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Stopping In Thin Air

Imagine you're going very fast -- much faster than a race car. In fact, imagine you're going 100 or 200 times faster than a race car. When you reach your destination, you need to stop relatively quickly. How would you do it? It wouldn't take a rocket scientist to think of using the brakes. But, it might take a rocket scientist to skip the brakes, ...

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StoppingInThinAir
Chemistry

The Melting Point

Physical properties of a material fall into two categories: intrinsic properties determined by the structure of the particular molecule, and bulk properties characteristic of quantities of molecules ... Continue reading

TheMeltingPoint
Chemistry

Table Salt - It's All In The Ions

All elements are defined by their individual atoms, which are in turn identified by the number of protons in the nucleus of each atom. Since protons are carriers of positive electrical charge, there ... Continue reading

TableSaltItsAllInTheIons
Astronomy

Magnitude of an Astronomical Object

'Visual magnitude' is a scale used by astronomers to measure the brightness of a star. The term 'visual' means the brightness is being measured in the visible part of the spectrum, the part you can ... Continue reading

MagnitudeofanAstronomicalObject
Biology

Tea Time!

Did you know that a disease of coffee plantations made the British tea drinkers? In the 1700s Britain had many coffeehouses that served as popular social gathering places to discuss current events and ... Continue reading

TeaTime

Is Earth Getting Fatter Around the Belt?

EarthBeltBesides being used for transmission of this email message to you, communication satellites are used for some neat science. By shooting a laser beam onto them and measuring how long it takes for light to bounce back, scientists at NASA measure precise orbits of a number of satellites and hence the Earth's gravitational field as a function of longitude and latitude. NASA has been making these measurements for the last 25 years and it turns out the results are quite interesting.

According to the satellite data, prior to 1998, Earth's gravitational field had been decreasing at the equator and increasing at the poles. Since Earth is shaped like a pumpkin, wider at the equator and narrower at the poles, this means that our planet was getting more spherical or thinner at the equator. This is consistent with how the melting of large ice mass from the poles since the last Ice Age would affect the Earth's shape. Namely, once the pressure from the ice was gone, the ground at the poles actually expanded outward.

Data since 1998 shows an abrupt change in this trend. Earth's gravitational field is increasing now at the equator! Is the Earth getting fatter around the belt? Only significant movement in ocean water, polar and glacial ice, or atmosphere could account for these changes. Scientists are still not sure what the answer is, but some early research findings suggest it may be the movement in ocean water. Somehow, ocean currents gather large quantities of water around the equator every once in a while. Some scientists suggest that this is a cyclic event, but data is still inconclusive.