
NSF Org: |
OPP Office of Polar Programs (OPP) |
Recipient: |
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Initial Amendment Date: | February 27, 2007 |
Latest Amendment Date: | July 7, 2010 |
Award Number: | 0632346 |
Award Instrument: | Standard Grant |
Program Manager: |
Julie Palais
OPP Office of Polar Programs (OPP) GEO Directorate for Geosciences |
Start Date: | April 1, 2007 |
End Date: | March 31, 2011 (Estimated) |
Total Intended Award Amount: | $0.00 |
Total Awarded Amount to Date: | $125,493.00 |
Funds Obligated to Date: |
FY 2010 = $20,000.00 |
History of Investigator: |
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Recipient Sponsored Research Office: |
1156 HIGH ST SANTA CRUZ CA US 95064-1077 (831)459-5278 |
Sponsor Congressional District: |
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Primary Place of Performance: |
1156 HIGH ST SANTA CRUZ CA US 95064-1077 |
Primary Place of
Performance Congressional District: |
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Unique Entity Identifier (UEI): |
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Parent UEI: |
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NSF Program(s): | ANT Glaciology |
Primary Program Source: |
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Program Reference Code(s): |
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Program Element Code(s): |
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Award Agency Code: | 4900 |
Fund Agency Code: | 4900 |
Assistance Listing Number(s): | 47.078 |
ABSTRACT
Johnson/0632161
This award supports a project to create a "Community Ice Sheet Model (CISM)". The intellectual merit of the proposed activity is that the development of such a model will aid in advancing the science of ice sheet modeling. The model will be developed with the goal of assuring that CISM is accurate, robust, well documented, intuitive, and computationally efficient. The development process will stress principles of software design. Two complementary efforts will occur. One will involve novel predictive modeling experiments on the Amundsen Sea Embayment region of Antarctica with the goal of understanding how interactions between basal processes and ice sheet dynamics can result in abrupt reconfigurations of ice-sheets, and how those reconfigurations impact other Earth systems. New modeling physics are to include the higher order stress terms that allow proper resolution of ice stream and shelf features, and the associated numerical methods that allow higher and lower order physics to be coexist in a single model. The broader impacts of the proposed activity involve education and public outreach. The model will be elevated to a high standard in terms of user interface and design, which will allow for the production of inquiry based, polar and climate science curriculum for K-12 education. The development of a CISM itself would represent a sea change in the way that glaciological research is conducted, eliminating numerous barriers to progress in polar research such as duplicated efforts, lack of transparency in publication, lack of a cryospheric model for others to link to and reference, and a common starting point from which to begin investigation. As the appropriate interfaces are developed, a curriculum to utilize CISM in education will be developed. Students participating in this grant will be required to be involved in public outreach through various mechanisms including local and state science fairs. The model will also serve as a basis for educating "a new generation" of climate scientists. This project is relevant to the International Polar Year (IPY) as the research team is multi-institutional and multi-disciplinary, will bring new groups and new specialties into the realm of polar research and is part of a larger group of proposals whose research focuses on research in the Amundsen Sea Embayment Plan region of Antarctica. The project is international in scope and the nature of software development is quite international, with firm commitments from the United Kingdom and Belgium to collaborate. In addition there will be an international external advisory board that will be used to guide development, and serve as a link to other IPY activities.
PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH
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PROJECT OUTCOMES REPORT
Disclaimer
This Project Outcomes Report for the General Public is displayed verbatim as submitted by the Principal Investigator (PI) for this award. Any opinions, findings, and conclusions or recommendations expressed in this Report are those of the PI and do not necessarily reflect the views of the National Science Foundation; NSF has not approved or endorsed its content.
Liquid water is widespread underneath the Antarctic ice sheet. In fact, changes in subglacial water distribution over time help control variations in ice discharge to the ocean. Hence, studies of water generation and flow in Antarctica represent a critical component of predicting future contribution of the Antarctic ice sheet to global sea level changes. In addition, water trapped beneath the ice sheet provides a possible habitat for microbial life. Antarctic aquatic environments represent a potential analogue for life on icy planetary bodies in our solar system, such as Encaladus and Europa. In this project, we developed a continent-wide heat-budget model for the Antarctic ice sheet (see the attached figure). The results of this model indicate that much more water is being generated beneath this ice sheet than previously thought. Fast-flowing outlet glaciers melt at the base at particularly high rates, as much as three feet per year. We calculated how much subglacial water should discharge beneath some of the major West Antarctic ice shelves, particularly the ones associated with large outlet glaciers emptying into the Amundsen Sea Embayment. These calculated water discharge rates can be used by others in modeling of sub-ice shelf ocean circulation to help verify if these ice shelves can become unstable in the near future. Microbiologists interested in life beneath the Antarctic ice sheet can use our results to understand the extent and potential connectivity of subglacial microbial habitats. This research project involved one Asian-American female doctoral student and one female undergraduate student. These students had the opportunity to learn advanced computer modeling skills, which required understanding of complex mathematical and physical concepts.
Last Modified: 07/02/2011
Modified by: Slawek M Tulaczyk
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