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Flipping Magnetic Fields

North and south. We take these directions for granted. Pull out a compass and the needle will swing to the north in response to the magnetism in the Earth's crust. The magnetic poles roughly coincide with the axis of the Earth's rotation. But some scientists believe that the Earth's magnetic field has reversed itself several times within geological ...

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FlippingMagneticFields
Physics

Why Does A Golf Ball Have Dimples?

A golf ball can be driven great distances down the fairway. How is this possible? The answer to this question can be found by looking at the aerodynamic drag on a sphere without dimples (while it's ... Continue reading

GolfBallDimples
Geology

Global Warming?

The contiguous United States experienced its 16th coolest summer on record and seventh coolest August, according to scientists at NOAA Climatic Data Center in Asheville, N.C. While much of the West, ... Continue reading

GlobalWarming
Geology

A National Park of Caves

Carlsbad Caverns National Park has been designated as a world heritage site because of its unique and surprising geology - a story more than 250 million years old that can be read both above and below ... Continue reading

ANationalParkofCaves
Biology

Steller Sea Lion Biology

The Steller sea lion (Eumetopias jubatus) is the largest member of the Otariid (eared seal) family. Males may be up to 325 cm (10-11 ft) in length and can weigh up to 1,100 kg (2,400 lb). Females are ... Continue reading

StellerSeaLionBiology

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.