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Maybe I've been growing things wrong, but last time I checked, a rise in temperature actually helped increase agriculture. Isn't that why we grow crops during the warmer months?
Originally posted by crimvelvet
Maybe I've been growing things wrong, but last time I checked, a rise in temperature actually helped increase agriculture. Isn't that why we grow crops during the warmer months?
How come every one forgets how lush the plant life was during the age of the dinosaurs?
The temperature change I would worry about is a drop in temp by 2 degrees. Canada would be in a world of hurt and so would Russia. That means that much less farmland to feed people.....Bring on as much CO2 as possible stop global cooling!!!
P.S. I always enjoy your posts
Originally posted by TheRedneck
reply to post by majestictwo
CO2 has a minimal effect on oceanic acidity levels; this is simply another claim that cannot be supported by science. The chemical equation used here is OH- + CO2 --> HCO3-.
blah blah small numbers
Most carbon dioxide released into the atmosphere as a result of the burning of fossil fuels will eventually be absorbed by the ocean1, with potentially adverse consequences for marine biota2–4. Here we quantify the changes in ocean pH that may result from this continued release of CO2 and compare these with pH changes estimated from geological and historical records.We find that oceanic absorption of CO2 from fossil fuels may result in larger pH changes over the next several centuries than any inferred from the geological record of the past 300 million years, with the possible exception of those resulting from rare, extreme events such as bolide impacts or catastrophic methane hydrate degassing.
Dynamic patterns and ecological impacts of declining ocean pH in a high-resolution multi-year dataset
J. Timothy Wootton1, Catherine A. Pfister, and James D. Forester2
+Author Affiliations
Department of Ecology and Evolution, University of Chicago, 1101 East 57th Street, Chicago, IL 60637
Communicated by Robert T. Paine, University of Washington, Seattle, WA, October 8, 2008 (received for review August 8, 2008)
Abstract
Increasing global concentrations of atmospheric CO2 are predicted to decrease ocean pH, with potentially severe impacts on marine food webs, but empirical data documenting ocean pH over time are limited. In a high-resolution dataset spanning 8 years, pH at a north-temperate coastal site declined with increasing atmospheric CO2 levels and varied substantially in response to biological processes and physical conditions that fluctuate over multiple time scales. Applying a method to link environmental change to species dynamics via multispecies Markov chain models reveals strong links between in situ benthic species dynamics and variation in ocean pH, with calcareous species generally performing more poorly than noncalcareous species in years with low pH. The models project the long-term consequences of these dynamic changes, which predict substantial shifts in the species dominating the habitat as a consequence of both direct effects of reduced calcification and indirect effects arising from the web of species interactions. Our results indicate that pH decline is proceeding at a more rapid rate than previously predicted in some areas, and that this decline has ecological consequences for near shore benthic ecosystems.
GEOPHYSICAL RESEARCH LETTERS, VOL. 34, L07603, doi:10.1029/2006GL028554, 2007
Impact of elevated CO2 on shellfish calcification
Frédéric Gazeau
Centre for Estuarine and Marine Ecology, Netherlands Institute of Ecology, Yerseke, Netherlands
Christophe Quiblier
Centre for Estuarine and Marine Ecology, Netherlands Institute of Ecology, Yerseke, Netherlands
Jeroen M. Jansen
Centre for Estuarine and Marine Ecology, Netherlands Institute of Ecology, Yerseke, Netherlands
Jean-Pierre Gattuso
Laboratoire d'Océanographie de Villefranche, Centre National de la Recherche Scientifique, Villefranche-sur-Mer, France
Laboratoire d'Océanographie de Villefranche, Université Pierre et Marie Curie, Paris VI, Villefranche-sur-Mer, France
Jack J. Middelburg
Centre for Estuarine and Marine Ecology, Netherlands Institute of Ecology, Yerseke, Netherlands
Carlo H. R. Heip
Centre for Estuarine and Marine Ecology, Netherlands Institute of Ecology, Yerseke, Netherlands
Abstract
Ocean acidification resulting from human emissions of carbon dioxide has already lowered and will further lower surface ocean pH. The consequent decrease in calcium carbonate saturation potentially threatens calcareous marine organisms. Here, we demonstrate that the calcification rates of the edible mussel (Mytilus edulis) and Pacific oyster (Crassostrea gigas) decline linearly with increasing pCO2. Mussel and oyster calcification may decrease by 25 and 10%, respectively, by the end of the century, following the IPCC IS92a scenario (∼740 ppmv in 2100). Moreover, mussels dissolve at pCO2 values exceeding a threshold value of ∼1800 ppmv. As these two species are important ecosystem engineers in coastal ecosystems and represent a large part of worldwide aquaculture production, the predicted decrease of calcification in response to ocean acidification will probably have an impact on coastal biodiversity and ecosystem functioning as well as potentially lead to significant economic loss.
Letters to Nature
Nature 407, 364-367 (21 September 2000) | doi:10.1038/35030078; Received 2 August 1999; Accepted 18 July 2000
Reduced calcification of marine plankton in response to increased atmospheric CO2
Ulf Riebesell1, Ingrid Zondervan1, Björn Rost1, Philippe D. Tortell2, Richard E. Zeebe1,3 and François M. M. Morel2
The formation of calcareous skeletons by marine planktonic organisms and their subsequent sinking to depth generates a continuous rain of calcium carbonate to the deep ocean and underlying sediments1. This is important in regulating marine carbon cycling and ocean–atmosphere CO2 exchange2. The present rise in atmospheric CO2 levels3 causes significant changes in surface ocean pH and carbonate chemistry4. Such changes have been shown to slow down calcification in corals and coralline macroalgae5,6, but the majority of marine calcification occurs in planktonic organisms. Here we report reduced calcite production at increased CO2 concentrations in monospecific cultures of two dominant marine calcifying phytoplankton species, the coccolithophorids Emiliania huxleyi and Gephyrocapsa oceanica . This was accompanied by an increased proportion of malformed coccoliths and incomplete coccospheres. Diminished calcification led to a reduction in the ratio of calcite precipitation to organic matter production. Similar results were obtained in incubations of natural plankton assemblages from the north Pacific ocean when exposed to experimentally elevated CO2 levels. We suggest that the progressive increase in atmospheric CO2 concentrations may therefore slow down the production of calcium carbonate in the surface ocean. As the process of calcification releases CO2 to the atmosphere, the response observed here could potentially act as a negative feedback on atmospheric CO2 levels.
D: The people should have the upper hand and they should have the upper hand for their own destiny and that's why we two, have gone as far as what we have to expose the NSSM200 report which was put in during the Ford administration, which I believe was written by Dr. Henry Kissinger, wherein he suggested the possible use of food as a weapon and its use against, in fact, as a tool against, the third world.
...
Now, at the same time we notice that is a correlation going with findings from the IPCC report concerning global warming that if the world average temperature rises, I believe between 2 and 3 degrees Celsius, that the Northern hemisphere, the higher latitude, growth will increase. However, if it goes over that it will decrease. Yet the lower latitudes ... by the way that's where you find most of the third world countries ... the 2 to 3 degree Celsius increase will cause starvation and crop loss.
K: OK.
D: Now isn't this funny, how they're just allowing the global warming to increase through the provoking ... with the use of fossil fuels? Now I'm not saying that's the total cause. It's not. There are cycles involved, short as well as long term cycles. But isn't that funny? And it's my best guess that they'll probably order just enough ameliorative steps to be taken where it levels off where the higher latitudes probably don't lose their crops, where you find the majority of the rich countries.
K: Interesting. Well, that's actually a fascinating critical observation. I think that it is also interesting that most of the crops are being grown, though, in the lower latitudes. They're not being grown in North America anymore.
D: Right. But you have sustainability, though.
K: Sure.
D: Whereas when you have the loss of the crops in the lower latitudes you're also losing a lot of the population from the third world, which, unfortunately, according to the way that the documents read, some people find them expendable.
K: Right.
D: We don't feel that way.
K: That's the Iron Mountain report ... also talks about things of that nature. And you're familiar with that.
...
D: At the same time, I mean, you know, when we start hearing that the Codex [Alimentarius] is being placed in place which actually delimits food value. Oh, you can have all the food you want and starve to death while you're eating it if there's no nutrients.
K: Right. Absolutely.
D: When I start hearing that food is being used as a weapon and it's being used concerning the use of fossil fuels, I start getting personally angry. There's not one person in the lower latitudes that's worth any less than me.
K: Right. Right.
D: You know, everybody is worth exactly the same thing on this Earth and unfortunately there are individuals who feel otherwise.
Carbonic acid is therefore one of the weaker of the acids. I'm drinking it right now. We call it 'carbonated water'. Every time you open a bottle of carbonated drink, that fizz you hear is CO2 escaping from the water, due to the sudden drop in pressure. The CO2 is put into the water under extremely high pressures in a factory, and using concentrated CO2. The head on a beer is made up mostly of CO2 molecules escaping for the same reason, although they exist in beer due to the yeast action during the brewing process. Neither condition (extreme pressure or high CO2 concentration) exists in the open atmosphere. Do a little math, study a little chemistry, and the fear disappears.
When carbon dioxide dissolves in the ocean it lowers the pH, making the ocean more acidic. Owing to a paucity of relevant observations,we have a limited understanding of the effects of pH reduction on marine biota.Coral reefs, calcareous plankton and other organisms whose skeletons or shells contain calcium carbonate may be particularly affected. Most biota reside near the surface, where the greatest pH change would be expected to occur, but deep-ocean biota may be more sensitive to pH changes.
To investigate the effects of CO2 emissions on ocean pH, we forced the Lawrence Livermore National Laboratory ocean general-circulation model (Fig. 1a) with the pressure of atmospheric CO2 (pCO2) observed from 1975 to 2000, and with CO2 emissions from the Intergovernmental Panel on Climate Change’s IS92a scenario1 for 2000–2100.
Simulated atmospheric CO2 exceeds 1,900 parts per million (p.p.m.) at around the year 2300.
Source: www.pnas.org...
Increasing global concentrations of atmospheric CO2 are predicted to decrease ocean pH, with potentially severe impacts on marine food webs, but empirical data documenting ocean pH over time are limited.
Source: www.agu.org...
Mussel and oyster calcification may decrease by 25 and 10%, respectively, by the end of the century, following the IPCC IS92a scenario (∼740 ppmv in 2100). Moreover, mussels dissolve at pCO2 values exceeding a threshold value of ∼1800 ppmv.
Source: www.nature.com...
Diminished calcification led to a reduction in the ratio of calcite precipitation to organic matter production. Similar results were obtained in incubations of natural plankton assemblages from the north Pacific ocean when exposed to experimentally elevated CO2 levels. We suggest that the progressive increase in atmospheric CO2 concentrations may therefore slow down the production of calcium carbonate in the surface ocean. As the process of calcification releases CO2 to the atmosphere, the response observed here could potentially act as a negative feedback on atmospheric CO2 levels.
Redneck : I take your point about this but if the bottle of 'carbonated water' was released then subjected to a vacuum wouldn't more CO2 be released. Atmosphere is around 14.6psi at sea level so couldn't we assume that the sea is under atmosphere pressure and therefore could hold some amount of CO2.
Originally posted by TheRedneck
reply to post by melatonin
The difference is your links are mostly predictions, whereas I am stating established chemical data...
I think I have made my point. while at least the scientists involved with this report disclosed their procedure, this procedure is virtual only with no real-world testing to determine if the results are accurate, and the input data is questionable, coming from predictions by the IPCC. Now, should they decide to run some actual experiments, please let me know.
See if you can find a link to answer those questions and you might just convince me there's a problem.
Oh, and I guess I should point out... there were no mathematical calculations or specific input data values involved in your links, only qualitative results mixed with a hint of quantitative values. To truly review an experiment, one must know both the input data and the output data.
TheRedneck
The whole post you made before was just deflection and red herring. You criticise a number of scientific papers for being predictions, yet the studies use the same information that you are, but apply it to relevant real-world scenarios, rather than silly examples of beer bottles, lol.
And so rather than accept real science, with real maths, done by real scientists, your own wishful-thinking and basic Chem101 is given comparable weight
I don't have such fanciful ideas like convincing you of anything on this issue. Your posts in this thread clearly show you're beyond that.
The Wilkins Ice Shelf, a broad plate of floating ice south of South America on the Antarctic Peninsula, had been stable for most of the last century before it began retreating in the 1990s. The peninsula has been experiencing extraordinary warming in the past 50 years of 2.5°C.