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Ablation Rates of Taylor Glacier, Antarctica
Entry ID: NSIDC-0326


Summary
Abstract: This data set provides glacier surface ablation rates for a network of approximately 250 sites on Taylor Glacier, spanning a period from 2003 to 2011. Here sublimation is the dominant ablation mechanism, though a few sites have accumulation. Ablation data are provided in meters water equivalent per year.

Data are available via FTP in space-delimited ASCII format.
Related URL
Description: Documentation

Description: FTP
Geographic Coverage
Spatial coordinates   
  N: -77.6   S: -77.9   E: 162.2   W: 160.1

Data Set Citation
Dataset Originator/Creator: Cuffey, K. M., A. Bliss, and J. Kavanaugh.
Dataset Title: Ablation Rates of Taylor Glacier, Antarctica
Dataset Series Name: NSIDC-0326
Dataset Release Date: 2007-12-01
Dataset Release Place: Boulder, Colorado USA
Dataset Publisher: NSIDC: National Snow and Ice Data Center
Version: 1
Online Resource: http://www.usap-dc.org/view/dataset/609326
Temporal Coverage
Start Date: 2002-11-19
Stop Date: 2011-01-12
Location Keywords
Data Set Progress
COMPLETE
Distribution
Distribution Media: FTP
Distribution Size: 11 KB
Distribution Format: ASCII Text (.txt)
Publications/References
Aciego, Sarah, Kurt M. Cuffey, Jeffrey L. Kavanaugh, D.L. Morse, and J.P. Severinghaus. 2007. Pleistocene Ice and Paleo-strain Rates at Taylor Glacier, Antarctica. Quaternary Research 68:303-313.

Bliss, A. K., K. M. Cuffey, and J. L. Kavanaugh. 2011. Sublimation and Surface Energy Budget of Taylor Glacier, Antarctica. Jounral of Glaciology. 57 (204, 684-696).

Bliss, A. K. 2011. Ablation on Taylor Glacier, Antarctica. PhD Thesis, University of California, Berkeley.

Kavanaugh, J. L., K. M. Cuffey, D. L. Morse, A. K. Bliss, and S. M. Aciego. 2009. Dynamics and Mass Balance of Taylor Glacier, Antarctica: 3. State of Mass Balance. Journal of Geophysical Research, 114, F04012, doi:10.1029/2009JF001331
Extended Metadata Properties
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Creation and Review Dates
DIF Creation Date: 2007-12-01
Last DIF Revision Date: 2017-08-23


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