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What is Haze?

Haze is caused when sunlight encounters tiny pollution particles in the air. Some light is absorbed by particles. Other light is scattered away before it reaches an observer. More pollutants mean more absorption and scattering of light, which reduce the clarity and color of what we see. Some types of particles such as sulfates, scatter more light, ...

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Haze
Physics

The Fourth State of Matter

There are three classic states of matter: solid, liquid, and gas; however, plasma is considered by some scientists to be the fourth state of matter. The plasma state is not related to blood plasma, ... Continue reading

ForthState
Astronomy

The Devil's In The Details

Did you ever make a mistake converting English numbers to metric numbers? Let's hope that your mistake didn't cost anyone $125 million dollars. That's what happened to NASA. The Mars Climate Orbiter's ... Continue reading

TheDevilsInTheDetails
Physics

Your Serve

NASA is well known for developing technology that makes things better, so can you believe that NASA actually did research on how to make tennis balls slower? ... Continue reading

YourServe
Astronomy

X-ray Telescopes

X-rays are a highly energetic form of light, not visible to human eyes. Light can take on many forms -- including radio waves, microwaves, infrared, visible, ultraviolet, X-ray and gamma radiation. ... Continue reading

XrayTelescopes

Arctic Carbon a Potential Wild Card in Climate Change Scenarios

ArcticCarbonThe Arctic Ocean receives about 10 percent of Earth's river water and with it some 25 teragrams [28 million tons] per year of dissolved organic carbon that had been held in far northern bogs and other soils. Now an international team of U.S. and German scientists, including some funded by the National Science Foundation, have used carbon-14 dating techniques to determine that most of that carbon is fairly young and not likely to affect the balance of global climate. Although the current carbon load does not seem likely to affect global climate significantly, they caution in their report that a well-documented Arctic warming trend could result in ancient carbon--a reservoir of the gas currently locked into peat bogs--being added to the mix and contributing to the well- documented Arctic warming trend.

'If current warming trends in the Arctic continue, we can expect to see more of the old carbon now sequestered in northern soils enter the carbon cycle as carbon dioxide. This will act as a positive feedback, tending to enhance the greenhouse effect and accelerate global warming,' said Ronald Benner, an NSF-funded researcher at the University of South Carolina. The team studied rivers in northern Russia and Alaska, along with the Arctic Ocean itself. Benner conducted some of his research as part of the Western Shelf-Basin Interactions research project, which is jointly funded by NSF and the U.S. Office of Naval Research. Previously, scientists had not known the age of the carbon that reaches the ocean. Was it recently derived from contemporary plant material, or had it been locked in soils for hundreds or thousands of years and therefore not part of Earth's recent carbon cycle?

The new findings complement recently published work by Laurence C. Smith, an NSF-funded researcher at the University of California, Los Angeles, indicating that massive Siberian peat bogs, widely known as the permanently frozen home of untold kilometers of moss and uncountable hordes of mosquitoes, also are huge repositories for gases that are thought to play an important role in the Earth's climate balance. Those gases, carbon dioxide and methane, are known to trap heat in the Earth's atmosphere, but the enormous amounts of the gases contained in the bogs haven't previously been accounted for in climate-change models.