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Gwen Noda

Nature Conservancy Magazine: Winter 2010 - A Guide to Our Oceans - 2 views

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    A Guide to Our Oceans
Gwen Noda

Governments refusal to address ocean acidification. - Sacramento Political Buzz | Exami... - 0 views

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    Global warming…the Earth is steadily getting warmer. The why is it getting warmer question will solicit so many theories that it would drive one mad to sort through them all. Global warming itself is sort of a misnomer; it is a symptom of the problem, not the cause. The cause for all the debate is whether or not the atmospheric increase of CO2 gas over the last two-hundred years has affected the Earth's climate. Recently scientists have discovered another reason to be concerned about the increasing level of atmospheric CO2. It is startling that the media and science has hardly touched upon ocean acidification. It would not be surprising if you have never heard this term. A LexisNexis search of the news wire services found in the past week there were 348 articles that mentioned global warming. Three articles contained ocean acidification. In the last 2 years, a LexisNexis search of all sources found a mere 216 articles that mentioned ocean acidification. That is a worldwide search of newspapers, magazines and wire services. The New York Times did not mention it a single time, but they ran so many Global Warming articles that there were too many matches for the page to display.
Gwen Noda

Science News for Kids: Home Page - 0 views

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    "Since 2003, this online sibling to Science News - the award-winning magazine - has been at the forefront of science education. It highlights developments from all science disciplines, delivering the information to the screens of computers in schools and households across the world."
Gwen Noda

Science Magazine: Sign In - 0 views

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    Keeping Coral Clean Seaweed overgrowth is a major problem for coral reefs and also seems to be a consequence of excessive harvesting of herbivorous fish. Dixson and Hay (p. 804) examined this effect on Fijian reefs. Species of small herbivorous gobies and coral-associated damselfish were compared for their effect on the toxic Chlorodesmis seaweed in experiments that required caging colonies of the branching coral Acropora nasuta and the associated fish species. Only the gobies actively removed algal fronds attached to the cages and only one species (itself toxic to predators) ate them; the damselfish simply defected from the arena when toxic algae were present. The hydrophobic toxins exuded in the algal mucus lysed coral polyps releasing cell constituents that, together with the algal toxin, attract the gobies, which then eat the algal fronds. Interestingly, the toxic goby became more toxic to predators after consumption of the seaweed, which may help to drive symbiosis with a coral colony.
Gwen Noda

Science Magazine: Sign In - 0 views

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    Warming and Melting Mass loss from the ice sheets of Greenland and Antarctica account for a large fraction of global sea-level rise. Part of this loss is because of the effects of warmer air temperatures, and another because of the rising ocean temperatures to which they are being exposed. Joughin et al. (p. 1172) review how ocean-ice interactions are impacting ice sheets and discuss the possible ways that exposure of floating ice shelves and grounded ice margins are subject to the influences of warming ocean currents. Estimates of the mass balance of the ice sheets of Greenland and Antarctica have differed greatly-in some cases, not even agreeing about whether there is a net loss or a net gain-making it more difficult to project accurately future sea-level change. Shepherd et al. (p. 1183) combined data sets produced by satellite altimetry, interferometry, and gravimetry to construct a more robust ice-sheet mass balance for the period between 1992 and 2011. All major regions of the two ice sheets appear to be losing mass, except for East Antarctica. All told, mass loss from the polar ice sheets is contributing about 0.6 millimeters per year (roughly 20% of the total) to the current rate of global sea-level rise.
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