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The Physics of Sandcastles

Give a plastic bucket and a shovel to a child, then turn her loose on a beach full of sand. She'll happily toil the day away building the sandcastle to end all sandcastles. It's pure fun. It's also serious physics. Sandcastles are built from grains - billions of tiny sharp-edged particles that rub and tumble together. The strength of a sandcastle ...

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Sandcastles
Physics

Ultraviolet Light

Ultraviolet light is a form of radiation which is not visible to the human eye. It's in an invisible part of the 'electromagnetic spectrum'. Radiated energy, or radiation, is given off by many ... Continue reading

UltravioletLight
Chemistry

Take Two And Call Me In The Morning

Aspirin has been used for hundreds of years to relieve pain and reduce inflammation. It belongs to a group of chemicals called salicylates and was originally derived from the bark of the willow tree. ... Continue reading

Aspirin
Chemistry

Oil Viscosity

Everybody recognizes 'oil' as a word for liquid materials that do not behave like water. They have a 'thickness' and self-cohesive character (autocohesion) that enables them to form a film on a ... Continue reading

OilViscosity
Astronomy

Near-Earth Supernovas

Supernovas near Earth are rare today, but during the Pliocene era of Australopithecus supernovas happened more often. Their source was an interstellar cloud called 'Sco-Cen' that was slowly gliding by ... Continue reading

Supernovas

Antarctica and Climate Change

AntarcticaandClimateChangeBecause of its influence on world weather and climate patterns, Antarctica lies at the heart of the debate on climate change and has become the premier location in which to study the effects of global warming. Over the course of the past 50 years, Antarctica's average year-round temperature has warmed by about 3-4 degrees Fahrenheit - more than 10 times the average worldwide increase during that period. As a result of these increases in temperature (which are not necessarily the result of global warming), the Antarctic continent has experienced changes in its landscape and ecology. Scientists are also concerned that with such dramatic increases in the icy continent's temperature, significant rises in global sea levels could occur if Antarctica's thick polar ice sheet melts. The West Antarctic ice sheet alone, if melted, could raise average sea levels around the world by about 20 feet, resulting in the flooding of low-lying coastal zones.

The effects of climate change on Antarctica vary from migrations of seal and penguin populations to other parts of the continent to abrupt changes in the glacial landscape. In March, 2000 the Larson B ice shelf in northern Antarctica - an area the size of Delaware - broke away from the continent and retreated into the sea. Similarly, in January, 1995, the Larson A ice shelf calved away from the continent, disappearing into the sea and bringing with it part of an Argentine base camp. Ice shelf instability is created as a result of higher sea and air temperatures, and a number of northern ice shelves have displayed similar trends such as the Wordie, Muller and Prince Gustav Channel shelves.

Perhaps most vulnerable to the effects of Antarctic climate change are the continent's wildlife populations. Increasing temperatures, less ice, and more snowfall have altered the patterns and habitats of several Antarctic species, such as the southern fur and elephant seals and Adelie and Chinstrap penguins. Although the past 20 years have seen an increase in the numbers of Chinstrap penguins on the continent, the opposite is true for the Adelie penguin. Rising Antarctic temperatures also have resulted in more snowfall on the continent; making breeding difficult for the ice-loving Adelie penguins. Seal populations, on the other hand, have benefited from the reduction in sea ice as they prefer breeding and feeding in open waters. Several seal populations in Antarctica have increased their numbers by over 300% in the last 20 years.