- Mar 22, 2004
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We have enough carbon based fossil fuels left to last a few hundred years, at most.
~Carbon comes from the earth, it gets cycled into the atmosphere, and gets returned to the earth. The cycle that this occurs naturally has been impacted by humans, and that can't be disputed. What it will do to the earth as we know it, is theory. The theory points towards a very high probability that it will alter the earths climate significantly, as we know it.
~Global warming is the Governments new Boogeyman. They want to force the private sector to spend trillions of dollars to stop and reverse our impact on the climate. Knowing full well that we can only control what goes on in our country.
~I think I have covered both sides of the basic argument. Personally, I know that global warming will not likely affect me in my lifetime, but I do have children. The probability of major climate change impacting them is to high for me to do nothing.
~I propose we look for methods to speed up what the earth does naturally, and on the cheap. I have contributed a method below. The impact of this fix would not be limited by our borders, and gives a true element of control. If you know of others, please contribute.
~
---------------------------------------------------------------------------------------
Here is one such method, on the cheap. If I could find a private company that sells carbon credits based on this technology, I would invest heavily in it.
Imagine if you will, growing the equivalent of a few million fully grown redwood trees in a matter of weeks, and how much carbon they could suck out of the atmosphere.
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Earth's carbon cycle is dominated by the ocean, which absorbs 50% of the CO2 released into the atmosphere by human activity. Carbon settling to the ocean bottom can eventually be stored for millions of years.
From Introduction to Climate Change United Nations Environmental Program's UNEP Global Resources Information Database (GRID) office in Arendal Norway.
The Oceanic Part of the Carbon Cycle
To understand the fate of CO2 in the atmosphere, we must understand earth's carbon cycle because atmospheric CO2 is only one part of the cycle. Several important oceanic processes influence the cycle. The figure above indicates that:
The ocean stores 50 times more carbon dioxide than does the atmosphere;
Much more carbon flows through the ocean than the amount produced by burning fossil fuels;
An amount of carbon equal to to the total amount stored in the atmosphere cycles through the ocean in about eight years [(750 GT) / (92 GT per year) = 8.3 years]; and
The flux in and out of the ocean is larger than the flux in and out of the land.
The carbon cycle in the ocean has two main parts, a physical part due to CO2 dissolving into sea water, and a biological part due to phytoplankton converting CO2 into carbohydrates.
Carbon dioxide dissolves into the ocean at high latitudes. CO2 is carried to the deep ocean by sinking currents, where it stays for hundreds of years. Eventually mixing brings the water back to the surface. The ocean emit carbon dioxide into the tropical atmosphere. This system of deep ocean currents is the marine physical pump for carbon. It help pumps carbon from the atmosphere into the sea for storage.
Global map of the average annual exchange CO2 flux (mol-C m-2 a-1) across the sea surface.
From Ocean Biogeochemistry and Global Change published by the International Geosphere Biosphere Program.
Phytoplankton in the ocean use CO2, sunlight, water, and nutrients and produce carbohydrates and oxygen. Animals eat the phytoplankton contributing to the oceanic food web leading to fish. Organic material sinks when phytoplankton and animals die, carrying some reduced carbon to the sea floor (Reduced carbon is carbon that can be oxidized to yield energy, water, and CO2.) A small fraction of the reduced carbon (0.4%) is eventually buried and stored in sediments for millions of years (Middelburg et al, 2007). But most of the reduced carbon in and below the sea floor is used by animals and bacteria, and returned to the ocean part of the carbon cycle. This is the marine biological pump for carbon. It too pumps carbon from the atmosphere into the sea for storage. To learn more about the biological pump, read the latest results of the International Geosphere Biosphere Program's Joint Global Ocean Flux Study of the carbon cycle in the ocean.
Global map of the primary productivity by oceanic phytoplankton.
From the International Geosphere Biosphere Program.
The storage of reduced carbon in oceanic sediments in sediments maintains the oxygen content of the atmosphere. If no reduced carbon were stored in sediments, atmospheric oxygen would be used up in about 15 million years.
It's a popular misconception that the concentration of oxygen in Earth's atmosphere is controlled by photosynthesis. Photosynthesis is certainly the source of atmospheric oxygen, but the amount it produces is in almost perfect balance with the amount consumed through the respiration of living organisms. It is only when organic matter is buried in ocean sediments, and so ceases to be decomposed, that atmospheric oxygen can accumulate. This burial process also reduces the levels of the greenhouse gas carbon dioxide released into the atmosphere. The exact rate of organic-matter burial is therefore a significant determinant of atmospheric composition, and thus global climate, over geological timescales.
From Masiello (2007).
Animals in the ocean use carbohydrates and oxygen and emit CO2. Plants respire CO2 during the night. As a result, all the oxygen produced by phytoplankton is used to converted to reduced carbon into carbon dioxide except for the small amount of reduced carbon stored in sediments.
Recently, people started burning fossil fuels, which released, in the form of CO2, the carbon produced by plants and stored as reduced carbon (now in the form of coal, oil, and gas) in sediments millions of years ago.
Thus burning of fossil fuels is a source of CO2 and the ocean is a sink of CO2. To learn more about what happens to CO2 released into the atmosphere, read the paper on Sinks for Anthropogenic Carbon in the August 2002 issue of Physics Today. The plot of fluxes is particularly useful.
Look at some images of chlorophyll distribution in the ocean to see where phytoplankton (microscopic floating plants) are common in the ocean. The Ocean Color home page has a nice animation of the seasonal cycle of phytoplankton concentration in the ocean.
Increasing the Oceanic Absorption of CO2
If the carbon cycle in the ocean processes so much more carbon than does the atmospheric part, can the oceanic part be enhanced to cause the ocean to store more carbon? After all, a small change in the storage rate could absorb all the carbon dioxide released by the burning of fossil fuels. John Martin proposed a way to do this.
?Give me a half tanker of iron, and I will give you an ice age.??John Martin.
Martin noticed that large areas of the ocean have sufficient nutrients to support the growth of large populations of phytoplankton, yet these areas have small populations of phytoplankton. He called these areas high-nutrient, low-chlorophyll zones (HNLCs). On further investigation, Martin determined the HNLC zones were deficient in iron, a micro-nutrient essential for life. Johnson then proposed that adding small amounts of iron to these regions would greatly increase productivity. This is the iron hypothesis.
Several recent experiments, including the Southern Ocean Iron Release Experimen, show the hypothesis is correct. Small amounts of iron in the right regions lead to larges increases in phytoplankton. One kilogram of iron leads to the production of 5,000 to 20,000 kilograms of phytoplankton.
Read about John Martin and his iron hypothesis, including all the information in links to his work shown on the right side of the web page. For a more controversial look at this solution to the CO2 problem, read the Wired Magazine article on Dumping Iron.
Oceanic Phytoplankton
Most of the primary production in the ocean is by single-celled microscopic organisms. The organisms include:
The Chromista, including Coccolithophorids, and Diatoms,
Dinoflagellates. And,
Photosynthetic bacteria and archaea.
To learn more about the micro-organisms in the ocean, read Marine Food Webs and Microbial Food Webs.
References
Masiello, C. A. (2007). Carbon cycle: Quick burial at sea. Nature 450 (7168): 360-361.
Middelburg, J. J. and F. J. R. Meysman (2007). OCEAN SCIENCE: Burial at Sea. Science 316 (5829): 1294-1295.
~Carbon comes from the earth, it gets cycled into the atmosphere, and gets returned to the earth. The cycle that this occurs naturally has been impacted by humans, and that can't be disputed. What it will do to the earth as we know it, is theory. The theory points towards a very high probability that it will alter the earths climate significantly, as we know it.
~Global warming is the Governments new Boogeyman. They want to force the private sector to spend trillions of dollars to stop and reverse our impact on the climate. Knowing full well that we can only control what goes on in our country.
~I think I have covered both sides of the basic argument. Personally, I know that global warming will not likely affect me in my lifetime, but I do have children. The probability of major climate change impacting them is to high for me to do nothing.
~I propose we look for methods to speed up what the earth does naturally, and on the cheap. I have contributed a method below. The impact of this fix would not be limited by our borders, and gives a true element of control. If you know of others, please contribute.
~
---------------------------------------------------------------------------------------
Here is one such method, on the cheap. If I could find a private company that sells carbon credits based on this technology, I would invest heavily in it.
Imagine if you will, growing the equivalent of a few million fully grown redwood trees in a matter of weeks, and how much carbon they could suck out of the atmosphere.
----------------------------------------------------------------------------------------
Earth's carbon cycle is dominated by the ocean, which absorbs 50% of the CO2 released into the atmosphere by human activity. Carbon settling to the ocean bottom can eventually be stored for millions of years.
From Introduction to Climate Change United Nations Environmental Program's UNEP Global Resources Information Database (GRID) office in Arendal Norway.
The Oceanic Part of the Carbon Cycle
To understand the fate of CO2 in the atmosphere, we must understand earth's carbon cycle because atmospheric CO2 is only one part of the cycle. Several important oceanic processes influence the cycle. The figure above indicates that:
The ocean stores 50 times more carbon dioxide than does the atmosphere;
Much more carbon flows through the ocean than the amount produced by burning fossil fuels;
An amount of carbon equal to to the total amount stored in the atmosphere cycles through the ocean in about eight years [(750 GT) / (92 GT per year) = 8.3 years]; and
The flux in and out of the ocean is larger than the flux in and out of the land.
The carbon cycle in the ocean has two main parts, a physical part due to CO2 dissolving into sea water, and a biological part due to phytoplankton converting CO2 into carbohydrates.
Carbon dioxide dissolves into the ocean at high latitudes. CO2 is carried to the deep ocean by sinking currents, where it stays for hundreds of years. Eventually mixing brings the water back to the surface. The ocean emit carbon dioxide into the tropical atmosphere. This system of deep ocean currents is the marine physical pump for carbon. It help pumps carbon from the atmosphere into the sea for storage.
Global map of the average annual exchange CO2 flux (mol-C m-2 a-1) across the sea surface.
From Ocean Biogeochemistry and Global Change published by the International Geosphere Biosphere Program.
Phytoplankton in the ocean use CO2, sunlight, water, and nutrients and produce carbohydrates and oxygen. Animals eat the phytoplankton contributing to the oceanic food web leading to fish. Organic material sinks when phytoplankton and animals die, carrying some reduced carbon to the sea floor (Reduced carbon is carbon that can be oxidized to yield energy, water, and CO2.) A small fraction of the reduced carbon (0.4%) is eventually buried and stored in sediments for millions of years (Middelburg et al, 2007). But most of the reduced carbon in and below the sea floor is used by animals and bacteria, and returned to the ocean part of the carbon cycle. This is the marine biological pump for carbon. It too pumps carbon from the atmosphere into the sea for storage. To learn more about the biological pump, read the latest results of the International Geosphere Biosphere Program's Joint Global Ocean Flux Study of the carbon cycle in the ocean.
Global map of the primary productivity by oceanic phytoplankton.
From the International Geosphere Biosphere Program.
The storage of reduced carbon in oceanic sediments in sediments maintains the oxygen content of the atmosphere. If no reduced carbon were stored in sediments, atmospheric oxygen would be used up in about 15 million years.
It's a popular misconception that the concentration of oxygen in Earth's atmosphere is controlled by photosynthesis. Photosynthesis is certainly the source of atmospheric oxygen, but the amount it produces is in almost perfect balance with the amount consumed through the respiration of living organisms. It is only when organic matter is buried in ocean sediments, and so ceases to be decomposed, that atmospheric oxygen can accumulate. This burial process also reduces the levels of the greenhouse gas carbon dioxide released into the atmosphere. The exact rate of organic-matter burial is therefore a significant determinant of atmospheric composition, and thus global climate, over geological timescales.
From Masiello (2007).
Animals in the ocean use carbohydrates and oxygen and emit CO2. Plants respire CO2 during the night. As a result, all the oxygen produced by phytoplankton is used to converted to reduced carbon into carbon dioxide except for the small amount of reduced carbon stored in sediments.
Recently, people started burning fossil fuels, which released, in the form of CO2, the carbon produced by plants and stored as reduced carbon (now in the form of coal, oil, and gas) in sediments millions of years ago.
Thus burning of fossil fuels is a source of CO2 and the ocean is a sink of CO2. To learn more about what happens to CO2 released into the atmosphere, read the paper on Sinks for Anthropogenic Carbon in the August 2002 issue of Physics Today. The plot of fluxes is particularly useful.
Look at some images of chlorophyll distribution in the ocean to see where phytoplankton (microscopic floating plants) are common in the ocean. The Ocean Color home page has a nice animation of the seasonal cycle of phytoplankton concentration in the ocean.
Increasing the Oceanic Absorption of CO2
If the carbon cycle in the ocean processes so much more carbon than does the atmospheric part, can the oceanic part be enhanced to cause the ocean to store more carbon? After all, a small change in the storage rate could absorb all the carbon dioxide released by the burning of fossil fuels. John Martin proposed a way to do this.
?Give me a half tanker of iron, and I will give you an ice age.??John Martin.
Martin noticed that large areas of the ocean have sufficient nutrients to support the growth of large populations of phytoplankton, yet these areas have small populations of phytoplankton. He called these areas high-nutrient, low-chlorophyll zones (HNLCs). On further investigation, Martin determined the HNLC zones were deficient in iron, a micro-nutrient essential for life. Johnson then proposed that adding small amounts of iron to these regions would greatly increase productivity. This is the iron hypothesis.
Several recent experiments, including the Southern Ocean Iron Release Experimen, show the hypothesis is correct. Small amounts of iron in the right regions lead to larges increases in phytoplankton. One kilogram of iron leads to the production of 5,000 to 20,000 kilograms of phytoplankton.
Read about John Martin and his iron hypothesis, including all the information in links to his work shown on the right side of the web page. For a more controversial look at this solution to the CO2 problem, read the Wired Magazine article on Dumping Iron.
Oceanic Phytoplankton
Most of the primary production in the ocean is by single-celled microscopic organisms. The organisms include:
The Chromista, including Coccolithophorids, and Diatoms,
Dinoflagellates. And,
Photosynthetic bacteria and archaea.
To learn more about the micro-organisms in the ocean, read Marine Food Webs and Microbial Food Webs.
References
Masiello, C. A. (2007). Carbon cycle: Quick burial at sea. Nature 450 (7168): 360-361.
Middelburg, J. J. and F. J. R. Meysman (2007). OCEAN SCIENCE: Burial at Sea. Science 316 (5829): 1294-1295.