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Originally posted by melatonin
And the important thing is that oceans and terrestrial biosphere are removing CO2. The increase is human sourced. If you don't want to accept 100%, which it is, then 95% is a fair number.
Originally posted by melatonin
It might well be, but that isn't so important. If you check the figures I posted above, the biosphere exchanges similar amounts (the amount released is taken up back up). We are adding an extra chunk, that is where the increase is coming from, a lot of the anthropogenic emissions are taken up in the biosphere. The rest is accumulating.
Are we overlooking potential abrupt climate shifts?
Most of the studies and debates on potential climate change, along with its ecological and economic impacts, have focused on the ongoing buildup of industrial greenhouse gases in the atmosphere and a gradual increase in global temperatures. This line of thinking, however, fails to consider another potentially disruptive climate scenario. It ignores recent and rapidly advancing evidence that Earth’s climate repeatedly has shifted abruptly and dramatically in the past, and is capable of doing so in the future.
Fossil evidence clearly demonstrates that Earthvs climate can shift gears within a decade, establishing new and different patterns that can persist for decades to centuries. In addition, these climate shifts do not necessarily have universal, global effects. They can generate a counterintuitive scenario: Even as the earth as a whole continues to warm gradually, large regions may experience a precipitous and disruptive shift into colder climates.
Science 31 March 2000:
Vol. 287. no. 5462, pp. 2467 - 2470
DOI: 10.1126/science.287.5462.2467
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Reports
Global Carbon Sinks and Their Variability Inferred from Atmospheric O2 and 13C
M. Battle, 1* M. L. Bender, 1 P. P. Tans, 2 J. W. C. White, 3 J. T. Ellis, 4 T. Conway, 2 R. J. Francey 5
Recent time-series measurements of atmospheric O2 show that the land biosphere and world oceans annually sequestered 1.4 ± 0.8 and 2.0 ± 0.6 gigatons of carbon, respectively, between mid-1991 and mid-1997. The rapid storage of carbon by the land biosphere from 1991 to 1997 contrasts with the 1980s, when the land biosphere was approximately neutral. Comparison with measurements of 13CO2 implies an isotopic flux of 89 ± 21 gigatons of carbon per mil per year, in agreement with model- and inventory-based estimates of this flux. Both the 13C and the O2 data show significant interannual variability in carbon storage over the period of record. The general agreement of the independent estimates from O2 and 13C is a robust signal of variable carbon uptake by both the land biosphere and the oceans.
Science 2 November 2001:
Vol. 294. no. 5544, pp. 1012 - 1013
DOI: 10.1126/science.1065307
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Perspectives
CLIMATE CHANGE:
Storing Carbon on Land
R. J. Scholes and I. R. Noble*
Each year, about 120 PgC (1 PgC = 1015 g of carbon) is exchanged in each direction between terrestrial ecosystems and the atmosphere; another 90 PgC is exchanged between ocean and atmosphere. For comparison, 6.3 PgC is emitted by burning fossil fuels, about half of which is taken up again by the biosphere within years to a decade (1). This net uptake, or "sink," is currently fairly evenly split between land and ocean, but the uptake processes are different, as are projected future behaviors of the two sinks.
Title: OCEANIC UPTAKE OF FOSSIL-FUEL CO2 - C-13 EVIDENCE
Author(s): QUAY PD, TILBROOK B, WONG CS
Source: SCIENCE 256 (5053): 74-79 APR 3 1992
Document Type: Article
Language: English
Cited References: 23 Times Cited: 224
Abstract: The delta-C-13 value of the dissolved inorganic carbon in the surface waters of the Pacific Ocean has decreased by about 0.4 per mil between 1970 and 1990. This decrease has resulted from the uptake of atmospheric CO2 derived from fossil fuel combustion and deforestation. The net amounts of CO2 taken up by the oceans and released from the biosphere between 1970 and 1990 have been determined from the changes in three measured values: the concentration of atmospheric CO2, the delta-C-13 of atmospheric CO2 and the delta-C-13 value of dissolved inorganic carbon in the ocean. The calculated average net oceanic CO2 uptake is 2.1 gigatons of carbon per year. This amount implies that the ocean is the dominant net sink for anthropogenically produced CO2 and that there has been no significant net CO2 released from the biosphere during the last 20 years.
Originally posted by Mauddib]The fact is that temperatures and CO2 have different levels of fluctuations between the different Climate Changes that occur on Earth.
The longer periods of fluctuations happen in millions of years, and during these periods temperatures change 10C, and CO2 levels have changed from around 280 ppm to over 7,000 ppm.
Originally posted by Mauddib]One of those large periods was the Jurassic which was about 210 million years ago or so. At the beginning of this time period temperatures were much higher than today, about an average 22C, and CO2 levels were a bit over 1,000 ppm, yet there was plant life and animal life.
For over 50 millions years there was fluctuation in temperatures, but the bigger fluctuations were in CO2 levels, almost at the end of the Jurassic CO2 levels shot up about 1,000 ppm, yet temperatures did not raise much, but in fact two thirds into the Jurassic, temperatures began plummeting down, CO2 levels went down slowly and then went up again meanwhile temperatures were still going down, then as temperatures began to increase CO2 levels actually decreased once again, and they went from about 2,100 ppm to 900 ppm, meanwhile temperatures did not change that dramatically.
Originally posted by Mauddib]During the entire Cretacious period there were some fluctuations in temperatures and CO2 levels, but the changes between these smaller periods were not as dramatic -, yet CO2 levels on the overall decreased during this entire time period, and CO2 levels continued to decrease even almost until the middle of the Tertiary period, millions of years later. Only about over 100 million years later did temperatures actually decrease dramatically until they reached the present period.
Originally posted by melatonin
Radiative energy comes at different energies - the electromagnetic spectrum. GHGs absorb strongly at particular wavelengths. The wavelengths that are not absorbed, or not so strongly absorbed, are readily emitted back to space.
Originally posted by melatonin
[edit on 14-4-2007 by melatonin]
Originally posted by darkbluesky
I can grasp the methodology behind atmospheric composition reconstruction, but how did these researchers determine historical temps?
Originally posted by melatonin the reconstructions are derived from temperature proxies. Obviously the observed climate records only go back a couple hundred of years. So, to get an indication of temperatures going back to these timescales, the paleoclimatologists use indirect measures. The proxies used are highly correlated with temperature and include: tree rings, corals, ice cores, sediments etc.
Originally posted by skyblueff0
5) How effective is water vapor in aborbing heat?
Originally posted by darkbluesky
Isn't that like trying to determine how many people were at yesterdays baseball game by counting the number of beer cups and peanut bags in the trash?
Originally posted by skyblueff0
Can you provide me link of the sources u got ur answer from? My questions are:
1) How much do carbon dioxide gas do human contribute annually?
-Energy Information Administration says 6.5 billion tons
-Wikipedia says 24 billion tons
2) How much carbon dioxide is recycle through the photosythesis process of trees and plants each year?
3) How much greenhouse gases does volcanos produce?
-One source says 110 billion tons
-The other says 10 billion tons
Science 2 November 2001:
Vol. 294. no. 5544, pp. 1012 - 1013
DOI: 10.1126/science.1065307
Prev | Table of Contents | Next
Perspectives
CLIMATE CHANGE:
Storing Carbon on Land
R. J. Scholes and I. R. Noble*
Each year, about 120 PgC (1 PgC = 10 15 g of carbon) is exchanged in each direction between terrestrial ecosystems and the atmosphere; another 90 PgC is exchanged between ocean and atmosphere. For comparison, 6.3 PgC is emitted by burning fossil fuels, about half of which is taken up again by the biosphere within years to a decade (1). This net uptake, or "sink," is currently fairly evenly split between land and ocean, but the uptake processes are different, as are projected future behaviors of the two sinks.
4) How many tons of carbon dioxide gases are stored in the ocean due to the Solubility Cycle each year?
-One of my sources say that the concentration level of Carbon Dioxide in the ocean is 50 times higher than the levels in the atmosphere, but thats to vague for me.
Science 31 March 2000:
Vol. 287. no. 5462, pp. 2467 - 2470
DOI: 10.1126/science.287.5462.2467
Prev | Table of Contents | Next
Reports
Global Carbon Sinks and Their Variability Inferred from Atmospheric O2 and 13C
M. Battle, 1* M. L. Bender, 1 P. P. Tans, 2 J. W. C. White, 3 J. T. Ellis, 4 T. Conway, 2 R. J. Francey 5
Recent time-series measurements of atmospheric O2 show that the land biosphere and world oceans annually sequestered 1.4 ± 0.8 and 2.0 ± 0.6 gigatons of carbon, respectively, between mid-1991 and mid-1997. The rapid storage of carbon by the land biosphere from 1991 to 1997 contrasts with the 1980s, when the land biosphere was approximately neutral. Comparison with measurements of 13CO2 implies an isotopic flux of 89 ± 21 gigatons of carbon per mil per year, in agreement with model- and inventory-based estimates of this flux. Both the 13C and the O2 data show significant interannual variability in carbon storage over the period of record. The general agreement of the independent estimates from O2 and 13C is a robust signal of variable carbon uptake by both the land biosphere and the oceans.
5) How effective is water vapor in aborbing heat?
Originally posted by skyblueff0
hey long lance and melatonin, thank you replying to my questions and informing me!!
by the way, hey melatonin, where did you get those sources from, it seems to me from academic journal, but I might be able to access them, through my school.
Would you suggest I change my information and sources in the paper (arguing human aren't the main cause of Global Warming)? OR...
Do you suggest I wait and use this sources to counter act statements from previous paper for my next paper, due to be written this weekend (arguing human are the main cause of Global warming.)?
Originally posted by melatonin
OK, you still need to answer these points.
6.2 GtC per year released into the atmosphere between 1991-1997 by humans. Where did it go?
2.8 Gtc per year increased in the atmosphere. Where did it come from?
Originally posted by melatonin
The oceans and terrestrial biosphere are removing CO2. There is no net release from these sources.
Global Variations in Oceanic CO2
The figures illustrate the horizontal and vertical changes in oceanic CO2 levels observed in the Indian Ocean. Fluctuations in these CO2 levels in the upper ocean can be 10 to 100 times more than the annual anthropogenic increase. Therefore researchers have to make hundreds of thousands of CO2 measurements to accurately distinguish the natural variability from the CO2 increase due to rising atmospheric concentrations.
Originally posted by melatonin
120 PgC is exchanged by terrestrial. 90PgC exchanged by oceans. There is no overall release by these sources. What they emit, they absorb. That is why CO2 levels were pretty stable for the 800 years before we emitted millions of tonnes of CO2.
Originally posted by melatonin
Are you seriously trying to say that 0.1% of the 2.8GtC per year for 1991-1997 is anthropogenic, when we actually released 6.2GtC per year?
Originally posted by melatonin
Also, muaddib, why are you still presenting cartoon graphics with little idea of their source? I provided a nice peer-reviewed figure from Briffa & Osborne (2002) you could use for the last 1000 years:
Accumulation and 18O records for ice cores from Quelccaya ice cap. The period of the Little Ice Age stands out clearly as an interval of colder temperature (lower 18O) and higher accumulation. Such evidence demonstrates the Little Ice Age was a climatic episode of global significance. From World Data Center for Paleoclimatology (educational slide set).
Climatic changes during the past 1300 years as deduced from the sediments of Lake Nakatsuna, central Japan
Authors
D. P. Adhikari, F. Kumon
Abstract
Limnological features and sediment characteristics were studied in Lake Nakatsuna, a mesotrophic lake in central Japan. The lake is dimictic, and is anoxic in the hypolimnion during thermal stratification from May to September. In an attempt to reconstruct paleoclimatic changes around the lake, a sediment core taken from the lake center spanning the past 1300 years was analyzed for its organic and inorganic contents. Climatic influences were examined on the variation of total organic carbon (TOC), total nitrogen (TN), and sand contents. Short- and long-term fluctuations in TOC, TN, and sand contents are evident, and variation in atmospheric temperature appears to be important for their long-term variability.
The sediment record from AD 900 to 1200 indicates hot summers and warm winters with less snow accumulation, whereas the record from AD 1200 to 1950 is characterized by high variation of temperature, with three cool phases from AD 1300 to 1470, 1700 to 1760, and 1850 to 1950. The warm period from AD 900 to 1200 corresponds well to the Medieval Warm Period, and the second and third cool phases are related to the Little Ice Age.
Originally posted by melatonin
Wouldn't like to think you want to mislead people..
Study: Lake Superior Warming Quickly
(AP) -- Lake Superior has been warming even faster than the climate around it since the late 1970s due to reduced ice cover, according to a study by professors at the University of Minnesota Duluth.
Summer surface temperatures on the famously cold lake have increased about 4.5 degrees since 1979, compared with about a 2.7-degree increase in the region's annual average air temperature, the researchers found. The lake's "summer season" is now beginning about two weeks earlier than it did 27 years ago.
................
The study was first published by the American Geophysical Union on March 23.
Originally posted by melatonin
..............
Most research suggests we are having a significant impact, whether we are the main cause is more debatable (i.e. we outweigh other effects). We are a cause.
Originally posted by Muaddib
Already done that... Some of it is anthropogenic, a great part is natural.... Again, in warming cycles there is an increase of atmosphereic gases such as CO2 and H2Ov. Another fact you keep trying to avoid talking about...
Cartoon graphics with no idea of the source?... These graphs have been used by several sources I have given in the past.
vathena.arc.nasa.gov...
Originally posted by melatonin
Show me evidence that this is the case.
All you have done is hand-waved. I've presented evidence that the oceans and terrestrial biosphere are net sinks not net sources of CO2. You need to show that they are losing more CO2 than they are taking up.
Originally posted by melatonin
Between 1991-1997 human sources emitted (6.2GtC), more than twice what is accumulating (2.8GtC). The ocean removed 2.0GtC, the land 1.4GtC. Do the maths.
Originally posted by melatonin
That webpage is using data from 1995, the webpage hasn't been updated for 10 years. Figures. You need to keep up.
The blue line represents the Northern Hemispheric temperature history as constructed by Esper’s research team (source: Esper et al., 2002).
Patrick J. Michaels
Senior Fellow in Environmental Studies
Pat Michaels is a senior fellow at the Cato Institute and a research professor of environmental sciences at the University of Virginia. According to Nature magazine, Michaels is one of the most popular lecturers in the nation on the subject of global warming. He is a past president of the American Association of State Climatologists and was program chair for the Committee on Applied Climatology of the American Meteorological Society. Michaels is a contributing author and reviewer of the United Nations Intergovernmental Panel on Climate Change. He was an author of the 2003 climate science "Paper of the Year" awarded by the Association of American Geographers, for the demonstration that urban heat-related mortality declined significantly as cities became warmer. His writing has been published in the major scientific journals, including Climate Research, Climatic Change, Geophysical Research Letters, Journal of Climate, Nature, and Science; and his articles have appeared also in the Washington Post, the Washington Times, the Philadelphia Inquirer, the Wall Street Journal, the Los Angeles Times, USA Today, Houston Chronicle, and the Journal of Commerce. He has appeared on ABC, NPR's All Things Considered, PBS, Fox News Channel, CNN, MSNBC, CNBC, BBC and Voice of America. He holds A.B. and S.M. degrees in biological sciences and plant ecology from the University of Chicago, and he received his Ph.D. in ecological climatology from the University of Wisconsin at Madison in 1979.
Originally posted by Muaddib
The evidence is in the fact that in the past nature has released more CO2 than present levels of CO2 melatonin....
And the upper oceans can have fluctuations in the uptake and sink of CO2 of 10 to 100 times that of all anthropogenic CO2 released in a year....
The figures illustrate the horizontal and vertical changes in oceanic CO2 levels observed in the Indian Ocean. Fluctuations in these CO2 levels in the upper ocean can be 10 to 100 times more than the annual anthropogenic increase. Therefore researchers have to make hundreds of thousands of CO2 measurements to accurately distinguish the natural variability from the CO2 increase due to rising atmospheric concentrations.
Dr. John Holdren of Harvard University told the U.S. Senate Republican Policy Committee, "Michaels is another of the handful of U.S. climate-change contrarians... He has published little if anything of distinction in the professional literature, being noted rather for his shrill op-ed pieces and indiscriminate denunciations of virtually every finding of mainstream climate science."