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quote:as soon as we run out of fossil fuels, or stop using them, the temperature will begin to catastrophically drop. We have, remaining to us, 120 years, at best, left on this planet.
quote:Originally posted by crandlesRuddimann's view of pre-industrial global warming is a minority opinion. See http://en.wikipedia.org/wiki/Global_warmingThe more majority opinion is that the current interglacial was meant to be a long one so it wasn't supposed to have ended yet.
quote:CO2 levels are likely to stay at elevated levels for thousands of years after we stop using fossil fuels and I doubt we will have a sudden dramatic ceasation of use of fossil fuels. Even if that did happen the warmest period would be at least a decade or two later.
quote:Originally posted by another_someonequote:Originally posted by crandlesRuddimann's view of pre-industrial global warming is a minority opinion. See http://en.wikipedia.org/wiki/Global_warmingThe more majority opinion is that the current interglacial was meant to be a long one so it wasn't supposed to have ended yet.What interglacial - we are not in an interglacial - we are still in a trelatively very cold climate in comparison to most of geological time. There has been a slight rise in temperature above the minimum, but we are well short of being in a warm period.quote:CO2 levels are likely to stay at elevated levels for thousands of years after we stop using fossil fuels and I doubt we will have a sudden dramatic ceasation of use of fossil fuels. Even if that did happen the warmest period would be at least a decade or two later.How do you work out such a long period for CO2 recycling - I would have thought that given that even with the raised levels of CO2 in the atmosphere, they are still only a minute proportion of the amount of O2 (all of which is converted from CO2), that it should not take long at all for the any excess CO2 (of the very slight amount we talk about) to also be converted to O2.Even the web site you quote (which certainly does not look like it is trying to underplay the impact of global warming) only talks abot 50 to 200 years to recycle the CO2, and I personally would be surprised if it took as long as that (although I claim no expertise for behind that opinion).George
quote:Originally posted by crandles>What interglacial? We are at the left hand side of http://en.wikipedia.org/wiki/Image:Ice_Age_Temperature.pngSo we are warmer than most of the last 450,000 years.
quote:An ice age is a period of long-term downturn in the temperature of Earth's climate, resulting in an expansion of the continental ice sheets, polar ice sheets and mountain glaciers ("glaciation"). Glaciologically, ice age is often used to mean a period of ice sheets in the northern and southern hemispheres; by this definition we are still in an ice age (because the Greenland and Antarctic ice sheets still exist). More colloquially, when speaking of the last few million years, ice age is used to refer to colder periods with extensive ice sheets over the North American and Eurasian continents: in this sense, the last ice age ended about 10,000 years ago. This article will use the term ice age in the former, glaciological, sense; and use the term glacial periods for colder periods during ice ages and interglacial for the warmer periods.Many glacial periods have occurred during the last few million years, initially at 40,000-year frequency but more recently at 100,000-year frequencies. These are the best studied. There have been four major ice ages in the further past.
quote:Originally posted by crandlesIf you go back more than 5 million years http://en.wikipedia.org/wiki/Geologic_temperature_recordyes we are colder than most of geologic time but I think the last 450,000 years is more relevant than what happened over 5 million years ago.
quote:The earliest hypothesized ice age is believed to have occurred around 2.7 to 2.3 billion (109) years ago during the early Proterozoic Age.The earliest well-documented ice age, and probably the most severe of the last 1 billion years, occurred from 800 to 600 million years ago (the Cryogenian period) and it has been suggested that it produced a Snowball Earth in which permanent sea ice extended to or very near the equator. It has been suggested that the end of this ice age was responsible for the subsequent Cambrian Explosion, though this theory is recent and controversial.A minor ice age occurred from 460 to 430 million years ago, during the Late Ordovician Period.There were extensive polar ice caps at intervals from 350 to 260 million years ago, during the Carboniferous and early Permian Periods, associated with the Karoo Ice Age.The present ice age began 40 million years ago with the growth of an ice sheet in Antarctica, but intensified during the Pleistocene (starting around 3 million years ago) with the spread of ice sheets in the Northern Hemisphere. Since then, the world has seen cycles of glaciation with ice sheets advancing and retreating on 40,000 and 100,000 year time scales. The last glacial period ended about 10,000 years ago.
quote:Originally posted by crandles>How do you work out such a long period for CO2 recyclingTry http://www.realclimate.org/index.php/archives/2005/03/how-long-will-global-warming-last/A couple of hundred years is a typical lifetime estimate. However there is a small proportion that takes a long time to disappear.
quote:Thus land-based plant sequestration should not be regarded as permanent.
quote:Originally posted by crandlesNot sure what wasn't completely true :?
quote:I disagree that it is ignoring photosynthesis. It just happens to be not very relevant. At equilibrium plant photosynthesis is matched by plant decay, animal respiration and soil decomposition. If you add a slug of new CO2 to the atmosphere, for a brief period the land takes up more carbon. However the amount of carbon that can be taken up by land is limited and a new equilibrium will be reached. This is small compared with the ocean uptake. Between land and ocean around 75% is taken up in a short period of a few hundred years. The remaining 25% takes much longer.
quote:I don't see why you have to ask where the oxygen comes from. The oxygen in the atmosphere is a massive store that represents millions of years of turnover from O2 to CO2 and back. The turnover isn't important it is the net balance. It isn't the O2 we are interested in it is the carbon.
quote:A balance is only something we can ignore if we understand how that balance in maintained, and how it changes.
quote:If humans are creating lots of CO2 through combustion, then they must in fact be using up lots of O2. If you then make the assertion that O2 and CO2 are in permanent balance, then it must follow that there is a process where the O2 that the humans have used is somehow replenished
quote:The absorption of CO2 by the oceans and by carbonate rocks does little to maintain the balance between O2 and CO2 (the processes are happening without regard to the levels of O2 in the atmosphere, excepting insofar as you may judge that in the extreme, an anoxic environment would not support shellfish and other living forms that convert CO2 to carbonates).
quote:It has to be remembered that the only significant means of creating free oxygen on this planet is through photosynthesis, and so one must see the creation of free oxygen as a direct measure of the rate of photosynthesis, and the amount of free oxygen on the planet as a store of historic CO2 that has been converted to O2. Clearly, the turnover is critical in any assessment of the pricess, since it indicates how responsive the system may be to environmental changes.
quote:Originally posted by crandlesquote:If humans are creating lots of CO2 through combustion, then they must in fact be using up lots of O2. If you then make the assertion that O2 and CO2 are in permanent balance, then it must follow that there is a process where the O2 that the humans have used is somehow replenishedWhy would anyone make that assertion? We are trying to see what happens to CO2 so assuming a permanent balance seems very odd. If the O2 stock was changing significantly maybe that would have an effect on the processes of O2 to CO2 and CO2 to O2. However the stock of O2 is so hugeit is changing but not changing significantly.quote:The absorption of CO2 by the oceans and by carbonate rocks does little to maintain the balance between O2 and CO2 (the processes are happening without regard to the levels of O2 in the atmosphere, excepting insofar as you may judge that in the extreme, an anoxic environment would not support shellfish and other living forms that convert CO2 to carbonates). As O2 is not in balance but staying practically constant, any change in ratio of CO2 to O2 is due to changes in CO2. If ocean absorbtion is taking up 75% of the extra CO2 we are producing, how do you decide that is doing "little to maintain the balance"?I still don't see the relevance of O2.
quote:Originally posted by science_guyquote:CO2 levels are likely to stay at elevated levels for thousands of years after we stop using fossil fuels and I doubt we will have a sudden dramatic ceasation of use of fossil fuels. Even if that did happen the warmest period would be at least a decade or two later.part of the reason the temperature will drop is because of the lack of heat from the combustion of fossil fuels. The reactions do produce heat, and that is part of what has kept this planet warm. Without that, the temperature will fall, because the orbit that alters the earth enough to cause the ice age, is well into the cycle and it will not have the immediate benifit of hot sun.
quote:Originally posted by another_someoneI shall be brief, but merely try and clarify the following point:Atmospheric O2 is 209,460 ppmv Atmospheric CO2 is 381 ppmv If 0.18% of the O2 in the atmosphere is converted to CO2, that is a 100% rise in CO2. If all of the CO2 in the atmosphere were to be converted to O2, it would only represent 0.18% change in the volume of O2 in the atmosphere.Are we sure that the volume of O2 in the atmosphere has remained constant to within 0.1% (i.e. less that 1 part per thousand change in total volume, or more accurately, in the number of moles, since volume can also vary because of changes in temperature and pressure) tolerance over geological time (or even within recent times)?George
quote:Originally posted by science_guythe orbit cycles are entirely my point. The orbit cycle started to enter the ice age at b.c. 3000. That means the orbit has had 5000 years to change. Sure the burning of fossil fuels is negligible, but even negligible amounts can add up to be a dominating resource. The point is that humans will no longer be able to survive on the planet for very much long, regardless of how it happens.
quote:Originally posted by crandlesWhy do we want to be sure that the moles of O2 has remained constant to with .1%? That would hardly have much effect on CO2 to O2 or on O2 to CO2. If it was varying more than .1% what would that mean? Well it would probably be to do with other reactions other than the O2 to CO2 and CO2 to O2 reaction. Why? because we know CO2 has not changed by 50% or more recently.So what has this got to do with what we are discussing?
quote:While I accept that the simple argument that forests will convert CO2 to O2 is simplistic, because forests are a complex environment that is generally carbon neutral; but equally, one has to ask where did the oxygen come from
quote:Originally posted by crandlesI am no nearer to understanding why 'one has to ask where did the oxygen come from'.I think these numbers could be a little out of date. I think human fossil fuel use was 7GT several years ago so 5.5 looks a little on the low side. Despite this, I think we understand the processes well enough to make intelligent estimates of how the numbers will change as the CO2 level increases. Models suggest that the carbon in vegetation has been increasing but is likely to soon start decreasing.If the best way of measuring the CO2 level is from ice cores then I don't see why you have to bother with an non optimal method of trying to measure the O2 level or worrying about where the O2 comes from.
quote:Originally posted by another_someoneI, on the other hand, do not understand exactly what the image is trying to say (that a picture says a thousand words does not mean that the thousand words actually make any sense).How, in that picture, would you extract a total figure for all of the CO2 that is converted to O2 through photosynthesis (maybe I am just not looking at the right bot to see the number, and am simply being a total fool, but I cannot see the number).What are the margins of error for these figures?George