As far as studying CO2 is concerned, I said I never did heat capacity ratio
experiments on CO2.
All experiments on co2 show how it absorbs infrared radiation, not how it raise the temperature of the heat source.
Not exact matches
Meanwhile, Ramanathan said that Jacobson's conclusion that black carbon might be the second - largest contributor to warming — behind only
CO2 — tracks with his own
experiments based
on observations of actual climatic conditions.
The simulations, which were run
on UCL's Legion supercomputer and HECToR (the UK national supercomputing service), provided a molecule - by - molecule view of how the
CO2 and greigite interacted, helping to make sense of what was being observed in the
experiments.
And that's what
experiments on plants grown in elevated
CO2 have always shown — until now.
In the first
experiment, elevated
CO2 concentrations did not show any effect
on the bladder wrack at any season.
For the study, Gentine and Lemordant took Earth system models with decoupled surface (vegetation physiology) and atmospheric (radiative)
CO2 responses and used a multi-model statistical analysis from CMIP5, the most current set of coordinated climate model
experiments set up as an international cooperation project for the International Panel
on Climate Change.
On arrival, islets were immediately placed in CMRL 1066 (Cellgro; Corning) enriched medium, supplemented with 2 mM l - glutamine (Cellgro CN - 25 -005-CI; Corning), 1 mM sodium pyruvate, (Cellgro CN -25-000-CI; Corning), 10 mM Hepes - free acid, (Cellgro CN - 25 -060-CI; Corning), 10 U / ml heparin (Hospira RL - 4311; Pfizer), and 10 mM nicotinamide, (CN N0636; Sigma - Aldrich) at 24 °C with 5 %
CO2 for 7 d to stabilize the islets before starting the
experiments.
In our
experiment, we monitored Escherichia coli diauxie growth phases online and focused
on dissolved
CO2 (dCO2) and oxygen readings.
As Table S1 in my paper showed, there are differences even in the response to histGHG vs 1 % per year
CO2 on the order of 10 %, so we would expect the TCR for each model to vary somewhat when computed based
on a slightly different set of
experiments, but even if the correct dT values and all forcings were included I don't believe the results would tell us anything useful.
Exxon's own scientists conducted an extensive research program
on climate change and «The Greenhouse Effect», running complex
CO2 monitoring
experiments and publishing peer - reviewed papers, because the company was deeply interested in this emerging threat to its core business, oil, and ultimately the company's survival.
Now, forgetting entirely the more complex issue of «climate sensitivity» and focusing only
on how tiny, minute concentrations of
CO2 can make a difference to global temps — one of the oft - repeated and simplistic denialist memes — is there a simple desktop
experiment to demonstrate how that can work?
Field
experiments on the ground and aircraft profiling of
CO2 over tropical forests have documented the impact of heat and drought
on forest productivity, but they are few and far between.
We incubated a natural diatom community from coastal New Zealand waters in a short - term incubation
experiment using a factorial matrix of temperature and
CO2, and measured effects
on community structure.
This is very difficult to explain to a non-scientist, but basically it is an established scientific fact based
on long - established
experiment and theory that simple molecules like O2 and N2 don't absorb infra - red radiation whereas more complicate molecules such as
CO2 and H2O can.
Causality of
CO2 influence
on climate is, after all, proved by
experiments of its effect
on absorbing longwave radiation.
The problems with associating sensitivity with a temperature in 2100 are twofold: first, at the time we reach
CO2 doubling, the temperature will lag behind the equilibrium value due to thermal inertia, especially in the ocean (thought
experiment — doubling
CO2 today will not cause an instant 3C jump in temperatures, any more than turning your oven
on heats it instantly to 450F), and secondly, the
CO2 level we are at in 2100 depends
on what we do between now and then anyway, and it may more than double, or not.
We had hoped that extra
CO2 would prompt more uptake by plants, but large - scale
experiments on forests supplemented with
CO2 gas did not yield increased growth.
As a youth I participated in many of my father's
experiments, observing first - hand the benefits of atmospheric
CO2 on plant life and the manifold problems with the model - based theory of climate change, all of which events occurred long, long before James Hansen stood in front of the U.S. Senate and brought the
CO2 debate to the eyes of the public in 1988.
Now, forgetting entirely the more complex issue of «climate sensitivity» and focusing only
on how tiny, minute concentrations of
CO2 can make a difference to global temps — one of the oft - repeated and simplistic denialist memes — is there a simple desktop
experiment to demonstrate how that can work?
In essence, this technology is kind of akin to the thought
experiment in which I mused
on whether the climate challenge would be easier to grasp if
CO2 were pink.
(I'd love to see some data visualization
experiments on this idea from Adam Nieman, building
on his work showing the volume of daily
CO2 emissions from cities and the like.)
Current attempts by national governments worldwide to control industrial
CO2 emissions following the recommendations of the IPCC could be viewed within the scientific paradigm as the projection of a large scale
experiment on the earth's climate system to validate the hypothesis that anthropogenic
CO2 emissions through the burning of fossil fuels and land use changes (inter alia) are a major factor driving climate change.
Effects of Atmospheric
CO2 Concentration
on Wheat Yield: Review of Results from
Experiment using Various Approaches to Control
CO2 Concentration.
«Seasonal Cycle
Experiments on Climate Sensitivity Due to a Doubling of
CO2 with an Atmospheric General Circulation Model Coupled to a Simple Mixed Layer Ocean Model.»
Comparing model predictions of GHG - induced warming with recent natural temperature fluctuations also indicates the potential scale of man - made climate change.Early modelling
experiments focused
on the total long - term change resulting from a doubling of carbon dioxide (
CO2) levels.
Based
on thousands of laboratory and field
experiments increasing
CO2 is not causing a climate problem and is a great benefit to agriculture, the environment, and humanity.
In my limited reading
on the web I have read of laboratory
experiments with flasks of pure
CO2 and light sources in excess of 1,000 K and yes,
CO2 on CO2 molecular collisions do show line broadening.
«Natural
Experiments» and
CO2 - Induced Climate Change: The Controversy Drags
on (Editorial).»
As a lay person, I asked why we can't do
experiments on a replica of the atmosphere, which would include adding
CO2 to it and seeing by how much it warmed up in sunlight / infra red etc..
Princeton has done an analysis
on «Century - scale change in water availability:
CO2 - quadrupling
experiment,» which is to say 1100 ppm.
Based
on the empirical evidence of the laboratory
experiments, it is quite possible that the increasing
CO2 in the atmosphere during interglacial periods could have amplified the warming already occurring.
How exactly are you proving your point when you admit (emphasis mine)... «yes, the temperature moved FIRST» and you make hidden conciliatory statements like... «for the MAJORITY of that time» and then you freely admit... «
CO2 did not trigger the warmings» and then you rely
on the lamest of hollow arguments... «according to climate THEORY and model
EXPERIMENTS» and then you stumble back to close with complete opinion and conjecture... «we may well» and «The likely candidates» Anyone with a brain will read your post and laugh - it's pathetic and you've actually done nothing but strengthen the skeptics argument.
Long - term
CO2 enrichment studies confirm the findings of shorter - term
experiments, demonstrating numerous growth - enhancing, water - conserving, and stress - alleviating effects of elevated atmospheric
CO2 on plants growing in both terrestrial and aquatic ecosystems.
I then later posted a longer commentary
on the Atmospheric
CO2 Thermostat that included (1) a description of our recent water vapor feedback / forcing
experiments, (2) an illustration describing high accuracy GCM LW radiation calculations, (3) a short discourse
on the latitudinal nature of climate feedbacks, and (4) an overview of those things that we know well (about climate), and those things that we know less well.
You might not find a recent journal article
on the specific
CO2 experiment, because it was settled a long time ago, before most journals went to electronic publishing.
Do you understand the implications of the fact that we've already performed a very large scale
experiment, testing the effect of
CO2 level
on the rate of sea - level rise — and found no effect at all?
The warming we've had in the last thirty years implies that at best, we could expect 1 °C from a doubling of
CO2, but observations from eight natural
experiments around the globe, and even
on Mars and Venus suggest that 0.4 °C is the upper bound of climate sensitivity to any cause.
A recent paper in Science reported
on a breakthrough
experiment in Iceland in which
CO2 (from a volcanic source) dissolved in water was injected into basalts at depths of 400-1000 metres.
In Part A, you will carry out a class
experiment to test the effects of increased amounts of
CO2 on pH. Then, you will analyze time - series graphs to search for relationships between trends in atmospheric
CO2, dissolved
CO2 in seawater, and changes in ocean pH. In Part B, you will review and analyze the results of research compiled by the Woods Hole Oceanographic Institute
on the effect of ocean acidification
on a variety of marine organisms.
The explanation of main stream science for the warming effect of
CO2 is based
on knowledge learned from laboratory
experiments, but it's not possible to replicate the whole process in a laboratory, because the thickness of the troposphere is an important part of the explanation.
you may observe that at around 400 ppmv, the net rate of photosynthesis in ideal greenhouse conditions begins to gain much less per additional unit of
CO2; we've already hit the point of diminishing returns and by Liebig's Law of the Minimum can say with some confidence that
experiments could find that additional
CO2 on plants in the wild may be net detrimental right now.
I thought I saw
on this site some time back a home
experiment you can do to show that temperature causes an increase in atmospheric
CO2 levels.
Our global civilization is conducting an unprecedented, unplanned
experiment (major global recession) in reducing human
CO2 emissions, and it's not having much impact
on CO2 levels in the atmosphere.
Very few experimental approaches have assessed ecosystem responses to multi-factorial treatments such as listed above (Norby and Luo, 2004), and
experiments on warming, rainfall change or atmospheric
CO2 level are virtually absent in savannas, with many ecosystem studies confined mainly to temperate grasslands (Rustad et al., 2001).
There are few factorial
experiments on multiple changing factors, but they suggest interactions that are not predictable from single factor
experiments — such as the dampening effect of elevated
CO2 on California C3 grassland responses to increased rainfall, nitrate and air temperature (Shaw et al., 2002).
There are no test results from
experiments on whether or not
CO2 causes more cooling or warming or what the net effect is and unless someone will sue the oil companies to research this, we will never know.
9.3.1 Global Mean Response 9.3.1.1 1 % / yr
CO2 increase (CMIP2)
experiments 9.3.1.2 Projections of future climate from forcing scenario
experiments (IS92a) 9.3.1.3 Marker scenario
experiments (SRES) 9.3.2 Patterns of Future Climate Change 9.3.2.1 Summary 9.3.3 Range of Temperature Response to SRES Emission Scenarios 9.3.3.1 Implications for temperature of stabilisation of greenhouse gases 9.3.4 Factors that Contribute to the Response 9.3.4.1 Climate sensitivity 9.3.4.2 The role of climate sensitivity and ocean heat uptake 9.3.4.3 Thermohaline circulation changes 9.3.4.4 Time - scales of response 9.3.5 Changes in Variability 9.3.5.1 Intra-seasonal variability 9.3.5.2 Interannual variability 9.3.5.3 Decadal and longer time - scale variability 9.3.5.4 Summary 9.3.6 Changes of Extreme Events 9.3.6.1 Temperature 9.3.6.2 Precipitation and convection 9.3.6.3 Extra-tropical storms 9.3.6.4 Tropical cyclones 9.3.6.5 Commentary
on changes in extremes of weather and climate 9.3.6.6 Conclusions
ΔF = α ln (C / C0)(end of quote) So when I do an
experiment on a nightly basis I find that every night, the temperature goes dDOWN inspite of all the
CO2 that man has added that day & the IPCC & Arrhenius mantra that that more GHGz means more warming.
There can never be conducted an
experiment with atmospheric levels of
CO2 on the planet to conclude with statements about cause and effect.