The Glacier Dynamics lab at UIdaho welcomes Tristan Amaral this semester. Tristan will be working on a NASA and NSF-funded project to examine the controls on calving around the Greenland Ice Sheet. He comes to us after graduating Summa Cum Laude from the University of New Hampshire, a published paper behind him, and experience working for the Juneau Icefield Research Program (JIRP). We’re happy to have him in Moscow!
The Uummannaq region of West Greenland is a spectacular area of steep cliffs, icefalls, and long fjords. While on a NASA-funded research project to better understand the connections between water in these fjords and the glaciers terminating there, I’ve had the extraordinary opportunity to fly, camp, hike, and work in this landscape. Now, you can get a taste for our work in a 4-minute movie set to music, that draws on video footage from 2015 fieldwork, and time lapse imagery from 2013. I hope you enjoy it!
Thanks to Sophie Gilbert (University of Idaho) for producing this movie.
One of my two presentations at the AGU fall meeting this year is the subject of a well done blog post. In the presentation, my co-authors and I reported the detection of over one million icequakes produced near the terminus of a tidewater glacier in west Greenland. Study of these icequakes will allow us to better understand the factors controlling the flow of glacier ice, and ultimately allow scientists to make more precise predictions of sea level rise.
We’re presently about half way through the meeting this year and its been a good week so far. During the Saturday and Sunday prior to the beginning of the AGU fall meeting, I participated in a planning workshop to lay the groundwork for a monitoring network to observe ice-ocean interactions in Greenland. I made the case for the value of seismology in understanding tidewater glacier dynamics.
My second invited presentation is a poster on Thursday afternoon. I’ll be sharing observations and interpretations of high-rate velocity variations near the front of one of Greenland’s largest ocean-terminating glaciers. The presentation is C43B-0805 High-resolution, terrestrial radar velocity observations and model results reveal a strong bed at stable, tidewater Rink Isbræ, West Greenland.
After spending September in Greenland, the UT/KU team has returned from our third and final field season in the Uummannaq region of western Greenland. We recovered equipment that has been monitoring tidewater glaciers in the region for two years, as well as made a set of shorter-term, higher-resolution observations that required us to camp adjacent to one of the glaciers for 10 days. We’re looking forward to working with the data, and sharing our results at this fall’s AGU meeting, future conferences, and in publications.
The seismometers, GPS, timelapse cameras, and weather stations we recovered were in great shape. We also recorded excellent terrestrial interferometric radar observations (in spite of strong, consistent katabatic winds) and more seismic and GPS data. Due to the lateness of our field work (our previous field work has been in July and August), we also got to experience the transition in seasons, from fall to winter. This meant wonderful twilight, rich red tundra, and the first snows on the mountain tops.
You can read more about this interdisciplinary, NASA-funded project here.
At the annual meeting of the Program for Arctic Regional Climate Assessment (PARCA) hosted at the NASA Goddard Space Flight Center, I’ll be presenting new data that allow a more complete view of the iceberg calving process. These data include ground-based radar interferometry, seismic, and ocean current observations that reveal how major calving events proceed over 10s of hours before, during and after an iceberg detaches from the terminus. This PARCA presentation will be the first view of these data, collected during the 2014 summer at the terminus of Rink Isbrae in West Greenland. Further analyses of these data, taken together, will contribute to our understand of how and why calving occurs at Greenland’s largest outlet glaciers, and what the effects of these events are on the glaciers and adjacent ocean.
The PARCA meeting takes place on January 27th in Greenbelt, Maryland. You can read more about the project that supported collection of this data here.
During the last several days, I have taken part in an international workshop to identify the major gaps in the scientific community’s understanding of interactions between the Greenland Ice Sheet and its surrounding ocean.
The workshop on Greenland Ice Sheet-Ocean Interactions, under the acronym GROCE, was hosted by the Alfred Wegener Institute, in Bremerhaven, Germany. Over the two day meeting, ~28 scientists from Germany, Norway, the UK, Poland, Japan, Canada, the US and other countries framed the questions we considered most essential for understanding Greenland’s rapid changes, as well as the strategies and resources necessary to respond to those questions. It was interesting and exciting to hear the commonalities and differences in research priorities from the broad cross section of glaciologists and oceanographers in attendance.
The report produced to summarize our workshop will be used to help guide funding agencies and the proposal efforts of the broader scientific community.
Next stop for me: San Francisco. The annual meeting of the American Geophysical Union starts there on Monday.