| Atmosphere Threatened By Pollutants Entering Ocean  Station, TX -- A large quantity of nitrogen compounds emitted into the 
    atmosphere by humans through the burning of fossil fuels and the use of 
    nitrogen fertilizers enters the oceans and may lead to the removal of some 
    carbon dioxide from the atmosphere, concluded a team of international 
    scientists led by Texas A&M University Distinguished Professor of 
    Oceanography and Atmospheric Sciences Robert Duce.
 The team of 30 experts from institutions around the world presented its 
    conclusions in the current issue of the journal Science.
 
 Human-caused atmospheric nitrogen compounds are carried by wind and 
    deposited into the ocean, where they act as a fertilizer and lead to 
    increased production of marine plant life. The increase in plant life causes 
    more carbon dioxide to be drawn from the atmosphere into the ocean. This 
    process results in the removal of about 10 percent of the human-caused 
    carbon dioxide in the atmosphere, thus potentially reducing the climate 
    warming potential, according to the team's paper.
 
 However, some of the nitrogen deposited in the ocean is re-processed to form 
    another nitrogen compound called nitrous oxide, which is then released back 
    into the atmosphere from the ocean. Nitrous oxide is a powerful greenhouse 
    gas itself – about 300 times more powerful per molecule than carbon dioxide 
    – thus cancelling out about two-thirds of the apparent gain from the carbon 
    dioxide removal, Duce explained. "But of course, the whole system is so 
    complex that we're still rather unsure about what some of the other impacts 
    might be within the ocean," he said.
 
 In most areas of the ocean, nitrogen is the nutrient that limits the 
    production of plant life, Duce said. So when all of the nitrogen in an area 
    of the surface ocean is used up, no more plant life forms in that area. The 
    team found that human-caused nitrogen deposits account for up to one-third 
    of the external input of nitrogen into the ocean, and this increase in 
    nitrogen available for the production of plant life causes more plants to 
    form, Duce explained.
 
 Oceanic plant life is produced from marine carbon (bicarbonate) in the 
    ocean, and that amount of bicarbonate is in equilibrium with the carbon 
    dioxide in the atmosphere. So when more bicarbonate is used up to produce 
    marine plant life, it disrupts the equilibrium, and carbon dioxide is drawn 
    down to the ocean from the atmosphere to restore the balance, Duce 
    explained.
 
 Thus, the human-caused nitrogen fertilization of the ocean removes some of 
    the most important greenhouse gas – carbon dioxide – from the atmosphere, 
    Duce said. This gain, however, is offset by the nitrogen compound, nitrous 
    oxide, that also forms in the ocean due to the nitrogen fertilization and is 
    re-emitted into the atmosphere as a powerful greenhouse gas, he added.
 
 "If you don't consider the impact of human-caused nitrogen when trying to 
    model climate change, you're missing a possibly significant part of the 
    overall carbon cycle as well as the nitrogen cycle," Duce said. "So nitrogen 
    deposition is potentially a very important factor in the climate change 
    issue."
 
 According to the team's calculations, about 54 million tons of nitrogen 
    produced from human activities entered the ocean from the atmosphere in the 
    year 2000. The team also found that the current nitrogen emissions are about 
    10 times what they were in 1860, Duce said. He added that the amount of 
    nitrogen entering the atmosphere is expected to rise in the coming decades 
    with the increase in demand for energy and fertilizers, and the team 
    estimates that by the year 2030, human-caused nitrogen emissions will have 
    risen to around 62 million tons per year.
 
 "Clearly, there is much that we do not know about the extent and timescale 
    of the impacts of this nitrogen deposition on the oceans and the subsequent 
    feedbacks to the climate system," Duce said. "The implications are complex 
    and interactive, and this is a very important issue that policy makers need 
    to address and that scientists trying to model and understand the future of 
    climate and climate change need to take into consideration."
 
 SOURCE: Texas A&M University
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