Fiber-optic cables like the ones that bring television and Internet into millions of homes are now being used to measure how fast ice shelves in Antarctica are melting, according to new research.
Researchers installed moorings containing fiber-optic cables hundreds of meters down into the McMurdo Ice Shelf in West Antarctica to collect temperature information about the base of the ice shelf, where the thick platform of floating ice meets the ocean. The sensors were able to measure mere millimeters of ice loss at the interface, demonstrating that the new fiber-optic method could be used to remotely monitor the ice shelves in real-time.
Data on the melting rates of ice shelves provides scientists with critical information on the stability of the Antarctic ice sheets and sea level rise.
GeoSpace spoke with Scott Tyler, a hydrologist at the University of Nevada, Reno and one of the study’s principal investigator, about the new research that has been accepted for publication in Geophysical Research Letters, a journal of the American Geophysical Union.
GeoSpace: How did you become interested in this idea to begin with?
Scott Tyler: My group does a lot of work with fiber optic temperature sensing for environmental monitoring—measuring in lakes, streams, and the atmosphere. A colleague of mine, an ice core specialist, said this would be an interesting tool to measure glacier temperature and look at ocean temperatures in the Antarctic. I talked to Dave Holland an oceanographer at New York University, and Victor Zagorodnov, a glaciologist [at Ohio State University in Columbus, Ohio] and ace ice core driller, and we put together a proposal to the National Science Foundation to measure the temperature of the ocean and the ice continuously with a fiber optic temperature sensing system and [to develop] a light-weight and portable drilling system that could zip down through the ice and get access to the ocean below.
Then Scott Kobs [a graduate student in Geological Sciences and Engineering at the University of Nevada Reno] came up with the idea to look carefully at the temperature record over the 14-month deployment. We can actually see the bottom of the shelf moving up over time; instead of an average annual melt rate we can get the melt rate almost on a daily basis, which is pretty hard to do.
Let’s say I put something down through the ice and it’s now looking up at the bottom of this ice shelf. As the ice shelf melts the sensor gets further and further away from the ice, and at some point it can’t measure the interface anymore because it’s melted up away from it. But because our tool just has this fiber cable hanging in a hole, as the ice melts it exposes more and more of our optical fiber, so we just keep seeing the interface.
GeoSpace: How do the fiber optic sensors work?
Scott Tyler: Think about when you shine a light in a dusty room, you can see the sparkles of the dust in the room. The color of those sparkles—the backscattered light or the reflection—actually tells me the temperature of the dust.
So in an optical fiber I send a little pulse of light down the fiber, just like a flashlight, and then measure the reflection that I see as the light goes down the optical fiber. It’s a really subtle change in color that your eyes can’t see but our instruments can. The color of that light tells me the temperature of that place along the fiber. I can calculate where that was because I know the speed of light in the fiber and a stopwatch [keeps track of] when I sent the light and when I see that sparkle of light. So I can get a temperature and a distance down the optical fiber.
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Source by Advancing Earth and Space Science
By Kate Wheeling
