Category Archives: Uncategorized

Greenland Preparation II: Glacier Travel Training

As part of our preparation for summer field work in Greenland, we took part in a 2-day Glacier Travel course at the International Mountain Climbing School in North Conway, New Hampshire. In the course, our team learned the basics of roped glacier travel and crevasse rescue.

Testing a snow anchor in the rapidly melting spring New Hampshire snow.
Testing a snow anchor in the rapidly melting spring New Hampshire snow.
Preparing to haul a team member out of a "crevasse."
Preparing to haul a team member out of a “crevasse.”

 

Greenland Preparation I: Discharge measurement

This spring semester we began preparations for upcoming fieldwork on the Greenland Ice Sheet, supported by an NSF project in collaboration with Jason Gulley at USF. The goal of the project is to study the links between meltwater delivery to moulins (deep holes in the surface of the ice sheet), the evolution of conduit systems within the ice, and the sliding motion of the ice sheet. When meltwater reaches the base of the ice, it can lift the ice, reduce friction, and accelerate the sliding of the ice. However, models of the processes behind these links remain relatively poorly constrained by data. To examine these links in the field, we will measure water levels within the moulins, discharge within the meltwater streams that feed the moulins, and use GPS units to record the motion of the ice.

In preparation for work in Greenland this summer, we have been refining our protocols for discharge measurement within the meltwater streams. We will make these measurements by injecting known quantities of a harmless fluorescent dye (Rhodamine) and measuring concentrations of that dye downstream using field fluorometers.

Pumping dye into nalgene bottles for shipment to Greenland.
Pumping dye into nalgene bottles for shipment to Greenland.
Prototype pump setup for dye injection.
Prototype pump setup for dye injection.
Dye in a spring run where we were testing the measurement procedure.
Dye in a spring run where we were testing the measurement procedure.
Field fluorometers deployed in stream.
Field fluorometers deployed in stream.

 

Glacier caving in Svalbard

Ken Mankoff rappelling into the moulin entrance of Bird Brain Cave, Hornsund, Svalbard.

In fall of 2016, I participated in a National Geographic sponsored glacier cave expedition to the Polish Polar Station at Hornsund. The expedition was lead by Ken Mankoff (Penn State). Geomicrobiologist Jenn Macalady (Penn State) and italian geologist/caver/mountaineer Maurizio Mainiero filled out the team. Following up on prior work, the focus of the expedition was 3D scanning within glacier caves. We hoped to better characterize the roughness of subglacial conduits and the impacts that conduit geometry has on subglacial water flow and pressure. In general, glacier caves play an important role in routing meltwater from glacial surfaces to the toe of the glacier. The efficiency of these flow paths can have a strong influence on the speed at which a glacier slides. However, current models of these flow paths are relatively poorly constrained due to a general lack of data. Our trips to the belly of the glacier were aimed at filling this data gap. Our trip was plagued by warm temperatures that made the field work challenging (due to high water in the caves). However, we had just enough days below freezing to collect the critical data we needed.

We acknowledge the valuable support of both the National Geographic Society’s Research and Exploration fund and the Polish Institute of Geophysics, which were our hosts in Hornsund.

Jenn Macalady taking water samples from the main stream in Bird Brain Cave.

Blowing Spring Cave Observatory

Students in the fall 2014 Karst Hydrogeology course installing equipment and conducting research projects at Blowing Spring Cave.

The Blowing Spring Cave Observatory is a field site that we use for a variety of research and educational purposes. Research at the site started with Kathy Kneirim’s PhD research examining carbon and E. coli dynamics at the site (Kneirim et al. 2013Kneirim et al. 2015). Equipment to monitor dissolved and gaseous carbon dioxide, as well as air flow velocity and other basic environmental parameters, were installed in spring of 2014. Over 30 additional water quality and air temperature data loggers were installed during Covington’s Karst Hydrogeology course in fall of 2014, resulting in what may be one of the most heavily instrumented caves anywhere. A recent piece on the local NPR show Ozarks at Large featured our work at this site.

Ongoing work in the cave is focusing on interactions between carbon dioxide concentrations within the cave stream and cave ventilation processes as a part of Holly Young’s masters thesis work. The cave airflow is driven primarily by the chimney effect, where the entrance of the cave acts as a lower entrance. This means that fresh outside air is drawn into the cave during cool periods, whereas air blows out the entrance during warm outside weather. Preliminary data suggest that the periods of time when the cave stream is undersaturated with respect to calcite, and therefore capable of dissolving the limestone rock in which it is formed, are largely controlled by these airflow patterns.

Carbon dioxide concentrations in the air (red line) and water (blue line) of the cave along with cave airflow velocity (black line). Negative velocities (red shading) are periods of time when outside air is drawn into the cave entrance resulting in low concentrations of carbon-dioxide in the air. After longer periods of airflow reversals the carbon-dioxide concentrations in the cave stream also begin to fall. The tends to result in saturated or supersaturated conditions in the stream.
Carbon dioxide concentrations in the air (red line) and water (blue line) of the cave along with cave airflow velocity (black line). Negative velocities (red shading) are periods of time when outside air is drawn into the cave entrance resulting in low concentrations of carbon dioxide in the air. After longer periods of airflow reversal the carbon dioxide concentrations in the cave stream also begin to fall. This tends to result in saturated or supersaturated conditions in the stream.

Undergraduate research, begun in the Karst Hydrogeology course and continued by Alex Breeding, is studying cave air temperature dynamics within entrance zones and trying to quantify distance into the cave that air temperature is influenced by outside temperatures. Contrary to prior theoretical work, our new model and observational data suggest that this zone of external temperature influence expands over the duration of the winter. A few weeks of cave air temperature data are depicted in the animation below. The leftmost data point is outside temperature.

We thank the Bella Vista Village Property Owners Association for their helpful cooperation with this work and for access to Blowing Spring Cave.