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The WOC and marine carbon
trading
Monday, 18 May 2009
Indonesia's Maritime Affairs and Fisheries Ministry showed a strong
desire to propose marine carbon trading as an additional component in
the Clean Development Mechanism (CDM) during the just concluded World
Ocean Conference (WOC) in Manado, North Sulawesi. In other words, beside
forests, the Indonesian delegation wants the Indonesian seas to be
considered in carbon trading.
Will this proposal benefit the country?
Before finding out the proper answer, it is better to understand air-sea
carbon exchange and its controlling factors. There are four main
parameters: Partial pressure of CO2 (pCO2), dissolved inorganic carbon
(DIC), total alkalinity and pH. Although they interrelate in the ocean,
the reference parameter is pCO2. If pCO2 at the ocean's surface (SSpCO2)
is lower than pCO2 in the atmosphere, the surface of the ocean absorbs
atmospheric CO2, and vice versa. SSpCO2 itself is controlled by the sea
surface temperature (SST), so it varies from low to high latitudes.
SSpCO2 in tropical oceans is in general higher than in temperate ocean.
The mechanism of how the SST affects SSpCO2 can be illustrated with a
cup of Coke. Gas concentration in the Coke tends to disappear when the
cup is put under the Sun, compared to when it is put in a fridge. This
is what happens in dissolving CO2 in the ocean. Gas solubility in
temperate oceans is much higher, resulting in lower gas partial pressure
than in tropical oceans. This mechanism is known as the solubility pump.
On the other hand, photosynthesis by phytoplankton will reduce dissolved
CO2 in seawater. Organic matter production during photosynthesis will
sink to deeper layers (at depths of more than 1,000 meters) and will be
buried in the bottom sediment. This is called the biological pump.
However, the deposition of organic matter in shallow seas cannot be
categorized as a biological pump since the deposited sediment at the
bottom can be eroded by strong tidal currents. In this case, the organic
carbon can be released back into the water column.
Takahasi, a researcher at Columbia University's Lamont-Doherty Earth
Observatory, deals with the global SSpCO2 in several publications
dealing with carbon sources and sinks in tropical and temperate oceans.
Some regions, like middle-latitude oceans, are influenced by the
combination of solubility and biological pumps, depending on season and
ocean characteristics. Therefore, it should be noted that marine
photosynthesis will not directly uptake atmospheric CO2. The air-sea gas
exchange is determined by the four parameters, known as the marine
carbonate system.
The previous explanation clearly shows Indonesian seas tend to be a
carbon source. My research on the Java Sea and cruise data from the
Meteorological Research Institute of Japan along the Makassar Strait to
the Celebes Sea also reached a similar conclusion.
Regarding the carbon cycle and future climate system, the ocean
in general may play an important role. Sabine, a researcher at the
National Oceanic and Atmospheric Administration's (NOAA) Pacific Marine
Environmental Laboratory, reported in a publication in 2004 that from
the 1800s until 1994, the ocean removed about 118 Pg C (1 Pg=1015
grams). This is equal to about half of the CO2 released into the
atmosphere from the burning of fossil fuels. The carbon cycle during the
pre-industrial era is then determined by scientists as a natural cycle.
On the other hand, the emission of CO2 after the industrial era is
categorized as anthropogenic carbon. Concentrations of atmospheric CO2
during the pre-industrial era and now are about 280 ppm (parts per
million) and 380 ppm, respectively.
A decade ago, it was not clear what the fate of anthropogenic carbon in
the ocean was, particularly its spatial distribution. There was no
accurate method to determine the concentration of anthropogenic carbon
in the ocean. However, the method improved year by year. Then, a recent
paper by Gruber and his colleagues (published in February 2009) reported
a synthesis of oceanic sources, sinks and transport of atmospheric CO2,
including natural and anthropogenic carbon in the ocean. They concluded
the world's oceans now act as sinks for anthropogenic atmospheric CO2.
Their findings agree well with Sabine (2004). So the ocean in general
naturally acted as a carbon source during the pre-industrial era, but
changed into a sink due to anthropogenic perturbation.
Concerning marine carbon trading, one of the difficulties is related to
boundaries and transboundary currents. In addition, if the carbon
trading deals with the anthropogenic carbon cycle, then all marine
countries will benefit, because the entire oceans work as sinks.
However, it's not certain marine countries will benefit, since
the ocean becoming a carbon sink has a negative impact on marine
organisms (through marine acidification).
On the other hand, if carbon trading deal with the natural carbon
cycle, then countries located in tropical oceans, including Indonesia,
will have to pay the tax. However, this is impossible since the natural
carbon cycle occurred during the pre-industrial era.
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