2003-2004 USAP Field Season

Glaciology

Dr. Julie Palais
Program Manager

I-190-M

NSF/OPP 02-29546
Station: McMurdo Station
RPSC POC: Doug Miller
Research Site(s): McMurdo Station, USCG Icebreaker, Drygalski Ice Tongue, Ross Ice Shelf
Dates in Antarctica: Early October to mid February

Collaborative research of Earth's largest icebergs
Dr. Douglas R. MacAyeal
University of Chicago
Department of Geophysical Sciences
drm7@midway.uchicago.edu
http://amrc.ssec.wisc.edu/amrc/iceberg.html
 
RV Polar Sea "facing off" against iceberg B15A for the first time in January of 2001. This project flew off the deck of the Polar Sea and placed sensors and GPS receivers on the iceberg, allowing them to monitor it's position and weather conditions. Photo
Deploying Team Members: Tim Parker . Mary Templeton . Ronals Ross . Andrew Bliss . Jill Franks . Young-Jin Kim . Douglas R. MacAyeal . Emile Okal . Marianne H. Okal . Olga V. Sergienko . Jonathan E. Thom
Research Objectives: Icebergs released by the antarctic ice sheet represent the largest movements of fresh water within the natural environment. Several of these icebergs, B–15, C–19, and others calved since 2000, represent over 6,000 cubic kilometers of fresh water—an amount roughly equivalent to 100 years of the flow of the Nile River.

We will study the drift and breakup of the Earth’s largest icebergs, which were recently released into the Ross Sea as a result of calving from the Ross Ice Shelf. We will attempt to ascertain the physics of iceberg motion within the dynamic context of ocean currents, winds, and sea ice, which determine the forces that drive iceberg motion, and the relationship between the iceberg and the geographically and topographically determined pinning points on which it can ground. In addition, we will study the processes by which icebergs influence the local environment (sea ice near Antarctica, access to penguin rookeries, air-sea heat exchange and upwelling at iceberg margins, nutrient fluxes), as well as the processes by which icebergs generate globally far-reaching ocean acoustic signals that are detected by seismic-sensing networks.

In addition, we will attempt to deploy automatic weather stations, seismometer arrays, and global positioning system tracking stations on several of the largest icebergs presently adrift, or about to be adrift, in the Ross Sea. Data generated and relayed via satellite to our home institutions will lead to theoretical analysis and computer simulation and will be archived on a Web site (http://amrc.ssec.wisc.edu/amrc/iceberg.html) that scientists and the general public can access.

A better understanding of the impact of iceberg drift on the environment, and particularly the impact on ocean stratification and mixing, is essential to understanding the abrupt global climate changes witnessed by proxy during the Ice Age and future greenhouse warming. More specifically, the study will generate a knowledge base useful for the better management of antarctic logistical resources that can occasionally be influenced by the adverse effects icebergs have on sea ice (the shipping lanes to McMurdo Station, for example).