There are many types of C-130s. I am not sure what the “L” stands for, but it means the plane lands on skis. These planes are old (from the 1980s I believe) and mechanical issues are frequent. This season we have been delayed due to problems with the engine, propeller, and rear ski. If maintenance requires at least a whole shift’s worth of work, then the plane is “hard broke”.
Radar instruments such as CDR (Crevasse Detection Radar) have been attached to the lever arm of an LC-130 in the past. This is why IcePod was designed with Hercs in mind as our platform. And for the reason that these are the only aircrafts available in McMurdo suitable for our kind of surveying .
IcePod is equipped with two sets of radar: Deep Ice Radar (DICE) and Shallow Ice Radar (SIR). DICE can penetrate through ice up to about 4kms and can detect the base of the ice shelf, while SIR provides better resolution, seeing to 400m. The SIR is a frequency modulated continuous wave system, while the DICE is a pulsed system. The SIR uses different antennas for transmitting and receiving; DICE is a mono-static system (although it does not appear so).
Expecting to be scheduled only for backup this week with deinstallation Friday night, the ROSETTA team cheered at the dinner table upon news that our flights were in fact scheduled as priority. If all goes well, these nine more flight opportunities are enough to obtain 10km resolution over the whole Shelf! Since Monday morning we have flown three consecutive flights and hopefully the night shift takes off shortly, to make that four.
The previous two flights were lines north of Roosevelt Island. In both flights, cloudy skies forced us to fly above 1800 meters; survey elevation is usually around 950 meters. Today’s flight brought Chris, Grant and I all the way to the southern portion of the Ross Ice Shelf, beyond Crary Ice Rise, where our grid has the least data coverage.
Sure, 7.2 hours is a long time to spend in a plane. But the views are utterly spectacular.
Take-off was scheduled for 9am rather than 8am, which gave us an extra hour of sleep. The plane stayed at the fuel pits for an hour and a half longer than expected. There were issues filling up one of the auxiliary tanks.
Thankfully, a member of the Guard aboard let us know, so we went to the Willy Field galley and refueled ourselves with coffee.
We left the runway closer to 11am, and successfully flew two mid-shelf lines. All were anxious to leave the runway and return to surveying, after more than a week of delays.
We have had quite an unlucky streak of cancellations. The New York Air National Guard crew who fly the aircraft for day lines departed from the ice for some deserved r & r. Their southbound flight from Christchurch has been delayed a couple times. No Guard, no flight, no surveying. Also, many of our night flights have been delayed due to weather.
With all the down time I have been reading a lot. Most of the books borrowed from home I stowed in Christchurch, but fortunately the library has a wide selection, including one section just on the Antarctic. It is conveniently located on the first floor of my dorm, and run by volunteers. I very much enjoy this space. It is cozy and warm, and gusts of wind against the glass produce the only sounds in the room.
You are probably wondering what ROSETTA-Ice is really all about.
ROSETTA-Ice is a current project that is acquiring geophysical data over the Ross Ice Shelf, using an LC-130 aircraft. The Ross Ice Shelf (RIS) is a floating extension of the West Antarctic Ice Sheet that occupies the southern Ross Embayment in West Antarctica. It buttresses ice that flows from West Antarctic ice sheets.
The aim of ROSETTA-Ice is to learn more about the interactions between ice, ocean, and underlying rock. The acronym ROSETTA broken down (get ready): A systems approach to understanding the Ross Ocean and ice Shelf Environment and Tectonic setting Through Aerogeophysical surveys and modeling.
We care about the bathymetry beneath the RIS because it controls the circulation of sub-Shelf ocean water that may warm the ice shelf from below. Obviously, this is bad for the stability of the RIS. Obscured by thick ice and water, the bathymetry beneath the RIS cannot be measured directly, and therefore is very poorly known. Depth-sounding data from the 1970’s Ross Ice Shelf Geophysical Glaciological Survey (RIGGS) produced a map at 55 km resolution. 55 kms! ROSETTA-Ice is working towards 10 km resolution. The bathymetry and geology may be constrained by gravity and magnetic data. ROSETTA uses IcePod, a suite of instruments contained in, well, a metal pod, that is attached to the lever arm of the aircraft, to primarily study the ice. ALAMOs (air-launched autonomous micro observers) help us learn more about the ocean, measuring profiles of temperature and salinity.
Most members of the team are from Lamont Doherty Earth Observatory, Earth Institute at Columbia University. Others represent institutions such as Colorado College, Earth and Space Research in Seattle, GNS in New Zealand, Scripps Institute of Oceanography at UC San Diego, and the USGS in Denver. So it is very much a collaborative effort; engineers, geologists, geophysicists, glaciologists, oceanographers and modelers, working together.