in precipitation intensity and comparing that to the internal
variability and the observation, the researchers conclude that the probability of intense precipitation on any given day has
increased by 7 percent over the last 50
years — well outside the bounds of natural
variability.
Of course, on a timescale of one decade the noise in the temperature signal from internal
variability and measurement uncertainty is quite large, so this might be hard to determine, though tamino showed that five
year means show a monotonic
increase over recent decades, and one might not unreasonably expect this to cease for a decade in a grand solar minimum scenario.
Increased variability and unpredictability of conditions
year to
year, likely in a dissipative system being pushed out of its current basin of metastability, could make things very difficult for farmers worldwide.
It is these uppermost few percent of events that are important, and models and theory are nearly unanimous now that they are and will continue to
increase, notwithstanding natural climate
variability on shorter time scales (as much as 20
years).»
A globally warm medieval period could be a simple forced response to
increased solar, in which case it doesn't imply any larger intrinsic
variability than already assumed, and since solar has been pretty much constant over the last 50
years, improvements to our understanding of solar forced climate changes are irrelevant for the last few decades.
Now — apparently — if the next 20
years fail to show the expected level of
increase — then it's all down to natural
variability.
Wili: As ice volume decreases, the fraction of volume which is new ice
increases, and hence the
year to
year variability in new ice becomes a larger fraction of the total ice volume
variability, so I don't think the smoothed downward slope will stay as smooth, i.e. you should expect bigger surprises to the upside on a given winter if it is cold and has heavy snow fall.
Averaging smoothes out day - to - day and
year - to -
year natural weather
variability and extremes, removing much of the chaotic behavior, revealing any underlying long term trends in climate, such as a long term
increase or decrease in temperature, or long term shifts in precipitation patterns.
-- Without forgetting a significant interannual
variability in OHC
increase... the average value, 10 - 15
years ago, was close to 8 ZJ per
year, that is # 250 TW on average.
-- I calculated potential intensity trends over the period 1980 - 2012 & The disparity between the reanalysis potential intensity trends over the past 30
years and the projected trends over this century suggests either that most of the observed
increase in potential intensity (and actual intensity of high category storms) is due to natural
variability,....»
Global temperature has in recent
years increased more slowly than before, but this is within the normal natural
variability that always exists, and also within the range of predictions by climate models — even despite some cool forcing factors such as the deep solar minimum not included in the models.
It would seem that if you wanted to examine this using GCMs and temperature
variability, you'd want to run the more realistic scenario of a gradual 1 %
increase in CO2 per
year followed by adjustment to equilibrium.
If you are of the opinion that temperature
variability on a short time scale is insignificant, how can we declare as fact that the rise in global temperature over the past 50
years is incontrovertibly tied to the
increase in CO2 levels?
Fig. 6 confirms that there has been little
increase of the 60 - month (5 -
year) and 132 - month (11 -
year) running means in the past decade, although it is not obvious that such a slowdown is outside the norm of unforced decadal
variability.
But the evidence shows this can't be true; temperature changes before CO2 in every record of any duration for any time period; CO2
variability does not correlate with temperature at any point in the last 600 million
years; atmospheric CO2 levels are currently at the lowest level in that period; in the 20th century most warming occurred before 1940 when human production of CO2 was very small; human production of CO2
increased the most after 1940 but global temperatures declined to 1985; from 2000 global temperatures declined while CO2 levels
increased; and any reduction in CO2 threatens plant life, oxygen production, and therefore all life on the planet.
What I think we'll see (in fact, I'm pretty sure of it) is a paper later on this
year giving a pretty good summary of natural
variability that led to the «hiatus» in atmospheric temperature
increases and their relative contributions:
My own expectation is that we will have a great
increase in
year - over-
year variability but that it will be difficult to say much else.
A fragmentation of the cultural landscapes in the arid and semi-arid lands of Mongolia has
increased vulnerability and reduced the adaptive capacities to climate
variability of traditional pastoral systems, which have evolved over thousands of
years.
You do not mention
increased year - over-
year and decade - over-decade
variability as the climate system gets further from equilibrium.
All together, the trend and
variability don't look that bad... Anyway, the trend of accumulation in the atmosphere is far more of interest than the
year - by -
year increase and the
variability around the
increase...
For the past 55 million
years the global surface temperature has declined by more than 10 °C from a «hot house» condition into an «ice house» with
increasing temperature
variability as depicted in Figure 1 (Mya = millions of
years ago).
«When you're
increasing the
variability of the climate, one
year you can have a flood and the next
year you can have a drought.
«Looking at 1,000
years of temperature records, researchers found that natural
variability in surface temperatures over the course of just a decade can account for
increases and dips in warming rates.»
The expected
increase in temp in a BAU scenario will likely go far outside of the bound of
variability that we have seen over the past 10,000
years
FE in # 510: referencing discussion on nature as a sink to last 50
years «there is no visible
increase or decrease in natural
variability over 50
years.»
As of this writing, there is observational and modeling evidence that: 1) both annular modes are sensitive to month - to - month and
year - to -
year variability in the stratospheric flow (see section on Stratosphere / troposphere coupling, below); 2) both annular modes have exhibited long term trends which may reflect the impact of stratospheric ozone depletion and / or
increased greenhouse gases (see section on Climate Change, below); and 3) the NAM responds to changes in the distribution of sea - ice over the North Atlantic sector.
To give a comparison, why the
variability of a variable is not important at all: the
increase or decrease in sealevel needs some 25
years to statistically separate the few mm change from the meters of
variability caused by waves, tides, storm surges,...
We were talking about the
variability of the CO2
increase over the past 50
years.
And that is all what matters for the
year by
year increase or decrease or the
variability in the atmosphere.
Whether the faster rate for 1993 to 2003 [3.1 mm /
year] reflects decadal
variability or an
increase in the longer - term trend is unclear.
I will confess that I was initially baffled by this post, for it was my prejudice that the general
increase in OHC over the last ~ 50
years leaves so little room for benign warming due to some internal
variability, that is I failed initially to see what case had to be answered and hence I failed to comprehend your argument.
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.
However, the
increase in sea ice extent for 2009 does not exceed past interannual
variability in a near - continuous, 30 -
year downward trend in summer sea ice extent.
The robustly project
increased moisture flux convergence and precipitation in the pan-Arctic region over the 21st century, as did their AR4 counterparts (Kattsov et al., 2007; Rawlins et al., 2010 Then we get: since nearly all models project a large precipitation
increase rising above the
variability year - round, it is likely the pan-Arctic region will experience a statistically - significant
increase in precipitation by mid-century.
Irrespective of what one thinks about aerosol forcing, it would be hard to argue that the rate of net forcing
increase and / or over-all radiative imbalance has actually dropped markedly in recent
years, so any change in net heat uptake can only be reasonably attributed to a bit of natural
variability or observational uncertainty.
The Earth responds to the milliwatts per
year from
increasing CO2 at the same rate that it responds to seasonal solar power
variability.
The direct climate forcing due to measured solar
variability, about 0.2 W / m2, is comparable to the
increase in carbon dioxide forcing that occurs in about seven
years, using recent CO2 growth rates.
«However, Fig. 15 and the associated uncertainties discussed in Section 3.4 show that long term estimates of time variable sea level acceleration in 203
year global reconstruction are significantly positive, which supports our previous finding (Jevrejeva et al., 2008a), that despite strong low frequency
variability (larger than 60
years) the rate of sea level rise is
increasing with time.»
Even significant if you include the
year by
year variability in
increase rate (of + / - 0.5 ppmv) around the trend.
I don't consider myself to be an expert by any means but in the few
years I have been taking an interest in the subject of climate change I have tried to educate myself as much as possible about the various scientific arguments surrounding the subject, and one thing that has constantly been impressed upon my mind is that when there is a long term trend caused by
increasing GHG levels there will periods when it is masked (or accentuated) by short term natural
variability.
Apart from colder regions and seasons, characterised by greater internal climate
variability, the odds of warm events are found to have significantly
increased and temperatures above the threshold of 1 - in - 10
year events during 1961 — 1990 have become at least twice as likely to occur.