Download Iceworld Map For Condition 27
Delmy Moonsommy
Glaciers form as layers of snow accumulate on top of each other. Each layer of snow is different in chemistry and texture, summer snow differing from winter snow. Over time, the buried snow compresses under the weight of the snow above it, forming ice. Particulates and dissolved chemicals that were captured by the falling snow become a part of the ice, as do bubbles of trapped air. Layers of ice accumulate over seasons and years, creating a record of the climate conditions at the time of formation, including snow accumulation, local temperature, the chemical composition of the atmosphere including greenhouse gas concentrations, volcanic activity, and solar activity.
Ice cores are cylinders of ice drilled from ice sheets and glaciers. They are essentially frozen time capsules that allow scientists to reconstruct climate far into the past. Layers in ice cores correspond to years and seasons, with the youngest ice at the top and the oldest ice at the bottom of the core. By drilling down into the ice sheet or glacier and recovering ice from ancient times, scientists are able to determine the past composition and behavior of the atmosphere, what the climate was like when the snow fell, and how the size of ice sheets and glaciers have changed in the past in response to different climate conditions. Ice cores have provided climate and ice dynamics information over many hundred thousand years in very high, sometimes seasonal, resolution. This information allows scientists to determine how and why climate changed in the past. By understanding how and why climate changed in the past, scientists are able to improve predictions of how climate will change in the future.
Because of their high time-resolution, the physical nature of their proxy records, and their ability to archive actual greenhouse (and non-greenhouse) gas concentrations from the past, ice cores have become one of the golden standards in paleoclimate research.
NSF-ICF's most important responsibility is for the safe and secure storage and curation of ice cores that are collected primarily by National Science Foundation sponsored projects. NSF-ICF currently stores over 17,000 meters of ice core collected from various locations in Antarctica, Greenland, and North America. NSF-ICF's main archive freezer is 55,000 cubic feet in size and is held at a temperature of -36C.
When a shipment of new ice arrives, the insulated boxes carrying the cores are quickly unloaded into the main archive freezer. Once the new ice has come to thermal equilibrium with its new surroundings, it is carefully unpacked, organized, racked and inspected. After racking, the tubes are checked into NSF-ICF's inventory system.
In addition to the main archive freezer, NSF-ICF also has an exam room held at -25C that scientists use when examining the ice cores. The exam room is 12,000 cubic feet in size and is contiguous with the main archive area. In addition, there is also a Class-100 HEPA-filtered, cold clean room held at -25C that scientists can use.
Scientists often use the exam room to cut samples from the ice cores, and then ship the samples back to their university or laboratory for analysis. Very few analyses on the ice cores are actually carried-out at the NSF-ICF facility. Almost all of the measurements that are made on the ice cores are conducted back at the scientist's university or laboratory.
The floor plan of the exam room will be specifically tailored to the number of scientists and the type of science or sampling which will be done during a particular CPL. As many as 10 different preparation, cutting, or analysis stations may be set up to accommodate the core with additional processing being performed off the main line if required.
At sites where the ice is well below freezing, such as the interiors of the polar ice sheets, mechanical drills must be used. In contrast, thermal drills are particularly effective at coring through warmer ice (e.g., ice approximately above -10C) and are frequently used on mid- or low-latitude glaciers. On many non-polar glaciers, however, ice conditions can vary from "cold" ice to "warm" ice, requiring both mechanical and thermal drilling to retrieve the best possible core quality over the entire depth interval that is drilled.
When scientists are interested in collecting ice cores from the top 20- to 30-meters of a glacier or ice sheet a hand auger is commonly used. In the United States, there are four types of hand augers commonly used: the SIPRE auger, the PICO auger, the Kovacs auger, and the IDDO auger.
The hand auger is the most basic of the mechanical drills and consists of a barrel and cutting head. The barrel is typically 1 meter long and with an internal diameter of either 3 or 4 inches. A protruding thread spiraling up and around the barrel is used to remove the ice chips from the cutting face. The cutter head includes 2 or 3 hardened steel or carbide teeth, and the protrusion of the teeth can be adjusted to control the depth of cut. If the depth of cut is set too small, the cutter head will skid over the ice surface rather than cut down into it. If the depth of cut is set too large, the teeth will become lodged in the ice halting the drilling altogether.
While most cable-suspended drills are similar in design, the details do vary from drill to drill, often with specific projects and field sites in mind. For instance, due to the remoteness and high-altitude of most non-polar glaciers, the drills used at these locations must be lightweight and of modular design to allow for transportation by helicopter, or for glaciers located above the range of helicopter operation (e.g., above 5500 meters elevation), transportation by either porters or pack animals. In the polar regions, extremely low temperatures and very remote and logistically complicated field sites influence the design of the drills used.
Below are general descriptions for two types of cable-suspended ice coring drills: electromechanical and electrothermal. More detailed information can be found by reading the literature noted in References and Links.
There are many versions of the electromechanical (EM) drill used in ice coring. The portion of the drill that goes down the borehole is called the sonde, and its only physical connection to the surface is through its suspending cable. The components of the sonde typically include a cutting head that is attached to an inner barrel, an outer barrel, a motor to rotate the inner barrel, and an anti-torque system that counteracts the rotational cutting action.
The cutting head typically has 3 to 4 hardened steel or carbide teeth that shave ice in an annulus around the central, vertical core. The protrusion of the teeth and their subsequent depth of cut into the ice are controlled with small, adjustable buttons called shoes that are located on the bottom face of the cutter head. The vertical distance between the bottom of the shoes and the cutters determines the depth of cut into the ice.
A protruding thread, also referred to as flights, spiraling up and around the inner barrel is used to remove the ice chips from the cutting face. As the cutting head spins around and the cutters shave the ice, the chips are transported up the flights between the two barrel sections. The inner barrel spins while the outer barrel stays stationary, and it is that difference that actually drives the chips upward along the flights to the top of the sonde thus removing them from the cutting face.
Most cable-suspended EM drills are designed as double-barreled (e.g., an inner barrel and an outer barrel) for several reasons. Double-barreled drills collect ice chips more efficiently than single-barreled drills, and the added stiffness of the double-barreled design typically results in fewer breaks in the cores that are drilled, as well as straighter boreholes.
The anti-torque system on EM drills often consists of three or four leaf springs that anchor the sonde to the wall of the borehole. If there is no anti-torque section, the motor will cause the entire EM drill and cable to rotate inside the borehole, preventing the ice from being cut and causing the cable to become wrapped.
When a drill run is finished and the barrel is full with ice, the core is typically held in the inner barrel by spring-loaded lever arms called core dogs that grip, break, and retain the ice core when the cable and sonde is pulled upward. The sonde is then hoisted to the surface with the winch and the core removed. In many modern cable-suspended EM drill systems, the sonde and tower both tilt from the vertical position to the horizontal position to aid in the removal of the ice core and the chips.
The electrothermal (ET) drill uses a ring-shaped heating element in the coring head to melt an annulus around the ice to be cored, rather than shaving it away with cutters like the EM drill. The electrical power to heat the coring head is fed through the drill's suspending cable.
The meltwater that is produced by ET drills may either be left down the hole or stored in a tank within the sonde. When englacial temperatures are low and there is concern that the meltwater may re-freeze causing the borehole to close-in on itself, the meltwater is either stored in a tank in the sonde and emptied once on the surface, or the meltwater is mixed with an antifreeze solution and left down the hole. For depths below which borehole closure in an open hole is a concern, the meltwater is left down the hole to help prevent hole closure. If re-freezing is also a concern, the meltwater that is left down the hole is mixed with an antifreeze solution.
ET drills have only one barrel, so the size of the borehole is generally smaller than a borehole from an EM drill for a similar diameter ice core. ET drills are mechanically much simpler than EM drills because they contain fewer moving parts. They also do not require an anti-torque system since there is no rotational cutting action. ET drills are also generally more compact in size and weight than EM drills, in part because no chip storage is required.
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