Science Daily has had more than its usual quota of interesting pieces over the last few days. Here are a few of them:\
Very long lasers made of optical fibers offer a promising route to highly secure communications.
Nothing beats quantum communication for absolute security, but the new method, which relies on classical rather than quantum physics, provides faster communication over long distances. It would also be feasible with existing hardware, in contrast to quantum communication that will require development of new, and probably expensive, components.
A new technique to identify objects of art will be foolproof
The system is based on the owner of the work selecting, for example, one square centimetre. The roughness/texture and colour of that square centimetre are then measured on a micrometer scale, and put into a database. Objects and collections which are fingerprinted can then be easily identified and traced when on loan or in transport.
It sounds good, but mightn’t it be a bit premature to say it’s foolproof?
Greenland Ice Sheet Still Losing Mass
The study indicates that from April 2004 to April 2006, Greenland was shedding ice at about two and one-half times the rate of the previous two-year period, according to CU-Boulder researchers Isabella Velicogna and John Wahr. The researchers used measurements taken with the Gravity Recovery and Climate Experiment, or GRACE, to calculate that Greenland lost roughly 164 cubic miles of ice from April 2004 to April 2006 — more than the volume of water in Lake Erie.
Erie is by far the smallest of the Great Lakes by volume, but that’s still a hell of a lot of water. This last story has an explanation of how the dual-satellite GRACE experiment works.
A change in gravity due to a pass by GRACE over a portion of Greenland imperceptibly tugs the lead satellite away from the trailing satellite, said Velicogna. A sensitive ranging system allows researchers to measure the distance of the two satellites down to as small as 1 micron — about 1/50 the width of a human hair — and to then calculate the ice mass in particular regions of Greenland.